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[svn r5981] Everything in this crock of a directory gets past the validator. That's not to say that it's right. (All the links to external bodies' websites are completely wrong.)
This commit is contained in:
dave
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<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
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<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
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<html>
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"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
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<html xmlns="http://www.w3.org/1999/xhtml">
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<head>
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<head>
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<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
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<meta http-equiv="Content-Type" content=
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<title>
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"text/html; charset=iso-8859-1" />
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BEC
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<title>BEC</title>
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||||||
</title>
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<link rel="stylesheet" type="text/css" href=
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<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
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"../../css/main2.css" />
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||||||
</head>
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</head>
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<body>
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<body>
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<center><h2>Bristol Exploration Club</h2></center>
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<h1>Bristol Exploration Club</h1>
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The <a href="http://web.ukonline.co.uk/john/index.htm">Bristol Exploration
|
<p>The <a href="http://web.ukonline.co.uk/john/index.htm">Bristol Exploration
|
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Club</a> is one of the "elder clubs" of Mendip. They foster their own
|
Club</a> is one of the "elder clubs" of Mendip. They foster their own reputation
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reputation for worldwide expeditions by their slogan "The BEC gets
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for worldwide expeditions by their slogan "The BEC gets everywhere" seen on
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everywhere" seen on stickers in the most unlikely places :-). They certainly
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stickers in the most unlikely places :-). They certainly visited the Totes
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visited the Totes Gebirge of Austria well before expeditionary caving abroad
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Gebirge of Austria well before expeditionary caving abroad became
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became commonplace.
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commonplace.</p>
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<p>From 1965 to 1969, the BEC held expeditions to Austria, in the first
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<p>From 1965 to 1969, the BEC held expeditions to Austria, in the first couple
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couple of years working with the Austrians in Raucherkarhöhle, then
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of years working with the Austrians in Raucherkarhöhle, then later doing
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later doing much work in the already known cave of
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much work in the already known cave of <a
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<a href="../../noinfo/1626/50.htm">Ahnenschacht</a>, on the slopes of
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href="../../noinfo/1626/50.htm">Ahnenschacht</a>, on the slopes of
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Schönberg, in the north of the western massif of the Totes Gebirge. This
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Schönberg, in the north of the western massif of the Totes Gebirge. This is
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is now a very major system, but even in 1967, it was a very serious
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now a very major system, but even in 1967, it was a very serious proposition,
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proposition, being remote, and with a very deep entrance shaft, which became
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being remote, and with a very deep entrance shaft, which became epic in the wet,
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epic in the wet, especially when tackled on ladders, as was the way in those
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especially when tackled on ladders, as was the way in those days.</p>
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days.
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<p>The BEC's explorations were reported in a series of articles in their
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<p>The BEC's explorations were reported in a series of articles in their
|
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frequent (then monthly) newsletter the <b>Belfry Bulletin</b>, as well as
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frequent (then monthly) newsletter the <b>Belfry Bulletin</b>, as well as in
|
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in other more widely available journals. Not all references in this list
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other more widely available journals. Not all references in this list have CTS
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have CTS numbers, as most are too early, and nobody seems inclined to
|
numbers, as most are too early, and nobody seems inclined to produce
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produce retrospective CTS volumes.
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retrospective CTS volumes.</p>
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<dl>
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<dl>
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<dt><dd><cite>Belfry Bulletin 214</cite>, <b>Dachstein/Hirlatz/Raucher/Koppenbrüller/Eisriesenwelt</b>
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<dd><cite>Belfry Bulletin 214</cite>,
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<dt><dd><cite>Belfry Bulletin 222</cite>, <b>Raucherkarhöhle</b>
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<b>Dachstein/Hirlatz/Raucher/Koppenbrüller/Eisriesenwelt</b></dd>
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<dt><dd><cite>Belfry Bulletin 237 pp 93-97</cite>, <b>Ahnenschacht 1967</b>
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<dd><cite>Belfry Bulletin 222</cite>,
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<dt><dd><cite>Belfry Bulletin 239 (Jan 1968) pp 23-26</cite>, <b>Scientific work on 1967 trip</b>
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<b>Raucherkarhöhle</b></dd>
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<dt><dd><cite>Belfry Bulletin 246 (Sep 1968) pp 130-138</cite>, <b>Ahnenschacht 1968</b>, Alan Thomas
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<dd><cite>Belfry Bulletin 237 pp 93-97</cite>, <b>Ahnenschacht 1967</b></dd>
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<dt><dd><cite>Belfry Bulletin 249 (Dec 1968) pp 198-204</cite>, <b>Drainage development in the Western Totes Gebirge</b>, Mike Luckwill
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<dd><cite>Belfry Bulletin 239 (Jan 1968) pp 23-26</cite>,
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<dt>69.708<dd><cite>Cave Research Group of G.B. Newsletter 116 (June 1969) pp 7-9</cite> <b>A brief account of the history of the Ahnenschacht</b>, A.R.Thomas.
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<b>Scientific work on 1967 trip</b></dd>
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<dt>69.709<dd><cite>Descent 5 (July 1969) pp 31-35</cite>, <b>British Team challenges Austria's Ahnenschacht</b>, A.R.Thomas.
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<dd><cite>Belfry Bulletin 246 (Sep 1968) pp 130-138</cite>,
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<dt>69.707<dd><cite>Mendip Caving Group Newsletter 77 (August 1969) pp 1-3</cite>, <b>Austria 1969</b>, Greg Smith
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<b>Ahnenschacht 1968</b>, Alan Thomas</dd>
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<dt>69.711<dd><cite>Belfry Bulletin 259, (Oct 1969) pp 169-170</cite>, <b>New Austrian discovery (near Feuertal Ice Cave)</b>, Dave Yeandle.
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<dd><cite>Belfry Bulletin 249 (Dec 1968) pp 198-204</cite>,
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<dt>69.704<dd><cite>Shepton Mallet Caving Club Newsletter 6(5) (Oct 1969) pp 65-70</cite>, <b>Ahnenschacht 1969 ... near Ebensee, Austria</b>, R.D.Craig
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<b>Drainage development in the Western Totes Gebirge</b>, Mike
|
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<dt>69.710<dd><cite>Belfry Bulletin 261 (Dec 1969) pp 200-203</cite>, <b>Ahnenschacht 1969</b>, A.R.Thomas.
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Luckwill</dd>
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<dt>69.704A<dd><cite>Shepton Mallet Caving Club Journal 4(8) (Dec 1969) pp 15-21</cite>, <b>Ahnenschacht 1969 ... near Ebensee, Austria</b>, R.D.Craig
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<dt>69.708</dt>
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<dd><cite>Cave Research Group of G.B. Newsletter 116 (June 1969) pp
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7-9</cite> <b>A brief account of the history of the
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Ahnenschacht</b>, A.R.Thomas.</dd>
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<dt>69.709</dt>
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<dd><cite>Descent 5 (July 1969) pp 31-35</cite>, <b>British Team
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challenges Austria's Ahnenschacht</b>, A.R.Thomas.</dd>
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<dt>69.707</dt>
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<dd><cite>Mendip Caving Group Newsletter 77 (August 1969) pp
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1-3</cite>, <b>Austria 1969</b>, Greg Smith</dd>
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<dt>69.711</dt>
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<dd><cite>Belfry Bulletin 259, (Oct 1969) pp 169-170</cite>, <b>New
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Austrian discovery (near Feuertal Ice Cave)</b>, Dave Yeandle.</dd>
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<dt>69.704</dt>
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<dd><cite>Shepton Mallet Caving Club Newsletter 6(5) (Oct 1969) pp
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65-70</cite>, <b>Ahnenschacht 1969 ... near Ebensee, Austria</b>,
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R.D.Craig</dd>
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<dt>69.710</dt>
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<dd><cite>Belfry Bulletin 261 (Dec 1969) pp 200-203</cite>,
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<b>Ahnenschacht 1969</b>, A.R.Thomas.</dd>
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<dt>69.704A</dt>
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<dd><cite>Shepton Mallet Caving Club Journal 4(8) (Dec 1969) pp
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15-21</cite>, <b>Ahnenschacht 1969 ... near Ebensee, Austria</b>,
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R.D.Craig</dd>
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</dl>
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</dl>
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<hr />
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<hr />
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||||||
<!-- LINKS -->
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<!-- LINKS -->
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||||||
<ul>
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<ul>
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||||||
<li><a href="../../indxal.htm">Index</a> of all caves documented in 1623.</li>
|
<li><a href="../../indxal.htm">Index</a> of all caves documented in
|
||||||
|
1623.</li>
|
||||||
<li><a href="../../areas.htm">Overview</a> of area 1623</li>
|
<li><a href="../../areas.htm">Overview</a> of area 1623</li>
|
||||||
<li><a href="../../1626/index.htm">Overview</a>
|
<li><a href="../../1626/index.htm">Overview</a> of area 1626, and
|
||||||
of area 1626, and index to caves</li>
|
index to caves</li>
|
||||||
<li>Back to <a href="../../index.htm">Expedition Intro page</a></li>
|
<li>Back to <a href="../../index.htm">Expedition Intro
|
||||||
|
page</a></li>
|
||||||
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
||||||
<li><a href="../index.htm">Other groups</a> who have worked in the area
|
<li><a href="../index.htm">Other groups</a> who have worked in the
|
||||||
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area</li>
|
||||||
</ul>
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</ul>
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</body>
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</body>
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</html>
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</html>
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@@ -1,62 +1,63 @@
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<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
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<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
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<html lang=fr>
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"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
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<html lang="fr" xmlns="http://www.w3.org/1999/xhtml" xml:lang="fr">
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<head>
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<head>
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||||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
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<meta http-equiv="Content-Type" content=
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||||||
<title>
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"text/html; charset=iso-8859-1" />
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||||||
GSAB: CTS ref. 78.2003
|
<title>GSAB: CTS ref. 78.2003</title>
|
||||||
</title>
|
<link rel="stylesheet" type="text/css" href=
|
||||||
<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
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"../../css/main2.css" />
|
||||||
</head>
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</head>
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||||||
<body>
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<body>
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||||||
<h1 lang=de>TRUNKEMBOLDSCHACHT</h1>
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<h1 lang="de" xml:lang="de">TRUNKEMBOLDSCHACHT</h1>
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<p lang="de" xml:lang="de" style="text-align: center">
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<p lang=de>Totes Gebirge West - Hintergras
|
Totes Gebirge West - Hintergras</p>
|
||||||
<p align=right>Jean-Pierre Braun
|
<p style="text-align: right"><b>Jean-Pierre Braun</b></p>
|
||||||
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<p><b>Profondeur</b> : -854m<br />
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<p><b>Profondeur </b>: -854m<br>
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<b>Altitude</b> : 1610m</p>
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<p><b>Historique</b> : découvert en Juillet 1976 par F
|
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<b>Altitude </b>: 1610m
|
Vergier, attiré par un fort courant d'air froid sortant
|
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d'une petite galerie. Exploration du 12 au 23 Juillet 1976 par
|
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<p><b>Historique </b>: découvert en Juillet 1976 par F Vergier,
|
l'A.C.Toulon ( li Aragnous ), Lou Darboun (Cavaillon) et
|
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attiré par un fort courant d'air froid sortant d'une petite galerie.
|
Spéléo Ragaie. Poursuite de l'exploration au mois
|
||||||
Exploration du 12 au 23 Juillet 1976 par l'A.C.Toulon ( li Aragnous ), Lou
|
d'Août 1977 par les même groupes et ces individuels de
|
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Darboun (Cavaillon) et Spéléo Ragaie. Poursuite de
|
la Tronche.</p>
|
||||||
l'exploration au mois d'Août 1977 par les même groupes et ces
|
<p><b>Description</b> : Depuis 1610m, altitude d l'entrée,
|
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individuels de la Tronche.
|
jusque -287m, rien pour engendrer l'enthusiasme, mais un courant
|
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d'air assez sensible. Le Gouffre est entrecoupé de
|
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<p><b>Description </b>: Depuis 1610m, altitude d l'entrée, jusque
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méandre étroits: P8, P12, P17, P9, P20, P3, P12, P30,
|
||||||
-287m, rien pour engendrer l'enthusiasme, mais un courant d'air assez
|
P7, P6, P9, P8, P7, P5, P34, P6, P8, P5, P9. A -287m, un P18 permet
|
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sensible. Le Gouffre est entrecoupé de méandre étroits:
|
de déboucher dans un grande salle. L'eau disparait dans les
|
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P8, P12, P17, P9, P20, P3, P12, P30, P7, P6, P9, P8, P7, P5, P34, P6, P8,
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éboulis pour réapparaître dans toute une
|
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P5, P9. A -287m, un P18 permet de déboucher dans un grande salle.
|
série de puits arrosés dont le plus profond mesure
|
||||||
L'eau disparait dans les éboulis pour réapparaître dans
|
30m. Les crues ont empéché l'exploration du fond de
|
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toute une série de puits arrosés dont le plus profond mesure
|
cette branche à -456m, un puits d'une vingtaine de
|
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30m. Les crues ont empéché l'exploration du fond de cette
|
mètre était vraiment trop arrosé pour
|
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branche <20> -456m, un puits d'une vingtaine de mètre était
|
être descendu. A -488m, un passage bas était aussi
|
||||||
vraiment trop arrosé pour être descendu. A -488m, un passage
|
trop humide. De plus, le courant d'air était faible ou nul.
|
||||||
bas était aussi trop humide. De plus, le courant d'air était
|
Dans la salle à -308m, une remontée d'une quinzaine
|
||||||
faible ou nul. Dans la salle à -308m, une remontée d'une
|
de mètres permet d'acceder à un méandre
|
||||||
quinzaine de mètres permet d'acceder à un méandre
|
fossile assez large ou souffle un sensible courant d'air. Au bout
|
||||||
fossile assez large ou souffle un sensible courant d'air. Au bout de 30m ce
|
de 30m ce méandre s'ouvre sur l'énorme puits des
|
||||||
méandre s'ouvre sur l'énorme puits des Naufragés,
|
Naufragés, P242m, d'une section moyennes de 15/25m !! Dans
|
||||||
P242m, d'une section moyennes de 15/25m !! Dans ce puits plusiers
|
ce puits plusiers arrivées d'eau venaient vraisemblement de
|
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arrivées d'eau venaient vraisemblement de la première branche
|
la première branche explorée. Le bas du puits se
|
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explorée. Le bas du puits se re...... un diaclase. L'explo 76
|
re...... un diaclase. L'explo 76 s'était arretée au
|
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s'était arretée au sommet d'un puits estimé à
|
sommet d'un puits estimé à 40m. Elle s'est poursuivie
|
||||||
40m. Elle s'est poursuivie en Août 77 pour aboutir au siphon dans deux
|
en Août 77 pour aboutir au siphon dans deux réseaux
|
||||||
réseaux différentes par P54, P88, P53, P25. Le fond du gouffre
|
différentes par P54, P88, P53, P25. Le fond du gouffre se
|
||||||
se trouve à -854m, donc à l'altitude 756m, niveau de la
|
trouve à -854m, donc à l'altitude 756m, niveau de la
|
||||||
vallée.
|
vallée.</p>
|
||||||
<hr />
|
<hr />
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<p lang=en>
|
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="index.htm">GSAB articles list</a></li>
|
<li><a href="index.htm">GSAB articles list</a></li>
|
||||||
<li>Trunkemboldschacht :
|
<li>Trunkemboldschacht : <a href=
|
||||||
<a href="../../noinfo/1626/117.htm">description</a>, in English</li>
|
"../../noinfo/1626/117.htm">description</a>, in English</li>
|
||||||
<li><a href="../../1626/index.htm">Overview</a>
|
<li><a href="../../1626/index.htm">Overview</a> of area 1626, and
|
||||||
of area 1626, and index to caves</li>
|
index to caves</li>
|
||||||
<li>Back to <a href="../../index.htm">Expedition Intro page</a></li>
|
<li>Back to <a href="../../index.htm">Expedition Intro
|
||||||
|
page</a></li>
|
||||||
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
|
|||||||
@@ -1,69 +1,71 @@
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<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
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<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
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<html lang="fr">
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"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
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||||||
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<html lang="fr" xmlns="http://www.w3.org/1999/xhtml" xml:lang="fr">
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||||||
<head>
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<head>
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||||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
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<meta http-equiv="Content-Type" content=
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||||||
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"text/html; charset=iso-8859-1" />
|
||||||
<title>GSAB: CTS ref. 78.2013</title>
|
<title>GSAB: CTS ref. 78.2013</title>
|
||||||
<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
|
<link rel="stylesheet" type="text/css" href=
|
||||||
|
"../../css/main2.css" />
|
||||||
</head>
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</head>
|
||||||
<body>
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<body>
|
||||||
<h1 lang="de">FEUERTALSYSTEM</h1>
|
<h1 lang="de" xml:lang="de">FEUERTALSYSTEM</h1>
|
||||||
|
<p lang="de" xml:lang="de" style="text-align: center">Totes Gebirge West -
|
||||||
<p lang="de">Totes Gebirge West - Feuertal - Schönberg
|
Feuertal - Schönberg</p>
|
||||||
|
<p><b>Profondeur</b> : -913m<br />
|
||||||
<p><b>Profondeur </b>: -913m<br>
|
<b>Altitude</b> : 1950m</p>
|
||||||
|
<p><b>Historique</b> : connu dès 1973 par les GSAB, mais non
|
||||||
<b>Altitude </b>: 1950m
|
|
||||||
|
|
||||||
<p><b>Historique </b>: connu dès 1973 par les GSAB, mais non
|
|
||||||
exploré !!!!!!!! Exploré en 76 et 77 par Lou Barboun,
|
exploré !!!!!!!! Exploré en 76 et 77 par Lou Barboun,
|
||||||
A.C.Toulon, S.C.Toulon et Spéléo Ragaie.
|
A.C.Toulon, S.C.Toulon et Spéléo Ragaie.</p>
|
||||||
|
<p><b>Description</b> : voir <a href="fr/782012.htm">Spéalp
|
||||||
<p><b>Description </b>: voir <a href="fr/782012.htm">Spéalp no. 1</a>.
|
no. 1</a>. Apartir de -700m, suite de petits puits jusqu'a -854m ou
|
||||||
Apartir de -700m, suite de petits puits jusqu'a -854m ou des conduites
|
des conduites forcées mènent après quatre
|
||||||
forcées mènent après quatre puits à un siphon.
|
puits à un siphon. Cote -913m.</p>
|
||||||
Cote -913m.
|
|
||||||
|
|
||||||
<p>A la cote -500m, une grande galerie fossile a été
|
<p>A la cote -500m, une grande galerie fossile a été
|
||||||
explorée sur 2 km et se direige vers l'énorme réseau du
|
explorée sur 2 km et se direige vers l'énorme
|
||||||
<span lang="de"><a href="../../noinfo/1626/55.htm">Raucherkarhöhle</a></span>
|
réseau du <span lang="de" xml:lang="de"><a href=
|
||||||
(voir Spéalp no. 1). Un puits de 211m a été
|
"../../noinfo/1626/55.htm">Raucherkarhöhle</a></span> (voir
|
||||||
|
Spéalp no. 1). Un puits de 211m a été
|
||||||
exploré, au bout de celle-ci, mais ne donne rien. La galerie
|
exploré, au bout de celle-ci, mais ne donne rien. La galerie
|
||||||
continuerait en face ! Une jonction donnerait le profondeur de -1031m.
|
continuerait en face ! Une jonction donnerait le profondeur de
|
||||||
|
-1031m.</p>
|
||||||
<p>La prospection en surface a permis de trouver deux nouvelles
|
<p>La prospection en surface a permis de trouver deux nouvelles
|
||||||
entrées: le "Velo Tracteur", 1779m d'altitude et le "Carcajau" 1735m
|
entrées: le "Velo Tracteur", 1779m d'altitude et le
|
||||||
qui donnent tout les deux dans la grande galerie fossile.
|
"Carcajau" 1735m qui donnent tout les deux dans la grande galerie
|
||||||
|
fossile.</p>
|
||||||
<p>Ce gouffre n'est pas terminé et nous y verons probablement une
|
<p>Ce gouffre n'est pas terminé et nous y verons
|
||||||
équipe cette année.
|
probablement une équipe cette année.</p>
|
||||||
|
<p>J.C.Hans <acronym>GSAB</acronym></p>
|
||||||
<p>J.C.Hans <acronym>GSAB</acronym>
|
<h2><span lang="de" xml:lang="de">TOTES GEBIRGE WEST</span> ou
|
||||||
|
l'EXPLOSION</h2>
|
||||||
<h2><span lang="de">TOTES GEBIRGE WEST</span> ou l'EXPLOSION</h2>
|
<p>-913, -854, -607, -565, le tout à moins de 2km de
|
||||||
|
distance ! C'est en effet les cotes atteintes par les
|
||||||
<p>-913, -854, -607, -565, le tout à moins de 2km de distance ! C'est
|
Français au gouffre Quelli ou <span lang="de" xml:lang=
|
||||||
en effet les cotes atteintes par les Fran<61>ais au gouffre Quelli ou
|
"de">Feuertal</span>, au <span lang="de" xml:lang=
|
||||||
<span lang="de">Feuertal</span>, au <span lang="de">Trunkemboldschacht</span>
|
"de">Trunkemboldschacht</span> et par nous au Gouffre Ovni, et dans
|
||||||
et par nous au Gouffre Ovni, et dans une nouvelle branche de
|
une nouvelle branche de l'<span lang="de" xml:lang=
|
||||||
l'<span lang="de">Ahnenschacht</span>. Pour tout ces gouffres voir les
|
"de">Ahnenschacht</span>. Pour tout ces gouffres voir les
|
||||||
rensiegnements dans ce no. Nous avons reporté l'article sur
|
rensiegnements dans ce no. Nous avons reporté l'article sur
|
||||||
l'<span lang="de">Ahnenschacht</span> au prochain numéro, car une
|
l'<span lang="de" xml:lang="de">Ahnenschacht</span> au prochain
|
||||||
tentative de jonction va être réalisée par une Interclub
|
numéro, car une tentative de jonction va être
|
||||||
fin Juin et nous préférons attendre les résultats
|
réalisée par une Interclub fin Juin et nous
|
||||||
plutôt que de publier plusieurs fois les même topos.
|
préférons attendre les résultats plutôt
|
||||||
|
que de publier plusieurs fois les même topos.</p>
|
||||||
<p>J.C.Hans
|
<p>J.C.Hans</p>
|
||||||
<hr />
|
<hr />
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<p lang=en>
|
<p lang="en" xml:lang="en"> </p>
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="index.htm"><acronym>GSAB</acronym> articles list</a></li>
|
<li><a href="index.htm"><acronym>GSAB</acronym> articles
|
||||||
<li>Feuertalsystem :
|
list</a></li>
|
||||||
<a href="../../noinfo/1626/120.htm">description</a>, in English</li>
|
<li>Feuertalsystem : <a href=
|
||||||
<li><a href="../../1626/index.htm">Overview</a>
|
"../../noinfo/1626/120.htm">description</a>, in English</li>
|
||||||
of area 1626, and index to caves</li>
|
<li><a href="../../1626/index.htm">Overview</a> of area 1626, and
|
||||||
<li>Back to <a href="../../index.htm">Expedition Intro page</a></li>
|
index to caves</li>
|
||||||
<li><a href="../../../index.htm">Back to <acronym>CUCC</acronym> Home page</a></li>
|
<li>Back to <a href="../../index.htm">Expedition Intro
|
||||||
|
page</a></li>
|
||||||
|
<li><a href="../../../index.htm">Back to <acronym>CUCC</acronym>
|
||||||
|
Home page</a></li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
</html>
|
</html>
|
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|
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@@ -1,216 +1,205 @@
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<head><meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
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<meta http-equiv="Content-Type" content=
|
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"text/html; charset=iso-8859-1" />
|
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<title>GSAB: CTS ref. 78.2008 (in English translation)</title>
|
<title>GSAB: CTS ref. 78.2008 (in English translation)</title>
|
||||||
<LINK rel="alternate" lang="fr" href="../fr/782008.htm"
|
<link rel="alternate" lang="fr" href="../fr/782008.htm" title=
|
||||||
title="Gouffre Ovni">
|
"Gouffre Ovni" xml:lang="fr" />
|
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<link rel="stylesheet" type="text/css" href="../../../css/main2.css" />
|
<link rel="stylesheet" type="text/css" href=
|
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|
"../../../css/main2.css" />
|
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</head>
|
</head>
|
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<body>
|
<body>
|
||||||
<center><font size=-1>(<acronym>GSAB</acronym>) <b lang="fr">Spéalp</b> 2 (1978) pp 14-19</font>
|
<p style="text-align: center; font-size: 65%">
|
||||||
<h1 lang="fr">GOUFFRE OVNI</h1></center>
|
(<acronym>GSAB</acronym>) <b lang="fr"
|
||||||
|
xml:lang="fr">Spéalp</b> 2 (1978) pp 14-19</p>
|
||||||
<p>The summer <acronym>GSAB</acronym> expedition to the <span lang="de">Totes
|
<h1 lang="fr" xml:lang="fr">GOUFFRE OVNI</h1>
|
||||||
Gebirge</span> has allowed the exploration of this new cave of 565m depth.
|
|
||||||
Certainly, it is a little eclipsed by its two neighbours
|
|
||||||
(<b lang="de">Kelli</b> and <b lang="fr">Empégadure</b>) but it
|
|
||||||
remains no less of an accomplishment for a young team, only just broken into
|
|
||||||
their first large-scale trip.
|
|
||||||
|
|
||||||
|
<p>The summer <acronym>GSAB</acronym> expedition to the <span lang=
|
||||||
|
"de" xml:lang="de">Totes Gebirge</span> has allowed the exploration
|
||||||
|
of this new cave of 565m depth. Certainly, it is a little eclipsed
|
||||||
|
by its two neighbours (<b lang="de" xml:lang="de">Kelli</b> and
|
||||||
|
<b lang="fr" xml:lang="fr">Empégadure</b>) but it remains no
|
||||||
|
less of an accomplishment for a young team, only just broken into
|
||||||
|
their first large-scale trip.</p>
|
||||||
<p>For the location and discovery details, see the report in
|
<p>For the location and discovery details, see the report in
|
||||||
<b lang="fr">Spéalp</b> <acronym>GSAB-SSS</acronym>
|
<b lang="fr" xml:lang="fr">Spéalp</b>
|
||||||
<a href="782012.htm">number 1</a>.
|
<acronym>GSAB-SSS</acronym> <a href="782012.htm">number 1</a>.</p>
|
||||||
|
|
||||||
<h2>Description</h2>
|
<h2>Description</h2>
|
||||||
|
<p>The entrance, a bedding plane unblocked because of a draught,
|
||||||
<p>The entrance, a bedding plane unblocked because of a draught, gives access
|
gives access to a series of short pitches, dry at the start, which
|
||||||
to a series of short pitches, dry at the start, which get bigger, deeper,
|
get bigger, deeper, wider and wetter. The first exploration of 1976
|
||||||
wider and wetter. The first exploration of 1976 had reconnoitred to -200m to
|
had reconnoitred to -200m to the base of a 40m pitch (<b>The Black
|
||||||
the base of a 40m pitch (<b>The Black Hole</b>). The explorers of this year
|
Hole</b>). The explorers of this year started on the descent of a
|
||||||
started on the descent of a fine 60m pitch of constant shape, slightly
|
fine 60m pitch of constant shape, slightly sloping. At the bottom
|
||||||
sloping. At the bottom of this is the only chamber of the cave : <b>The
|
of this is the only chamber of the cave : <b>The Galactic Hall</b>.
|
||||||
Galactic Hall</b>. Here the cave splits into two routes, the active and the
|
Here the cave splits into two routes, the active and the
|
||||||
fossil.
|
fossil.</p>
|
||||||
|
|
||||||
<h3>Active system</h3>
|
<h3>Active system</h3>
|
||||||
|
<p>Downstream from the chamber a drop leads to a small chamber
|
||||||
<p>Downstream from the chamber a drop leads to a small chamber among
|
among boulders, the <b>Love Nest</b>. (No idea who ventured to call
|
||||||
boulders, the <b>Love Nest</b>. (No idea who ventured to call it this[?])
|
it this[?]) Between the boulders a 20m pitch opens, immediately
|
||||||
Between the boulders a 20m pitch opens, immediately followed by a 25m pitch.
|
followed by a 25m pitch. In fact, the last 25m of descent drops
|
||||||
In fact, the last 25m of descent drops between the walls of an immense aven
|
between the walls of an immense aven to land on a flat gravel
|
||||||
to land on a flat gravel floor. A diagonal chimney leads to a trickle of
|
floor. A diagonal chimney leads to a trickle of water.</p>
|
||||||
water.
|
<p>A fissure marks the start of the <b>Anti-matter meander</b>,
|
||||||
|
where one immediately rejoins the underground stream. This has an
|
||||||
<p>A fissure marks the start of the <b>Anti-matter meander</b>, where one
|
average flow of two litres per second but quite rapidly increases
|
||||||
immediately rejoins the underground stream. This has an average flow of two
|
to 10-15 litres per second in flood. The first part of the meander
|
||||||
litres per second but quite rapidly increases to 10-15 litres per second in
|
is straight and interrupted by 3 small pitches and two drops. At
|
||||||
flood. The first part of the meander is straight and interrupted by 3 small
|
the top of the first, in the roof, is the connection with the
|
||||||
pitches and two drops. At the top of the first, in the roof, is the
|
fossil system. Quickly, the meander becomes less amenable: high and
|
||||||
connection with the fossil system. Quickly, the meander becomes less
|
narrow, it is plastered with mud (the anti-matter) which makes
|
||||||
amenable: high and narrow, it is plastered with mud (the anti-matter) which
|
progress quite arduous. Three pitches of 5, 14 and 10, punctuate
|
||||||
makes progress quite arduous. Three pitches of 5, 14 and 10, punctuate
|
progress. This last, followed by a drop of 3m, gives access to a
|
||||||
progress. This last, followed by a drop of 3m, gives access to a section of
|
section of passage blocked by clay. At the end of this, the stream
|
||||||
passage blocked by clay. At the end of this, the stream disappers into a
|
disappers into a fissure with tight impenetrable bends. The passage
|
||||||
fissure with tight impenetrable bends. The passage is continued by a quite
|
is continued by a quite large fossil branch. After some 50m, the
|
||||||
large fossil branch. After some 50m, the draught goes into an earthy hole,
|
draught goes into an earthy hole, the start of a big pitch of 70m
|
||||||
the start of a big pitch of 70m in several stages.
|
in several stages.</p>
|
||||||
|
<p>Halfway down, the pitch is rejoined by the stream which is
|
||||||
<p>Halfway down, the pitch is rejoined by the stream which is avoided by a
|
avoided by a parallel fossil pitch. There immediately follows
|
||||||
parallel fossil pitch. There immediately follows another pitch of 55m,
|
another pitch of 55m, totally wet and characterised by an
|
||||||
totally wet and characterised by an elliptical cross-section and constant
|
elliptical cross-section and constant slope. At the bottom, the
|
||||||
slope. At the bottom, the water is engulfed by a fissure about three metres
|
water is engulfed by a fissure about three metres long, followed by
|
||||||
long, followed by a tight meander which we haven't pushed.
|
a tight meander which we haven't pushed.</p>
|
||||||
|
|
||||||
<h3>Fossil system</h3>
|
<h3>Fossil system</h3>
|
||||||
|
<p>Upstream from the Galactic Hall, a window some metres high gives
|
||||||
<p>Upstream from the Galactic Hall, a window some metres high gives access to
|
access to a good-sized passage (3x3m on average), the <b>Little
|
||||||
a good-sized passage (3x3m on average), the <b>Little Green Men's
|
Green Men's passage</b>. One comes up against a climb of 3m at the
|
||||||
passage</b>. One comes up against a climb of 3m at the base of which the
|
base of which the trickle of water is lost into a meander cut below
|
||||||
trickle of water is lost into a meander cut below the fossil passage (see
|
the fossil passage (see below). After a narrowing and a climb, the
|
||||||
below). After a narrowing and a climb, the passage ends in boulders between
|
passage ends in boulders between which it is still possible to
|
||||||
which it is still possible to penetrate for a dozen metres.
|
penetrate for a dozen metres.</p>
|
||||||
|
|
||||||
<p>Back in the meander below the fossil passage: this ends at the
|
<p>Back in the meander below the fossil passage: this ends at the
|
||||||
<b><span lang="fr">Gomette</span> pitch</b> (discovered by the <span
|
<b><span lang="fr" xml:lang="fr">Gomette</span> pitch</b>
|
||||||
lang="fr">Gaumais</span>), a 60m pitch, spray-lashed in its lower part by
|
(discovered by the <span lang="fr" xml:lang="fr">Gaumais</span>), a
|
||||||
"the wee-wee". At the base of this pitch is the beginning of the <b>Mutants'
|
60m pitch, spray-lashed in its lower part by "the wee-wee". At the
|
||||||
meander</b>. This is a passage for masochists <span lang="fr">par
|
base of this pitch is the beginning of the <b>Mutants' meander</b>.
|
||||||
excellence</span>: at the bottom, tight and suit-snagging. It ends in a
|
This is a passage for masochists <span lang="fr" xml:lang="fr">par
|
||||||
series of climbs and a 30m pitch joining the active system.
|
excellence</span>: at the bottom, tight and suit-snagging. It ends
|
||||||
|
in a series of climbs and a 30m pitch joining the active
|
||||||
|
system.</p>
|
||||||
<h2>Geology</h2>
|
<h2>Geology</h2>
|
||||||
|
|
||||||
<h3>General</h3>
|
<h3>General</h3>
|
||||||
|
<p>From the geological point of view, the <span lang="fr" xml:lang=
|
||||||
<p>From the geological point of view, the <span lang="fr">Gouffre Ovni</span>
|
"fr">Gouffre Ovni</span> is a typical example of the karstic
|
||||||
is a typical example of the karstic phenomena of the massif, and likewise of
|
phenomena of the massif, and likewise of the greater part of the
|
||||||
the greater part of the karst of Austria. There isn't a zone of pitches
|
karst of Austria. There isn't a zone of pitches leading to a
|
||||||
leading to a master-cave on an impermeable bed (of the Pyrenean type) nor
|
master-cave on an impermeable bed (of the Pyrenean type) nor tight
|
||||||
tight vertical caves (of the <span lang="fr">Vercors</span> or <span
|
vertical caves (of the <span lang="fr" xml:lang="fr">Vercors</span>
|
||||||
lang="fr">Chartreuse</span> type). The primary factors in the formation are
|
or <span lang="fr" xml:lang="fr">Chartreuse</span> type). The
|
||||||
the intense orogenic fracturing combined with a very wet climate and heavy
|
primary factors in the formation are the intense orogenic
|
||||||
snow-falls since the start of the era.
|
fracturing combined with a very wet climate and heavy snow-falls
|
||||||
|
since the start of the era.</p>
|
||||||
<p>These caves generally open by virtue of the simple form of the
|
<p>These caves generally open by virtue of the simple form of the
|
||||||
discontinuities in the limestones (joints, bedding-planes). Then they enlarge
|
discontinuities in the limestones (joints, bedding-planes). Then
|
||||||
more and more by following the larger-scale phenomena (faults,
|
they enlarge more and more by following the larger-scale phenomena
|
||||||
master-joints). The master-cave, when it exists, is generally only short and
|
(faults, master-joints). The master-cave, when it exists, is
|
||||||
near the resurgence.
|
generally only short and near the resurgence.</p>
|
||||||
|
<h3 lang="fr" xml:lang="fr">Gouffre Ovni</h3>
|
||||||
<h3 lang="fr">Gouffre Ovni</h3>
|
<p>The entrance is in a bedding plane open for about two metres.
|
||||||
|
There follows a series of pitches, quite small, formed in a quite
|
||||||
<p>The entrance is in a bedding plane open for about two metres. There
|
sinuous joint and enlarged on bedding planes and very strong
|
||||||
follows a series of pitches, quite small, formed in a quite sinuous joint and
|
[<span lang="fr" xml:lang="fr">pendage</span> - dictionary failure]
|
||||||
enlarged on bedding planes and very strong [<span lang="fr">pendage</span> -
|
in this zone. At about -200m, the influence of another factor
|
||||||
dictionary failure] in this zone. At about -200m, the influence of another
|
starts to be felt. The pitches become bigger and bigger and the
|
||||||
factor starts to be felt. The pitches become bigger and bigger and the walls
|
walls cleaner and cleaner. This section is characterised by a fault
|
||||||
cleaner and cleaner. This section is characterised by a fault running roughly
|
running roughly East-West (see figure 1).</p>
|
||||||
East-West (see figure 1).
|
<div class="centre"><img alt="fig. 1, 3k gif" width="512" height="128" src=
|
||||||
|
"../ovnif1.png" /></div>
|
||||||
<p><center><img alt="fig. 1, 3k gif" width=512 height=128
|
<p>This fault controls the major part of the formation of the cave.
|
||||||
src="../ovnif1.png"></center>
|
In effect, the course of the cave is hollowed out of different
|
||||||
|
levels of this fault. (figure 2)</p>
|
||||||
<p>This fault controls the major part of the formation of the cave. In
|
<div class="onleft">
|
||||||
effect, the course of the cave is hollowed out of different levels of this
|
<img alt="fig. 2, 3k gif" width="275" height="385" src="../ovnif2.png" />
|
||||||
fault. (figure 2)
|
<p class="caption"><b>Figure 2: Plan of
|
||||||
|
the fault</b></p></div>
|
||||||
<p><img alt="fig. 2, 3k gif" width=275 height=385 align="left" hspace=10
|
|
||||||
vspace=10 src="../ovnif2.png">
|
|
||||||
|
|
||||||
<b>Figure 2: Plan of the fault</b>
|
|
||||||
|
|
||||||
<ul>
|
<ul>
|
||||||
<li>1st The Zorglub pitch and the Father Christmas chimneys.
|
<li>1st The Zorglub pitch and the Father Christmas chimneys.</li>
|
||||||
|
<li>2nd The Galactic Hall and the first third of the Little Green
|
||||||
<li>2nd The Galactic Hall and the first third of the Little Green Men's
|
Men's passage (the other two thirds lie on bedding planes).</li>
|
||||||
passage (the other two thirds lie on bedding planes).
|
<li>3rd The pitch to pass [?] the time and the <span lang="fr"
|
||||||
|
xml:lang="fr">Gaumette</span> pitch with the Mutants' meander.</li>
|
||||||
<li>3rd The pitch to pass [?] the time and the
|
<li>4th The major part of the Anti-matter meander (the unwedging of
|
||||||
<span lang="fr">Gaumette</span> pitch with the Mutants' meander.
|
this part [?]) by connection with the rest (plan) is [complete
|
||||||
|
translation failure - something about the fault being broken
|
||||||
<li>4th The major part of the Anti-matter meander (the unwedging of this
|
?]</li>
|
||||||
part [?]) by connection with the rest (plan) is [complete translation
|
|
||||||
failure - something about the fault being broken ?]
|
|
||||||
|
|
||||||
</ul>
|
</ul>
|
||||||
<br clear="all">
|
<p style="clear: both">Following the large part of the Anti-matter meander, a
|
||||||
|
very narrow zone marks the junction with a second fault orientated
|
||||||
<p>Following the large part of the Anti-matter meander, a very narrow zone
|
<acronym>SE-NW</acronym> which controls the rest of the cave. [next sentence is
|
||||||
marks the junction with a second fault orientated <acronym>SE-NW</acronym>
|
real gobbledegook to me unless there is a misprint in the french ?] One rotted
|
||||||
which controls the rest of the cave. [next sentence is real gobbledegook to
|
to believe conspicuously the survey, which concerns a meander in a joint seen
|
||||||
me unless there is a misprint in the french ?] One rotted to believe
|
its sinuosity [???]. In fact, the straight part and space of this fault is
|
||||||
conspicuously the survey, which concerns a meander in a joint seen its
|
impracticable because it overhangs continually a perpendicular of 6m whence the
|
||||||
sinuosity [???]. In fact, the straight part and space of this fault is
|
lips are sloping and muddy. One is therefore obliged to borrow the bottom in
|
||||||
impracticable because it overhangs continually a perpendicular of 6m whence
|
[<span lang="fr" xml:lang="fr">surcreusement</span> - what a time for a
|
||||||
the lips are sloping and muddy. One is therefore obliged to borrow the bottom
|
dictionary failure !]. More unwavering [lots of alternative translations for
|
||||||
in [<span lang="fr">surcreusement</span> - what a time for a dictionary
|
this word - none make much sense] by an unhooking where the stream destroys
|
||||||
failure !]. More unwavering [lots of alternative translations for this word -
|
itself [sinks ?]. The passage continues in the same direction always controlled
|
||||||
none make much sense] by an unhooking where the stream destroys itself [sinks
|
by the jointing/faulting. The zone of pitches which follows develops equally
|
||||||
?]. The passage continues in the same direction always controlled by the
|
in the lower part of the fault; [<span lang="fr" xml:lang="fr">elle ait</span>
|
||||||
jointing/faulting. The zone of pitches which follows develops equally in the
|
is the present subjunctive of <span lang="fr" xml:lang= "fr">avoir</span> -
|
||||||
lower part of the fault; [<span lang="fr">elle ait</span> is the present
|
what the fuck does present subjunctive translate as ?] well what/as/who/as/how
|
||||||
subjunctive of <span lang="fr">avoir</span> - what the fuck does present
|
has the appearance of a forced conduit [phreatic passage/lift ?]</p>
|
||||||
subjunctive translate as ?] well what/as/who/as/how has the appearance of a
|
|
||||||
forced conduit [phreatic passage/lift ?]
|
|
||||||
|
|
||||||
<h3>Possibilities for continuation</h3>
|
<h3>Possibilities for continuation</h3>
|
||||||
|
<p>As one the remark to the observation of the survey, the main
|
||||||
<p>As one the remark to the observation of the survey, the main passage
|
passage continues unexplored. It appears that [present subjunctive
|
||||||
continues unexplored. It appears that [present subjunctive of to be] in the
|
of to be] in the presence of a simple phenomenon of regression and
|
||||||
presence of a simple phenomenon of regression and so logically one should
|
so logically one should find another series of fossil pitches
|
||||||
find another series of fossil pitches dropping to the base level. (figures 3
|
dropping to the base level. (figures 3 and 4)</p>
|
||||||
and 4)
|
<div class="center">
|
||||||
|
<img alt="Fig. 3 - 5k gif" style="border: 2px solid black" width="460" height="480" src=
|
||||||
<center><p><img alt="Fig. 3 - 5k gif" width=460 height=480
|
"ovnif3.png" />
|
||||||
src="ovnif3.png"><p><img alt="Fig. 4 - 3k gif" width=320 height=340
|
<img style="border: 2px solid black" alt="Fig. 4 - 3k gif" width="320" height="340" src=
|
||||||
src="ovnif4.png"></center>
|
"ovnif4.png" />
|
||||||
|
</div>
|
||||||
<p>The strength [power, force ?] of the <span lang="de">Dachsteinkalk</span>
|
<p>The strength [power, force ?] of the <span lang="de" xml:lang=
|
||||||
(granular Jurassic limestone) lies next to the 700m from the entrance. [??]
|
"de">Dachsteinkalk</span> (granular Jurassic limestone) lies next
|
||||||
|
to the 700m from the entrance. [??]</p>
|
||||||
<h3>Meteorologie</h3>
|
<h3>Meteorologie</h3>
|
||||||
|
<div class="onright">
|
||||||
<p><img alt="fig. 5 - 2k gif" width=265 height=435 align=right hspace=10
|
<img alt="fig. 5 - 2k gif" width="265" height="435"
|
||||||
vspace=0 src="../ovnif5.png">
|
src="../ovnif5.png" /> <p class="caption"><b>Figure 5:
|
||||||
<b>Figure 5: Diagram of the draughts at the principal points of
|
Diagram of the draughts at the principal points of
|
||||||
perception:</b>
|
perception:</b></p></div>
|
||||||
|
<p>As we have already said, there is a strong draught which drew
|
||||||
<p>As we have already said, there is a strong draught which drew our
|
our attention to Ovni. This draught was blowing in a hot period
|
||||||
attention to Ovni. This draught was blowing in a hot period (summer) [so] we
|
(summer) [so] we logically [expected] to find the presence of an
|
||||||
logically [expected] to find the presence of an intermediate entrance. Seeing
|
intermediate entrance. Seeing the strength of the cold draught
|
||||||
the strength of the cold draught [<span lang="fr">chassé</span>], the
|
[<span lang="fr" xml:lang="fr">chassé</span>], the existence
|
||||||
existence of an upper entrance is fairly certain. Prospecting on the hillock
|
of an upper entrance is fairly certain. Prospecting on the hillock
|
||||||
above the entrance didn't yield results. It concerns there of an objective to
|
above the entrance didn't yield results. It concerns there of an
|
||||||
see again because the vegetation and the snakes didn't permit us to operate
|
objective to see again because the vegetation and the snakes didn't
|
||||||
an efficient search pattern.
|
permit us to operate an efficient search pattern.</p>
|
||||||
|
<p>The junction with this higher entrance must be at the level of
|
||||||
<p>The junction with this higher entrance must be at the level of the Little
|
the Little Green Men's passage; either by the wet chimney at the
|
||||||
Green Men's passage; either by the wet chimney at the bottom of the 1st fault
|
bottom of the 1st fault or in the roof of 2/3, there where the
|
||||||
or in the roof of 2/3, there where the draught is lost. For the other part,
|
draught is lost. For the other part, the presence at the bottom of
|
||||||
the presence at the bottom of another strong draught, suggests a lower
|
another strong draught, suggests a lower entrance, probably a
|
||||||
entrance, probably a fossil resurgence. Nevertheless these are only
|
fossil resurgence. Nevertheless these are only suppositions, the
|
||||||
suppositions, the caprices of a draught are very difficult to deal with.
|
caprices of a draught are very difficult to deal with.</p>
|
||||||
|
<h3 style="clear: both">Conclusions</h3>
|
||||||
<br clear="all">
|
<p>One sees from this brief analysis of the cave that the chances
|
||||||
|
of a continuation aren't minimal. Now this cave isn't extremely
|
||||||
<h3>Conclusions</h3>
|
difficult of access or of exploration. The work [god knows - rotted
|
||||||
|
to be there mend] very soon, but it is nevertheless a secondary
|
||||||
<p>One sees from this brief analysis of the cave that the chances of a
|
objective compared with other Austrian possibilities.</p>
|
||||||
continuation aren't minimal. Now this cave isn't extremely difficult of
|
<p lang="fr" xml:lang="fr">G Feller <acronym>GSAB</acronym></p>
|
||||||
access or of exploration. The work [god knows - rotted to be there mend] very
|
|
||||||
soon, but it is nevertheless a secondary objective compared with other
|
|
||||||
Austrian possibilities.
|
|
||||||
|
|
||||||
<p lang="fr">G Feller <acronym>GSAB</acronym>
|
|
||||||
<hr />
|
<hr />
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="../index.htm">GSAB articles list</a></li>
|
<li><a href="../index.htm">GSAB articles list</a></li>
|
||||||
<li><span lang="fr">Gouffre Ovni</span> :
|
<li><span lang="fr" xml:lang="fr">Gouffre Ovni</span> : <a href=
|
||||||
<a href="../../../noinfo/1626/122.htm">description</a>, in English</li>
|
"../../../noinfo/1626/122.htm">description</a>, in English</li>
|
||||||
<li><a href="../../../1626/index.htm">Overview</a>
|
<li><a href="../../../1626/index.htm">Overview</a> of area 1626,
|
||||||
of area 1626, and index to caves</li>
|
and index to caves</li>
|
||||||
<li>Back to <a href="../../../index.htm">Expedition Intro page</a></li>
|
<li>Back to <a href="../../../index.htm">Expedition Intro
|
||||||
|
page</a></li>
|
||||||
<li><a href="../../../../index.htm">Back to CUCC Home page</a></li>
|
<li><a href="../../../../index.htm">Back to CUCC Home page</a></li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
|
|||||||
@@ -1,370 +1,361 @@
|
|||||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
|
||||||
<html>
|
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
||||||
|
<html xmlns="http://www.w3.org/1999/xhtml">
|
||||||
<head>
|
<head>
|
||||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
<meta http-equiv="Content-Type" content= "text/html; charset=iso-8859-1" />
|
||||||
<title>
|
<title>GSAB: CTS ref. 78.2012 (in English translation)</title>
|
||||||
GSAB: CTS ref. 78.2012 (in English translation)
|
<link rel="alternate" lang="fr" href="../fr/782012.htm" title="Description des principaux gouffres de la zone ouest du massif" xml:lang="fr" />
|
||||||
</title>
|
<link rel="stylesheet" type="text/css" href= "../../../css/main2.css" />
|
||||||
<LINK rel="alternate" lang="fr" href="../fr/782012.htm"
|
|
||||||
title="Description des principaux gouffres de la zone ouest du massif">
|
|
||||||
<link rel="stylesheet" type="text/css" href="../../../css/main2.css" />
|
|
||||||
</head>
|
</head>
|
||||||
<body>
|
<body>
|
||||||
<center><font size=-1 lang="fr">(<acronym>GSAB</acronym>) Spéalp 1
|
<p style="text-align: center; font-size: 65%" lang="fr" xml:lang= "fr">(<acronym>GSAB</acronym>) Spéalp 1 (Juin 1977) pp 33-49</p>
|
||||||
(Juin 1977) pp 33-49</font>
|
<h1 lang="de" xml:lang="de">TOTES GEBIRGE</h1>
|
||||||
|
<h2 style="text-align: center">Description of the principal caves in the West of the massif.</h2>
|
||||||
<h1 lang="de">TOTES GEBIRGE</h1>
|
|
||||||
|
|
||||||
<h2>Description of the principal caves in the West of the massif.</h2></center>
|
|
||||||
|
|
||||||
<p><b>Introduction</b> : The choice of this area was quite arbitrary. Indeed,
|
|
||||||
there is very little chance that the area is all drained by the same
|
|
||||||
hydrological system. While for some caves, the presumed resurgence is almost
|
|
||||||
certain, the same is not true of others which may drain in totally the
|
|
||||||
opposite direction ! Our choice was governed by means of access: roads, gear
|
|
||||||
lift, paths, a refuge etc.. The <span lang="de">Totes Gebirge</span>, which
|
|
||||||
is one of the biggest karst ranges in Austria, is only easily accessible in
|
|
||||||
certain areas, such as the one we discuss in this article. In this area are
|
|
||||||
many kilometres of totally virgin lapiaz. Many hours walking are needed to
|
|
||||||
reach it. Moreover, in this area, only a tiny part is more-or-less
|
|
||||||
prospected. It includes the valleys of <span lang="de">Raucherkar</span> and
|
|
||||||
<span lang="de">Feuertal</span>, and the areas adjoining the path which goes
|
|
||||||
to them as well as the north face of <span lang="de">Hagender Kogel</span>,
|
|
||||||
in which lies the <span lang="de">Tropfsteinhöhle</span>, which had
|
|
||||||
extraordinary formations but which is today completely trashed out.
|
|
||||||
|
|
||||||
<p><b>Cave Research</b> : has been mainly carried out by our friends of
|
|
||||||
Upper Austria, an English group, two French groups, and ourselves. For our
|
|
||||||
part we did almost no prospecting, except in 1976. We contented ourselves
|
|
||||||
with the descent of certain known caves - again, not all of them (We
|
|
||||||
bitterly regret this today because others have made discoveries in our
|
|
||||||
place). Our effort was particularly carried out in
|
|
||||||
<span lang="de">Ahnenschacht</span>, but a chronic deficiency of able cavers
|
|
||||||
and relevant experience (in 1975 we were only 4) has prevented us from
|
|
||||||
getting as far as we would have liked.
|
|
||||||
|
|
||||||
<p><b>Geology/Hydrology</b> : Not having a geologist in the group, we could
|
|
||||||
only sketch out the major outlines. The great majority of the area is <span
|
|
||||||
lang="de">Dachsteinkalk</span>, also with some pockets of Dolomite, well seen
|
|
||||||
in certain places - notably north of the <span lang="de">Ahnenschacht</span>.
|
|
||||||
Another problem, the presence of a nappe (overfold) between -400 and -500m
|
|
||||||
which could cause problems in <span lang="de">Ahnenschacht</span>. For the
|
|
||||||
<span lang="de">Raucherkar</span>, the drainage is practically certain: the
|
|
||||||
flood resurgence is in <span lang="de">Nagelsteghöhle</span> to the
|
|
||||||
south of <span lang="de">Raucherkar</span>, and north of
|
|
||||||
<span lang="de">Altaussee</span>. It should be possible to connect the two
|
|
||||||
either directly, or by diving. <span lang="fr">QUELLI</span> should also go
|
|
||||||
in the same direction, at least if one believes its trend.
|
|
||||||
Nevertheless, with <span lang="fr">Quelli</span> opening up 2km NE of
|
|
||||||
<span lang="de">Raucherkar</span>, we need to be very careful in drawing
|
|
||||||
conclusions.
|
|
||||||
|
|
||||||
<p><b lang="de">AHNENSCHACHT</b> lies in an area with very complex
|
|
||||||
boundaries, and could very well go off in several totally different
|
|
||||||
directions. It is very possible that several directions can be followed. The
|
|
||||||
explorations have not proceeded far enough in plan to be able to decide.
|
|
||||||
|
|
||||||
<p><b lang="de">TRUNKEMBOLDSCHACHT</b> and <b lang="de">UFO SCHACHT</b>
|
|
||||||
should be expected to head off to the north where many resurgences can be
|
|
||||||
seen. The other directions should nevertheless not be ignored. At any rate,
|
|
||||||
the explorations will be pushed a lot further this year and perhaps it will
|
|
||||||
become clearer to us.
|
|
||||||
|
|
||||||
<p>From the hydrological point of view, it is very regrettable that no dye
|
|
||||||
tests have been carried out, and this through lack of authorisation,
|
|
||||||
collaboration and interest !!!
|
|
||||||
|
|
||||||
<h2 lang="de"><a id="id55">RAUCHERKARHÖHLENSYSTEM</a></h2>
|
|
||||||
|
|
||||||
<p><span lang="de">Steiermark - Totes Gebirge</span> - 1632m<br>
|
|
||||||
|
|
||||||
Depth 723m Length so far, about 20km<br>
|
|
||||||
|
|
||||||
Deepest point is a sump
|
|
||||||
|
|
||||||
<p><b>Location</b>: In the Western <span lang="de">Totes Gebirge</span>,
|
|
||||||
south of the <span lang="de">Schönberg</span>, 2km SE of <span
|
|
||||||
lang="de">Ahnenschacht</span>.
|
|
||||||
|
|
||||||
<p><b>History</b>: Exploration started in 1961. In 1965, the cave was 6km
|
|
||||||
long and 246m deep. The National Austrian expedition of 1965 reached -530m.
|
|
||||||
In 1973, <span lang="de"><acronym>LVfHK</acronym> Oberösterreich &
|
|
||||||
Steiermark</span> reached a sump at -723m, at which time the length had
|
|
||||||
reached 18km.
|
|
||||||
|
|
||||||
<p><b>Description</b>: The system has no less than 13 entrances ranged
|
|
||||||
between 1500 and 1623m altitude. The labyrinthine system contains several
|
|
||||||
levels of development mostly southwards towards
|
|
||||||
<span lang="de">Nagelsteghöhle</span> (the probable resurgence at an
|
|
||||||
altitude of 850m). It is interesting to note that the final sump has been
|
|
||||||
reached by systematically traversing round pitches in excess of 90-40m.
|
|
||||||
|
|
||||||
<p>Author of this summary : <span lang="fr">Etienne Degrave</span>.
|
|
||||||
|
|
||||||
<h2><a id="id120" lang="fr">QUELLI</a> or
|
|
||||||
<span lang="de">KACHERLSCHACHT</span></h2>
|
|
||||||
|
|
||||||
<p>Western <span lang="de">Totes Gebirge - Feuertal -
|
|
||||||
Schönberg</span><br>
|
|
||||||
|
|
||||||
Depth -708m Altitude about 1950m
|
|
||||||
|
|
||||||
<p><b>History</b>: Discovered in 1973 by the <acronym>GSAB</acronym> under
|
|
||||||
the name T3. Rediscovered in July 1976 by <span lang="fr">J.M.Piron</span>
|
|
||||||
and explored from 12th to 23rd of July by <span lang="fr">A.C.Toulon,
|
|
||||||
S.C.Toulon, Lou Darbon</span> and <span lang="fr">Spéléo
|
|
||||||
Ragaie</span>.
|
|
||||||
|
|
||||||
<p><b>Description</b>: P8, p19, p83, p33, p24, p17, p5, p33, p24, p9, p33,
|
|
||||||
p27, p103. At -400m one reaches a vast passage going up and downhill. The
|
|
||||||
downstream passage emerges at the top of an 84m pitch. Below this a winding
|
|
||||||
canyon interspersed with small pitches gives onto a 15m pitch and the end of
|
|
||||||
exploration at -708m.
|
|
||||||
|
|
||||||
<p lang="fr">Etienne Degrave
|
|
||||||
|
|
||||||
<h2><a id="id117" lang="fr">EMPAGADURE</a> or
|
|
||||||
<span lang="de">TRUNKEMBOLDSCHACHT</span></h2>
|
|
||||||
|
|
||||||
<p>Western <span lang="de">Totes Gebirge - Hintergras</span><br>
|
|
||||||
|
|
||||||
Depth -587m Altitude 1610m
|
|
||||||
|
|
||||||
<p><b>History</b>: Discovered in July 1976 by
|
|
||||||
<span lang="fr">F.Vergier</span>. Explored between 12th and 23rd July 1976 by
|
|
||||||
<span lang="fr">A.C.Toulon, S.C.Toulon, Lou Darbon</span> and
|
|
||||||
<span lang="fr">Spéléo Ragaie</span>.
|
|
||||||
|
|
||||||
<p><b>Description</b>: Down to -287m the cave is made up of shortish pitches
|
|
||||||
interspersed with tight meandering passage : p8, p12, p17, p9, p20, p3, p12,
|
|
||||||
p30, p7, p6, p9, p8, p7, p5, p34, p6, p8, p5, p9. At -287m, a 21m pitch
|
|
||||||
drops into a large chamber. The water disappears in the boulders to reappear
|
|
||||||
in a whole series of wet pitches of which the longest is 30m. Floods impeded
|
|
||||||
exploration at the bottom of this branch: at -456m a pitch of about 20m was
|
|
||||||
definitely too wet to be descended. At -488m a low passage was also too wet.
|
|
||||||
Moreover, the draught there was weak or absent.
|
|
||||||
|
|
||||||
<p>In the chamber at -308m, a reascent of about 15m gave access to a fairly
|
|
||||||
wide fossil canyon which blew a detectable draught. After 30m, this passage
|
|
||||||
opened onto the enormous "<span lang="fr">Puits de Naufragés</span>"
|
|
||||||
(The Castaway's pitch), with a cross section of 15 by 25 metres. On this
|
|
||||||
pitch, several inlets appeared to come from the first branch explored. The
|
|
||||||
bottom of the pitch contracted to a joint-guided rift, exploration ending at
|
|
||||||
the head of a pitch estimated at 40m.
|
|
||||||
|
|
||||||
<p lang="fr">Etienne Degrave
|
|
||||||
|
|
||||||
<h2 lang="de"><a id="id50">AHNENSCHACHT</a></h2>
|
|
||||||
|
|
||||||
<p>Location: Western <span lang="de">Totes Gebirge - Feuertal</span><br>
|
|
||||||
|
|
||||||
Depth: -612m Length so far: > 5km<br>
|
|
||||||
|
|
||||||
<b>Altitude</b>: 1890m
|
|
||||||
|
|
||||||
<p><b>History</b>: Discovered by our Upper Austrian colleagues in 1856. The
|
|
||||||
point -320m was reached by them in 1958. In 1967 and 1968 the
|
|
||||||
<a href="../../bec/index.htm">Bristol Exploration Club</a> reached -400m, the
|
|
||||||
Horizontal network, with a length of 1 km, was discovered. In 1972, 73, 74
|
|
||||||
and 75, the <acronym>GSAB</acronym> "<span lang="fr">Les Gours</span>"
|
|
||||||
explored and discovered over 5km of passage and about 1500m of pitches. This
|
|
||||||
got them to -612m. We note also the participation, in 1974, of three French
|
|
||||||
clubs from Eastern France: <span lang="fr">S.C.Vesoul, G.S.Clerval</span> and
|
|
||||||
<span lang="fr">S.S.Daules</span>. In 1975 <acronym>CARSS</acronym> joined a
|
|
||||||
mini-expedition in July and likewise, <acronym>CASEO</acronym> in August.
|
|
||||||
|
|
||||||
|
<p><b>Introduction</b> : The choice of this area was quite
|
||||||
|
arbitrary. Indeed, there is very little chance that the area is all
|
||||||
|
drained by the same hydrological system. While for some caves, the
|
||||||
|
presumed resurgence is almost certain, the same is not true of
|
||||||
|
others which may drain in totally the opposite direction ! Our
|
||||||
|
choice was governed by means of access: roads, gear lift, paths, a
|
||||||
|
refuge etc.. The <span lang="de" xml:lang="de">Totes
|
||||||
|
Gebirge</span>, which is one of the biggest karst ranges in
|
||||||
|
Austria, is only easily accessible in certain areas, such as the
|
||||||
|
one we discuss in this article. In this area are many kilometres of
|
||||||
|
totally virgin lapiaz. Many hours walking are needed to reach it.
|
||||||
|
Moreover, in this area, only a tiny part is more-or-less
|
||||||
|
prospected. It includes the valleys of <span lang="de" xml:lang=
|
||||||
|
"de">Raucherkar</span> and <span lang="de" xml:lang=
|
||||||
|
"de">Feuertal</span>, and the areas adjoining the path which goes
|
||||||
|
to them as well as the north face of <span lang="de" xml:lang=
|
||||||
|
"de">Hagender Kogel</span>, in which lies the <span lang="de"
|
||||||
|
xml:lang="de">Tropfsteinhöhle</span>, which had extraordinary
|
||||||
|
formations but which is today completely trashed out.</p>
|
||||||
|
<p><b>Cave Research</b> : has been mainly carried out by our
|
||||||
|
friends of Upper Austria, an English group, two French groups, and
|
||||||
|
ourselves. For our part we did almost no prospecting, except in
|
||||||
|
1976. We contented ourselves with the descent of certain known
|
||||||
|
caves - again, not all of them (We bitterly regret this today
|
||||||
|
because others have made discoveries in our place). Our effort was
|
||||||
|
particularly carried out in <span lang="de" xml:lang=
|
||||||
|
"de">Ahnenschacht</span>, but a chronic deficiency of able cavers
|
||||||
|
and relevant experience (in 1975 we were only 4) has prevented us
|
||||||
|
from getting as far as we would have liked.</p>
|
||||||
|
<p><b>Geology/Hydrology</b> : Not having a geologist in the group,
|
||||||
|
we could only sketch out the major outlines. The great majority of
|
||||||
|
the area is <span lang="de" xml:lang="de">Dachsteinkalk</span>,
|
||||||
|
also with some pockets of Dolomite, well seen in certain places -
|
||||||
|
notably north of the <span lang="de" xml:lang=
|
||||||
|
"de">Ahnenschacht</span>. Another problem, the presence of a nappe
|
||||||
|
(overfold) between -400 and -500m which could cause problems in
|
||||||
|
<span lang="de" xml:lang="de">Ahnenschacht</span>. For the
|
||||||
|
<span lang="de" xml:lang="de">Raucherkar</span>, the drainage is
|
||||||
|
practically certain: the flood resurgence is in <span lang="de"
|
||||||
|
xml:lang="de">Nagelsteghöhle</span> to the south of
|
||||||
|
<span lang="de" xml:lang="de">Raucherkar</span>, and north of
|
||||||
|
<span lang="de" xml:lang="de">Altaussee</span>. It should be
|
||||||
|
possible to connect the two either directly, or by diving.
|
||||||
|
<span lang="fr" xml:lang="fr">QUELLI</span> should also go in the
|
||||||
|
same direction, at least if one believes its trend. Nevertheless,
|
||||||
|
with <span lang="fr" xml:lang="fr">Quelli</span> opening up 2km NE
|
||||||
|
of <span lang="de" xml:lang="de">Raucherkar</span>, we need to be
|
||||||
|
very careful in drawing conclusions.</p>
|
||||||
|
<p><b lang="de" xml:lang="de">AHNENSCHACHT</b> lies in an area with
|
||||||
|
very complex boundaries, and could very well go off in several
|
||||||
|
totally different directions. It is very possible that several
|
||||||
|
directions can be followed. The explorations have not proceeded far
|
||||||
|
enough in plan to be able to decide.</p>
|
||||||
|
<p><b lang="de" xml:lang="de">TRUNKEMBOLDSCHACHT</b> and <b lang=
|
||||||
|
"de" xml:lang="de">UFO SCHACHT</b> should be expected to head off
|
||||||
|
to the north where many resurgences can be seen. The other
|
||||||
|
directions should nevertheless not be ignored. At any rate, the
|
||||||
|
explorations will be pushed a lot further this year and perhaps it
|
||||||
|
will become clearer to us.</p>
|
||||||
|
<p>From the hydrological point of view, it is very regrettable that
|
||||||
|
no dye tests have been carried out, and this through lack of
|
||||||
|
authorisation, collaboration and interest !!!</p>
|
||||||
|
<h2 lang="de" xml:lang="de"><a id="id55" name=
|
||||||
|
"id55">RAUCHERKARHÖHLENSYSTEM</a></h2>
|
||||||
|
<p><span lang="de" xml:lang="de">Steiermark - Totes Gebirge</span>
|
||||||
|
- 1632m<br />
|
||||||
|
Depth 723m Length so far, about 20km<br />
|
||||||
|
Deepest point is a sump</p>
|
||||||
|
<p><b>Location</b>: In the Western <span lang="de" xml:lang=
|
||||||
|
"de">Totes Gebirge</span>, south of the <span lang="de" xml:lang=
|
||||||
|
"de">Schönberg</span>, 2km SE of <span lang="de" xml:lang=
|
||||||
|
"de">Ahnenschacht</span>.</p>
|
||||||
|
<p><b>History</b>: Exploration started in 1961. In 1965, the cave
|
||||||
|
was 6km long and 246m deep. The National Austrian expedition of
|
||||||
|
1965 reached -530m. In 1973, <span lang="de" xml:lang=
|
||||||
|
"de"><acronym>LVfHK</acronym> Oberösterreich &
|
||||||
|
Steiermark</span> reached a sump at -723m, at which time the length
|
||||||
|
had reached 18km.</p>
|
||||||
|
<p><b>Description</b>: The system has no less than 13 entrances
|
||||||
|
ranged between 1500 and 1623m altitude. The labyrinthine system
|
||||||
|
contains several levels of development mostly southwards towards
|
||||||
|
<span lang="de" xml:lang="de">Nagelsteghöhle</span> (the
|
||||||
|
probable resurgence at an altitude of 850m). It is interesting to
|
||||||
|
note that the final sump has been reached by systematically
|
||||||
|
traversing round pitches in excess of 90-40m.</p>
|
||||||
|
<p>Author of this summary : <span lang="fr" xml:lang="fr">Etienne
|
||||||
|
Degrave</span>.</p>
|
||||||
|
<h2><a id="id120" lang="fr" name="id120" xml:lang="fr">QUELLI</a>
|
||||||
|
or <span lang="de" xml:lang="de">KACHERLSCHACHT</span></h2>
|
||||||
|
<p>Western <span lang="de" xml:lang="de">Totes Gebirge - Feuertal -
|
||||||
|
Schönberg</span><br />
|
||||||
|
Depth -708m Altitude about 1950m</p>
|
||||||
|
<p><b>History</b>: Discovered in 1973 by the
|
||||||
|
<acronym>GSAB</acronym> under the name T3. Rediscovered in July
|
||||||
|
1976 by <span lang="fr" xml:lang="fr">J.M.Piron</span> and explored
|
||||||
|
from 12th to 23rd of July by <span lang="fr" xml:lang=
|
||||||
|
"fr">A.C.Toulon, S.C.Toulon, Lou Darbon</span> and <span lang="fr"
|
||||||
|
xml:lang="fr">Spéléo Ragaie</span>.</p>
|
||||||
|
<p><b>Description</b>: P8, p19, p83, p33, p24, p17, p5, p33, p24,
|
||||||
|
p9, p33, p27, p103. At -400m one reaches a vast passage going up
|
||||||
|
and downhill. The downstream passage emerges at the top of an 84m
|
||||||
|
pitch. Below this a winding canyon interspersed with small pitches
|
||||||
|
gives onto a 15m pitch and the end of exploration at -708m.</p>
|
||||||
|
<p lang="fr" xml:lang="fr">Etienne Degrave</p>
|
||||||
|
<h2><a id="id117" lang="fr" name="id117" xml:lang=
|
||||||
|
"fr">EMPAGADURE</a> or <span lang="de" xml:lang=
|
||||||
|
"de">TRUNKEMBOLDSCHACHT</span></h2>
|
||||||
|
<p>Western <span lang="de" xml:lang="de">Totes Gebirge -
|
||||||
|
Hintergras</span><br />
|
||||||
|
Depth -587m Altitude 1610m</p>
|
||||||
|
<p><b>History</b>: Discovered in July 1976 by <span lang="fr"
|
||||||
|
xml:lang="fr">F.Vergier</span>. Explored between 12th and 23rd July
|
||||||
|
1976 by <span lang="fr" xml:lang="fr">A.C.Toulon, S.C.Toulon, Lou
|
||||||
|
Darbon</span> and <span lang="fr" xml:lang=
|
||||||
|
"fr">Spéléo Ragaie</span>.</p>
|
||||||
|
<p><b>Description</b>: Down to -287m the cave is made up of
|
||||||
|
shortish pitches interspersed with tight meandering passage : p8,
|
||||||
|
p12, p17, p9, p20, p3, p12, p30, p7, p6, p9, p8, p7, p5, p34, p6,
|
||||||
|
p8, p5, p9. At -287m, a 21m pitch drops into a large chamber. The
|
||||||
|
water disappears in the boulders to reappear in a whole series of
|
||||||
|
wet pitches of which the longest is 30m. Floods impeded exploration
|
||||||
|
at the bottom of this branch: at -456m a pitch of about 20m was
|
||||||
|
definitely too wet to be descended. At -488m a low passage was also
|
||||||
|
too wet. Moreover, the draught there was weak or absent.</p>
|
||||||
|
<p>In the chamber at -308m, a reascent of about 15m gave access to
|
||||||
|
a fairly wide fossil canyon which blew a detectable draught. After
|
||||||
|
30m, this passage opened onto the enormous "<span lang="fr"
|
||||||
|
xml:lang="fr">Puits de Naufragés</span>" (The Castaway's
|
||||||
|
pitch), with a cross section of 15 by 25 metres. On this pitch,
|
||||||
|
several inlets appeared to come from the first branch explored. The
|
||||||
|
bottom of the pitch contracted to a joint-guided rift, exploration
|
||||||
|
ending at the head of a pitch estimated at 40m.</p>
|
||||||
|
<p lang="fr" xml:lang="fr">Etienne Degrave</p>
|
||||||
|
<h2 lang="de" xml:lang="de"><a id="id50" name=
|
||||||
|
"id50">AHNENSCHACHT</a></h2>
|
||||||
|
<p>Location: Western <span lang="de" xml:lang="de">Totes Gebirge -
|
||||||
|
Feuertal</span><br />
|
||||||
|
Depth: -612m Length so far: > 5km<br />
|
||||||
|
<b>Altitude</b>: 1890m</p>
|
||||||
|
<p><b>History</b>: Discovered by our Upper Austrian colleagues in
|
||||||
|
1856. The point -320m was reached by them in 1958. In 1967 and 1968
|
||||||
|
the <a href="../../bec/index.htm">Bristol Exploration Club</a>
|
||||||
|
reached -400m, the Horizontal network, with a length of 1 km, was
|
||||||
|
discovered. In 1972, 73, 74 and 75, the <acronym>GSAB</acronym>
|
||||||
|
"<span lang="fr" xml:lang="fr">Les Gours</span>" explored and
|
||||||
|
discovered over 5km of passage and about 1500m of pitches. This got
|
||||||
|
them to -612m. We note also the participation, in 1974, of three
|
||||||
|
French clubs from Eastern France: <span lang="fr" xml:lang=
|
||||||
|
"fr">S.C.Vesoul, G.S.Clerval</span> and <span lang="fr" xml:lang=
|
||||||
|
"fr">S.S.Daules</span>. In 1975 <acronym>CARSS</acronym> joined a
|
||||||
|
mini-expedition in July and likewise, <acronym>CASEO</acronym> in
|
||||||
|
August.</p>
|
||||||
<h3>Description: Entrance series</h3>
|
<h3>Description: Entrance series</h3>
|
||||||
|
<p>The entrance is in a small doline situated on the ridge
|
||||||
<p>The entrance is in a small doline situated on the ridge separating
|
separating <span lang="de" xml:lang="de">Feuertal</span> and
|
||||||
<span lang="de">Feuertal</span> and <span lang="de">Hintergras</span>. The
|
<span lang="de" xml:lang="de">Hintergras</span>. The cave starts
|
||||||
cave starts with four pitches (p14, p11, p5 and p11) which drop onto a slope
|
with four pitches (p14, p11, p5 and p11) which drop onto a slope
|
||||||
formed of big boulders (rope desirable). After this, another series of small
|
formed of big boulders (rope desirable). After this, another series
|
||||||
pitches (p9, p7, p6, p4, p10, p18, p11) from which is reached the "<span
|
of small pitches (p9, p7, p6, p4, p10, p18, p11) from which is
|
||||||
lang="de">Sinterterrasse</span>" at -141m.
|
reached the "<span lang="de" xml:lang="de">Sinterterrasse</span>"
|
||||||
|
at -141m.</p>
|
||||||
<p>From this point, one has left the zone of small pitches and started a
|
<p>From this point, one has left the zone of small pitches and
|
||||||
series of pitches which in reality are part of a single shaft down to -400m.
|
started a series of pitches which in reality are part of a single
|
||||||
|
shaft down to -400m.</p>
|
||||||
<p>Indeed, if you had an unfortunate accident on the
|
<p>Indeed, if you had an unfortunate accident on the "<span lang=
|
||||||
"<span lang="de">Sinterterrasse</span>", you would fall all the way to -400m.
|
"de" xml:lang="de">Sinterterrasse</span>", you would fall all the
|
||||||
These pitches are usually wet, especially after rain... Here is the list of
|
way to -400m. These pitches are usually wet, especially after
|
||||||
pitches: p25, <span lang="de">Schuppenstufe</span> 30, p10,
|
rain... Here is the list of pitches: p25, <span lang="de" xml:lang=
|
||||||
<span lang="de">Sicherungsstufe</span> 32,
|
"de">Schuppenstufe</span> 30, p10, <span lang="de" xml:lang=
|
||||||
<span lang="de">Schachtgabel</span> 48, a 10m ramp, <span lang="de">Josef
|
"de">Sicherungsstufe</span> 32, <span lang="de" xml:lang=
|
||||||
Schacht</span> 100m. On the <span lang="de">Josef Schacht</span>, a pendulum
|
"de">Schachtgabel</span> 48, a 10m ramp, <span lang="de" xml:lang=
|
||||||
6m from the top enables one to reach the entry to the "Horizontal network".
|
"de">Josef Schacht</span> 100m. On the <span lang="de" xml:lang=
|
||||||
Descending the <span lang="de">Josef Schacht</span> a little further, after a
|
"de">Josef Schacht</span>, a pendulum 6m from the top enables one
|
||||||
6.5m and a 10m pitch, access can be gained to a wide canyon, active in the
|
to reach the entry to the "Horizontal network". Descending the
|
||||||
bottom, and which ends in a fissure. This canyon is fossil in the upper level
|
<span lang="de" xml:lang="de">Josef Schacht</span> a little
|
||||||
and certainly presents possibilities for continuation.
|
further, after a 6.5m and a 10m pitch, access can be gained to a
|
||||||
|
wide canyon, active in the bottom, and which ends in a fissure.
|
||||||
<h4>Lateral development from <span lang="de">Josef Schacht</span></h4>
|
This canyon is fossil in the upper level and certainly presents
|
||||||
|
possibilities for continuation.</p>
|
||||||
<p>After one has crossed the "doorway" and a short squeeze, one enters the
|
<h4>Lateral development from <span lang="de" xml:lang="de">Josef
|
||||||
network proper. At this point is a passage covered in rather special
|
Schacht</span></h4>
|
||||||
formations. The first junction gives access to a network
|
<p>After one has crossed the "doorway" and a short squeeze, one
|
||||||
[ lines missing from original photocopy - sorry :-(]
|
enters the network proper. At this point is a passage covered in
|
||||||
|
rather special formations. The first junction gives access to a
|
||||||
|
network [ lines missing from original photocopy - sorry :-(]</p>
|
||||||
<h4>The Vegetable Garden</h4>
|
<h4>The Vegetable Garden</h4>
|
||||||
|
<p>This fossil system, which has not been fully travelled through,
|
||||||
<p>This fossil system, which has not been fully travelled through, contains
|
contains numerous possibilities. It is reached by three principal
|
||||||
numerous possibilities. It is reached by three principal access routes: the
|
access routes: the pitch already mentioned; a descending fissure a
|
||||||
pitch already mentioned; a descending fissure a little before the "Belgica";
|
little before the "Belgica"; and a sloping passage with formations
|
||||||
and a sloping passage with formations in the "Mammoth pitch" chamber. The
|
in the "Mammoth pitch" chamber. The system is composed of a big
|
||||||
system is composed of a big chamber with numerous passages and junctions; it
|
chamber with numerous passages and junctions; it is very poorly
|
||||||
is very poorly known and no doubt houses many surprises. Continuing along the
|
known and no doubt houses many surprises. Continuing along the
|
||||||
passage, one passes a step of 4m to find a junction, to the left at which
|
passage, one passes a step of 4m to find a junction, to the left at
|
||||||
lies the bivouac.
|
which lies the bivouac.</p>
|
||||||
|
|
||||||
<h4>"Belgica" system</h4>
|
<h4>"Belgica" system</h4>
|
||||||
|
<p>Directly after the bivouac, there is a 10m pitch, and at the
|
||||||
<p>Directly after the bivouac, there is a 10m pitch, and at the bottom, a new
|
bottom, a new junction: downhill the "Belgica" passage, of fairly
|
||||||
junction: downhill the "Belgica" passage, of fairly small dimensions, which
|
small dimensions, which leads, after traversing past three holes,
|
||||||
leads, after traversing past three holes, to a descent of an 8m and a 17m
|
to a descent of an 8m and a 17m pitch and to the squeezes passed by
|
||||||
pitch and to the squeezes passed by our French colleagues.
|
our French colleagues. [<span lang="fr" xml:lang="fr">A
|
||||||
[<span lang="fr">A revoir</span>]
|
revoir</span>]</p>
|
||||||
|
<p>Uphill, discovered by <span lang="fr" xml:lang=
|
||||||
<p>Uphill, discovered by <span lang="fr">D.Motte</span> and
|
"fr">D.Motte</span> and <acronym>PIE</acronym>, in the course of
|
||||||
<acronym>PIE</acronym>, in the course of the expedition in 1974, is the
|
the expedition in 1974, is the "<span lang="fr" xml:lang=
|
||||||
"<span lang="fr">Galerie de Francs comtois</span>". This is a large ascending
|
"fr">Galerie de Francs comtois</span>". This is a large ascending
|
||||||
fossil passage interspersed with traverses, dips and pitches. It reascends to
|
fossil passage interspersed with traverses, dips and pitches. It
|
||||||
-90m. At -150m, a 20m pitch reaches the "<span lang="fr">Resomega</span>".
|
reascends to -90m. At -150m, a 20m pitch reaches the "<span lang=
|
||||||
|
"fr" xml:lang="fr">Resomega</span>".</p>
|
||||||
<p>A little before the 20m pitch, a short descending canyon passage avoids
|
<p>A little before the 20m pitch, a short descending canyon passage
|
||||||
the 20m pitch and the series of squeezes following it.
|
avoids the 20m pitch and the series of squeezes following it. The
|
||||||
The "<span lang="fr">Resomega</span>" is an alternately ascending and
|
"<span lang="fr" xml:lang="fr">Resomega</span>" is an alternately
|
||||||
descending passage, very chaotic, interspersed with several junctions and
|
ascending and descending passage, very chaotic, interspersed with
|
||||||
pitches which leads to the "Balcon du Visionnaire", offering several
|
several junctions and pitches which leads to the "Balcon du
|
||||||
possibilities. A 60m pitch gives onto another 60m pitch which is undescended.
|
Visionnaire", offering several possibilities. A 60m pitch gives
|
||||||
There is another big pitch in excess of 100m and an unfinished ascending
|
onto another 60m pitch which is undescended. There is another big
|
||||||
passage. A little before, a 10m pitch allows one to reach a passage
|
pitch in excess of 100m and an unfinished ascending passage. A
|
||||||
interspersed with 3 junctions and 7 exits !!!! This shows the level of
|
little before, a 10m pitch allows one to reach a passage
|
||||||
complexity which we ran into.
|
interspersed with 3 junctions and 7 exits !!!! This shows the level
|
||||||
|
of complexity which we ran into.</p>
|
||||||
<p>It was also at the "<span lang="fr">Balcon du Visionnaire</span>" that an
|
<p>It was also at the "<span lang="fr" xml:lang="fr">Balcon du
|
||||||
accident occurred in 1975, which terminated exploration in that year.
|
Visionnaire</span>" that an accident occurred in 1975, which
|
||||||
|
terminated exploration in that year.</p>
|
||||||
<p>Back in the Horizontal network, and after passing a little bouldery climb
|
<p>Back in the Horizontal network, and after passing a little
|
||||||
an inlet is encountered, named "The Bath". The passage continues a little
|
bouldery climb an inlet is encountered, named "The Bath". The
|
||||||
longer, to end in a pitch. [To be completed]
|
passage continues a little longer, to end in a pitch. [To be
|
||||||
|
completed]</p>
|
||||||
<p>The following junction has been named "Mammoth Junction" because the
|
<p>The following junction has been named "Mammoth Junction" because
|
||||||
passage to the right leads onto the pitch of the same name. It is necessary
|
the passage to the right leads onto the pitch of the same name. It
|
||||||
to exercise great care and attention not to slip hereabouts, because a fall
|
is necessary to exercise great care and attention not to slip
|
||||||
would drop you into same.
|
hereabouts, because a fall would drop you into same.</p>
|
||||||
|
<p>The Mammoth Pitch, Para-pitch and probably the "Negus" pitch,
|
||||||
<p>The Mammoth Pitch, Para-pitch and probably the "Negus" pitch, form part of
|
form part of the same system ( see survey ) which is composed of a
|
||||||
the same system ( see survey ) which is composed of a 146m pitch, a 10m pitch
|
146m pitch, a 10m pitch and a narrow canyon interspersed with
|
||||||
and a narrow canyon interspersed with several cascades leading finally to a
|
several cascades leading finally to a 35m pitch giving onto the
|
||||||
35m pitch giving onto the sump at -612m. The Para-pitch, p106, is followed by
|
sump at -612m. The Para-pitch, p106, is followed by pitches of 5,
|
||||||
pitches of 5, 10 and 50m and drops via the latter into the "Mammoth Canyon"
|
10 and 50m and drops via the latter into the "Mammoth Canyon"</p>
|
||||||
|
<p>The "Negus" pitch, which is undescended, should also drop into
|
||||||
<p>The "Negus" pitch, which is undescended, should also drop into the same
|
the same canyon. Several other small pitches and active streamways
|
||||||
canyon. Several other small pitches and active streamways should also rejoin
|
should also rejoin this system.</p>
|
||||||
this system.
|
<p>The depth of 612m should be treated cautiously because the
|
||||||
|
method of survey used (height of a man) is fairly imprecise. The
|
||||||
<p>The depth of 612m should be treated cautiously because the method of
|
bottom could be anywhere between -580m and -630m. The shortage of
|
||||||
survey used (height of a man) is fairly imprecise. The bottom could be
|
time prevented us from redoing our survey. Maybe this year ????</p>
|
||||||
anywhere between -580m and -630m. The shortage of time prevented us from
|
<p>Turning left, the "Zipfer" passage is followed for 150m before
|
||||||
redoing our survey. Maybe this year ????
|
reaching an important junction: to the left "Chimneys passage", to
|
||||||
|
the right "Draughting passage".</p>
|
||||||
<p>Turning left, the "Zipfer" passage is followed for 150m before reaching an
|
|
||||||
important junction: to the left "Chimneys passage", to the right "Draughting
|
|
||||||
passage".
|
|
||||||
|
|
||||||
<h4>Chimneys Passage</h4>
|
<h4>Chimneys Passage</h4>
|
||||||
|
<p>This is very large with a constant slope, interrupted in the
|
||||||
<p>This is very large with a constant slope, interrupted in the middle by a
|
middle by a squeeze and a couple of drops. The "Schnaps pitch" (40m
|
||||||
squeeze and a couple of drops. The "Schnaps pitch" (40m with an unexplored,
|
with an unexplored, narrow canyon) is avoided by traversing to
|
||||||
narrow canyon) is avoided by traversing to reach a 25m pitch in which you
|
reach a 25m pitch in which you must pendulum 5m from the bottom in
|
||||||
must pendulum 5m from the bottom in order to reach a chamber in which is met
|
order to reach a chamber in which is met a small stream. Climbing
|
||||||
a small stream. Climbing up a little opposite, a short upper passage rejoins
|
up a little opposite, a short upper passage rejoins the stream by a
|
||||||
the stream by a 20m pitch. In the chamber, the descent of a 10m pitch allows
|
20m pitch. In the chamber, the descent of a 10m pitch allows the
|
||||||
the stream to be followed to a squeeze beyond which one can hear the grumble
|
stream to be followed to a squeeze beyond which one can hear the
|
||||||
of a large river ? A place to go back to.
|
grumble of a large river ? A place to go back to.</p>
|
||||||
|
|
||||||
<h4>Draughting passage</h4>
|
<h4>Draughting passage</h4>
|
||||||
|
<p>This is fossil, and tight in places, and allows exploration of a
|
||||||
<p>This is fossil, and tight in places, and allows exploration of a very
|
very complex network which intersects itself in various places and
|
||||||
complex network which intersects itself in various places and which could
|
which could hold very great surprises, since its exploration has
|
||||||
hold very great surprises, since its exploration has only been sketchily
|
only been sketchily outlined. The exit from this passage is in an
|
||||||
outlined. The exit from this passage is in an area of boulders where two
|
area of boulders where two possibilities exist:</p>
|
||||||
possibilities exist:
|
<p><b>To the left</b>: a tight passage has been forced on a slope
|
||||||
|
to "<span lang="de" xml:lang="de">Kitschacht</span>" (Tackle Bag
|
||||||
<p><b>To the left</b>: a tight passage has been forced on a slope to
|
Shaft) a magnificent 50m drop, very wide and completely free
|
||||||
"<span lang="de">Kitschacht</span>" (Tackle Bag Shaft) a magnificent 50m
|
hanging. At its base, several possibilities. A tight active canyon
|
||||||
drop, very wide and completely free hanging. At its base, several
|
which can be bypassed by a fossil passage, broken by an earthy drop
|
||||||
possibilities. A tight active canyon which can be bypassed by a fossil
|
of 3m to a huge 15m pitch leading to a sump at -360m.</p>
|
||||||
passage, broken by an earthy drop of 3m to a huge 15m pitch leading to a sump
|
<p>A drop of a few metres gives access to a huge fossil passage (
|
||||||
at -360m.
|
10 x 5m ). The floor of this is cut by a deep canyon which has not
|
||||||
|
been explored. After a hundred metres or so the passage ends at a
|
||||||
<p>A drop of a few metres gives access to a huge fossil passage ( 10 x 5m ).
|
vast wet pitch. Climbing over a big boulder on the right gives
|
||||||
The floor of this is cut by a deep canyon which has not been explored. After
|
access to another pitch upwards.</p>
|
||||||
a hundred metres or so the passage ends at a vast wet pitch. Climbing over a
|
<p>Just after the base of <span lang="de" xml:lang=
|
||||||
big boulder on the right gives access to another pitch upwards.
|
"de">Kitschacht</span>, a passage of 80m makes a connection with
|
||||||
|
the system of the "<span lang="fr" xml:lang=
|
||||||
<p>Just after the base of <span lang="de">Kitschacht</span>, a passage of 80m
|
"fr">Décollement</span>" pitch at the bottom of the 40m
|
||||||
makes a connection with the system of the "<span
|
shaft. A canyon leaving the junction passage can be followed for
|
||||||
lang="fr">Décollement</span>" pitch at the bottom of the 40m shaft. A
|
more than 300m, and exits, in several places, into the side of the
|
||||||
canyon leaving the junction passage can be followed for more than 300m, and
|
big fossil passage, just before the pitch upwards.</p>
|
||||||
exits, in several places, into the side of the big fossil passage, just
|
<p><b>To the right</b>: The "<span lang="fr" xml:lang=
|
||||||
before the pitch upwards.
|
"fr">Décollement</span>" pitch, with, at its base, a sloping
|
||||||
|
chamber full of boulders. To the left a very deep ascending canyon
|
||||||
<p><b>To the right</b>: The "<span lang="fr">Décollement</span>"
|
is unexplored. In the bottom is the "<span lang="fr" xml:lang=
|
||||||
pitch, with, at its base, a sloping chamber full of boulders. To the left a
|
"fr">Méandre Emeri</span>", so called because the formations
|
||||||
very deep ascending canyon is unexplored. In the bottom is the
|
are orientated in the direction of progress and of the draught.
|
||||||
"<span lang="fr">Méandre Emeri</span>", so called because the
|
This rejoins a wide pitch with an inlet. After this 15m pitch is a
|
||||||
formations are orientated in the direction of progress and of the draught.
|
short canyon and a damp 40m pitch. At the bottom, a huge descending
|
||||||
This rejoins a wide pitch with an inlet. After this 15m pitch is a short
|
passage suddenly turns almost vertical. This is the "Toboggan",
|
||||||
canyon and a damp 40m pitch. At the bottom, a huge descending passage
|
needing 20m of rope (a very spectacular passage). At this level one
|
||||||
suddenly turns almost vertical. This is the "Toboggan", needing 20m of rope
|
again cuts a new streamway. The passage continues, then contracts,
|
||||||
(a very spectacular passage). At this level one again cuts a new streamway.
|
and chokes at -385m.</p>
|
||||||
The passage continues, then contracts, and chokes at -385m.
|
<p><b>Conclusion</b>: An enormous amount to see and to go back and
|
||||||
|
finish. The more we explore, the more we find ! With more support
|
||||||
<p><b>Conclusion</b>: An enormous amount to see and to go back and finish.
|
we could do some extraordinary speleological work.</p>
|
||||||
The more we explore, the more we find ! With more support we could do some
|
<p style="text-align: right" lang="fr" xml:lang="fr">J.C.Hans</p>
|
||||||
extraordinary speleological work.
|
<h2><a id="id122" lang="de" name="id122" xml:lang="de">UFO
|
||||||
|
SCHACHT</a> or <span lang="fr" xml:lang="fr">GOUFFRE
|
||||||
<p align=right lang="fr">J.C.Hans
|
OVNI</span></h2>
|
||||||
|
<p><b>Location</b>: Western <span lang="de" xml:lang="de">Totes
|
||||||
<h2><a id="id122" lang="de">UFO SCHACHT</a> or <span lang="fr">GOUFFRE OVNI</span></h2>
|
Gebirge - Hintergras</span><br />
|
||||||
|
<b>Depth</b>: -201m <b>Altitude</b>: about 1500m</p>
|
||||||
<p><b>Location</b>: Western <span lang="de">Totes Gebirge - Hintergras</span><br>
|
<p><b>History</b>: Discovered in August 1974 by <span lang="fr"
|
||||||
|
xml:lang="fr">D.Motte</span>. Entrance unblocked by
|
||||||
<b>Depth</b>: -201m <b>Altitude</b>: about 1500m
|
<acronym>GSAB</acronym> in 1975 and 76. Explored in August 1976 by
|
||||||
|
<span lang="fr" xml:lang="fr">F.Dechany</span> and <span lang="fr"
|
||||||
<p><b>History</b>: Discovered in August 1974 by
|
xml:lang="fr">J.C.Hans</span>.</p>
|
||||||
<span lang="fr">D.Motte</span>. Entrance unblocked by <acronym>GSAB</acronym>
|
<p><b>Description</b>: The entrance consists of a crack about 20cm
|
||||||
in 1975 and 76. Explored in August 1976 by <span lang="fr">F.Dechany</span>
|
high, which was at first cleared as far as a chamber with no way
|
||||||
and <span lang="fr">J.C.Hans</span>.
|
on. The draught which had enabled us to find the entrance now
|
||||||
|
showed us the way on. After having unblocked a fissure dubbed "Sas"
|
||||||
<p><b>Description</b>: The entrance consists of a crack about 20cm high,
|
we arrived at a pitch. This is broken in five places. A second
|
||||||
which was at first cleared as far as a chamber with no way on. The draught
|
pitch broken into three leads to a short canyon, then to several
|
||||||
which had enabled us to find the entrance now showed us the way on. After
|
drops and pitches interspersed with short squeezes. The following
|
||||||
having unblocked a fissure dubbed "Sas" we arrived at a pitch. This is
|
pitches can be seen as forming a single 80m shaft, divided into
|
||||||
broken in five places. A second pitch broken into three leads to a short
|
five and becoming bigger and bigger in depth as well as width. The
|
||||||
canyon, then to several drops and pitches interspersed with short squeezes.
|
cave continues by a fault rift two or three metres wide and
|
||||||
The following pitches can be seen as forming a single 80m shaft, divided
|
penetrating by successive notches. The exploration will continue in
|
||||||
into five and becoming bigger and bigger in depth as well as width. The cave
|
August 1977.</p>
|
||||||
continues by a fault rift two or three metres wide and penetrating by
|
<p style="text-align: right" lang="fr" xml:lang="fr">J.C.Hans</p>
|
||||||
successive notches. The exploration will continue in August 1977.
|
|
||||||
|
|
||||||
<p align=right lang="fr">J.C.Hans
|
|
||||||
<hr />
|
<hr />
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="../index.htm"><acronym>GSAB</acronym> articles list</a></li>
|
<li><a href="../index.htm"><acronym>GSAB</acronym> articles
|
||||||
|
list</a></li>
|
||||||
<li><b>Cave descriptions</b> (in English translation):
|
<li><b>Cave descriptions</b> (in English translation):
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="../../../noinfo/1626/50.htm"><span lang="de">Ahnenschacht</span></a></li>
|
<li><a href="../../../noinfo/1626/50.htm"><span lang="de" xml:lang=
|
||||||
<li><a href="../../../noinfo/1626/117.htm"><span lang="de">Trunkemboldschacht</span></a></li>
|
"de">Ahnenschacht</span></a></li>
|
||||||
<li><a href="../../../noinfo/1626/120.htm"><span lang="de">Feuertalsystem</span></a></li>
|
<li><a href="../../../noinfo/1626/117.htm"><span lang="de"
|
||||||
<li><a href="../../../noinfo/1626/122.htm"><span lang="fr">Gouffre Ovni</span></a></li>
|
xml:lang="de">Trunkemboldschacht</span></a></li>
|
||||||
</ul></li>
|
<li><a href="../../../noinfo/1626/120.htm"><span lang="de"
|
||||||
<li><a href="../../../1626/index.htm">Overview</a>
|
xml:lang="de">Feuertalsystem</span></a></li>
|
||||||
of area 1626, and index to caves</li>
|
<li><a href="../../../noinfo/1626/122.htm"><span lang="fr"
|
||||||
<li>Back to <a href="../../../index.htm">Expedition Intro page</a></li>
|
xml:lang="fr">Gouffre Ovni</span></a></li>
|
||||||
<li><a href="../../../../index.htm">Back to <acronym>CUCC</acronym> Home page</a></li>
|
</ul>
|
||||||
|
</li>
|
||||||
|
<li><a href="../../../1626/index.htm">Overview</a> of area 1626,
|
||||||
|
and index to caves</li>
|
||||||
|
<li>Back to <a href="../../../index.htm">Expedition Intro
|
||||||
|
page</a></li>
|
||||||
|
<li><a href="../../../../index.htm">Back to <acronym>CUCC</acronym>
|
||||||
|
Home page</a></li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
</html>
|
</html>
|
||||||
|
|||||||
@@ -1,115 +1,120 @@
|
|||||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
|
||||||
<html>
|
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
||||||
|
<html xmlns="http://www.w3.org/1999/xhtml">
|
||||||
<head>
|
<head>
|
||||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
<meta http-equiv="Content-Type" content=
|
||||||
|
"text/html; charset=iso-8859-1" />
|
||||||
<title>GSAB: CTS ref. 79.1855</title>
|
<title>GSAB: CTS ref. 79.1855</title>
|
||||||
<link rel="stylesheet" type="text/css" href="../../../css/main2.css" />
|
<link rel="stylesheet" type="text/css" href=
|
||||||
|
"../../../css/main2.css" />
|
||||||
</head>
|
</head>
|
||||||
<body>
|
<body>
|
||||||
<center><font size=-1>(<acronym>GSAB</acronym>)
|
<p style="font-size: 65%; text-align: center">(<acronym>GSAB</acronym>) <span
|
||||||
<span lang="fr">Spéalp</span> 3 (Oct. 1978) pp 44-45</font>
|
lang="fr" xml:lang="fr">Spéalp</span> 3 (Oct. 1978) pp 44-45</p>
|
||||||
<h1><span lang="de">AHNENSCHACHT</span> 77-78</h1></center>
|
<h1><span lang="de" xml:lang="de">AHNENSCHACHT</span> 77-78</h1>
|
||||||
|
|
||||||
<p><b>Situation </b>: <span lang="de">Totes Gebirge West - Feuertal</span><br>
|
|
||||||
|
|
||||||
<b>Depth </b>: -607m<br>
|
|
||||||
|
|
||||||
<b>Altitude </b>: 1890m ; <span lang="de">Frigoschacht</span> 1875m<br>
|
|
||||||
|
|
||||||
<b>History </b>: see <a href="782012.htm"><span lang="fr">Spéalp</span> number 1</a>
|
|
||||||
|
|
||||||
<p>The <acronym>GSAB</acronym> expedition was organised from 5th to 29th
|
|
||||||
August, 1977
|
|
||||||
|
|
||||||
<p>Several individuals from different clubs joined up, and in parallel with
|
|
||||||
the exploration of the <span lang="fr">Gouffre Ovni</span> (-565m), the
|
|
||||||
<acronym>GSAB</acronym> expedition deepened
|
|
||||||
<span lang="de">Ahnenschacht</span> and cleared up some unknowns.
|
|
||||||
|
|
||||||
|
<p><b>Situation</b> : <span lang="de" xml:lang="de">Totes Gebirge
|
||||||
|
West - Feuertal</span><br />
|
||||||
|
<b>Depth</b> : -607m<br />
|
||||||
|
<b>Altitude</b> : 1890m ; <span lang="de" xml:lang=
|
||||||
|
"de">Frigoschacht</span> 1875m<br />
|
||||||
|
<b>History</b> : see <a href="782012.htm"><span lang="fr" xml:lang=
|
||||||
|
"fr">Spéalp</span> number 1</a></p>
|
||||||
|
<p>The <acronym>GSAB</acronym> expedition was organised from 5th to
|
||||||
|
29th August, 1977</p>
|
||||||
|
<p>Several individuals from different clubs joined up, and in
|
||||||
|
parallel with the exploration of the <span lang="fr" xml:lang=
|
||||||
|
"fr">Gouffre Ovni</span> (-565m), the <acronym>GSAB</acronym>
|
||||||
|
expedition deepened <span lang="de" xml:lang=
|
||||||
|
"de">Ahnenschacht</span> and cleared up some unknowns.</p>
|
||||||
<ul>
|
<ul>
|
||||||
<li><span lang="de">Frigoschacht</span> (alt 1875m) was connected at a depth
|
<li><span lang="de" xml:lang="de">Frigoschacht</span> (alt 1875m)
|
||||||
of 130m via pitches of 17, 5, 9, 9, 5 and 18m, with a final 11m pitch into
|
was connected at a depth of 130m via pitches of 17, 5, 9, 9, 5 and
|
||||||
<span lang="de">Ahnenschacht</span>.
|
18m, with a final 11m pitch into <span lang="de" xml:lang=
|
||||||
<li>The Vegetable Garden was surveyed
|
"de">Ahnenschacht</span>.</li>
|
||||||
<li>The Yodl system was explored, pushing
|
<li>The Vegetable Garden was surveyed</li>
|
||||||
<span lang="de">Ahnenschacht</span>'s depth to 607m
|
<li>The Yodl system was explored, pushing <span lang="de" xml:lang=
|
||||||
<li>The <acronym>KGB</acronym> system was explored.
|
"de">Ahnenschacht</span>'s depth to 607m</li>
|
||||||
|
<li>The <acronym>KGB</acronym> system was explored.</li>
|
||||||
</ul>
|
</ul>
|
||||||
|
|
||||||
<h3>Yodl system</h3>
|
<h3>Yodl system</h3>
|
||||||
|
<p>From the entrance, after 70m down the <span lang="de" xml:lang=
|
||||||
<p>From the entrance, after 70m down the <span lang="de">Josef
|
"de">Josef schacht</span>, climb down 7m over a large block and
|
||||||
schacht</span>, climb down 7m over a large block and descend about 12m in the
|
descend about 12m in the bottom of a meander. Progress is then in
|
||||||
bottom of a meander. Progress is then in the meander, with a short climb in a
|
the meander, with a short climb in a fault on the left and a 120m
|
||||||
fault on the left and a 120m pitch, in sections of 22m and 100m. Beyond is a
|
pitch, in sections of 22m and 100m. Beyond is a tight canyon with a
|
||||||
tight canyon with a 20m pitch to a sump at -607m (the last part of the 100m
|
20m pitch to a sump at -607m (the last part of the 100m pitch is
|
||||||
pitch is wet).
|
wet).</p>
|
||||||
|
|
||||||
<h4>Participants :</h4>
|
<h4>Participants :</h4>
|
||||||
|
<dl lang="fr" xml:lang="fr">
|
||||||
<dl lang="fr">
|
<dt><acronym>GSAB</acronym> :</dt>
|
||||||
<dt><acronym>GSAB</acronym> :<dd>F Dechany, E Degrave, D Ferrière, J C Hans
|
<dd>F Dechany, E Degrave, D Ferrière, J C Hans</dd>
|
||||||
<dt><acronym>GSAB-CASEO</acronym> :<dd>G Feller, J Kirsch
|
<dt><acronym>GSAB-CASEO</acronym> :</dt>
|
||||||
<dt><acronym>SSSPA</acronym> :<dd>Pierre Dethier
|
<dd>G Feller, J Kirsch</dd>
|
||||||
<dt><acronym>GSREDAN</acronym> :<dd>J P Braun
|
<dt><acronym>SSSPA</acronym> :</dt>
|
||||||
<dt><acronym>ES GEODE</acronym> :<dd>F Saussus
|
<dd>Pierre Dethier</dd>
|
||||||
<dt><acronym>SC</acronym> Calcaires :<dd>J M Piron
|
<dt><acronym>GSREDAN</acronym> :</dt>
|
||||||
<dt><span lang="en">no club affiliations</span> :<dd>T Disneur, H Weber
|
<dd>J P Braun</dd>
|
||||||
|
<dt><acronym>ES GEODE</acronym> :</dt>
|
||||||
|
<dd>F Saussus</dd>
|
||||||
|
<dt><acronym>SC</acronym> Calcaires :</dt>
|
||||||
|
<dd>J M Piron</dd>
|
||||||
|
<dt><span lang="en" xml:lang="en">no club affiliations</span>
|
||||||
|
:</dt>
|
||||||
|
<dd>T Disneur, H Weber</dd>
|
||||||
</dl>
|
</dl>
|
||||||
|
<h3>Mini-expedition from 25th June to 5th July (among
|
||||||
<h3>Mini-expedition from 25th June to 5th July (among individuals)</h3>
|
individuals)</h3>
|
||||||
|
<p>The possibility of a connection with <span lang="fr" xml:lang=
|
||||||
<p>The possibility of a connection with
|
"fr">Epagédure</span> prompted a number of individual
|
||||||
<span lang="fr">Epagédure</span> prompted a number of individual
|
Belgian cavers to organise a mini-expedition.</p>
|
||||||
Belgian cavers to organise a mini-expedition.
|
<p>We didn't make the connection, since a bed of dolomite
|
||||||
|
eliminated all hope. However, the trip did allow several Belgian
|
||||||
<p>We didn't make the connection, since a bed of dolomite eliminated all
|
cavers to discover a new Austrian cave.</p>
|
||||||
hope. However, the trip did allow several Belgian cavers to discover a new
|
<p><b lang="fr" xml:lang="fr">Le Bilan</b> : -500m at first,
|
||||||
Austrian cave.
|
several different endings and a new theory for the pursuit of
|
||||||
|
caves.</p>
|
||||||
<p><b lang="fr">Le Bilan</b> : -500m at first, several different endings
|
<p>-150m in the upstream system from the <span lang="de" xml:lang=
|
||||||
and a new theory for the pursuit of caves.
|
"de">Josef schacht</span> : stopped by something and fissure (a
|
||||||
|
high and tight canyon).</p>
|
||||||
<p>-150m in the upstream system from the <span lang="de">Josef schacht</span>
|
|
||||||
: stopped by something and fissure (a high and tight canyon).
|
|
||||||
|
|
||||||
<p>A new look at some areas: Enigmatic, <acronym>KGB</acronym>,
|
<p>A new look at some areas: Enigmatic, <acronym>KGB</acronym>,
|
||||||
<span lang="fr">Gruyère</span> and Schnaps.
|
<span lang="fr" xml:lang="fr">Gruyère</span> and
|
||||||
|
Schnaps.</p>
|
||||||
<p>A visit and more exploration in the Belgica series.
|
<p>A visit and more exploration in the Belgica series.</p>
|
||||||
|
<p><b>After the Bivouac</b> : a 10m pitch, then turn left into a
|
||||||
<p><b>After the Bivouac </b>: a 10m pitch, then turn left into a small
|
small passage, ignore three pitches to the side, then descend
|
||||||
passage, ignore three pitches to the side, then descend pitches of 8 and 13m
|
pitches of 8 and 13m to arrive at some easy squeezes on the left.
|
||||||
to arrive at some easy squeezes on the left. After this, a climb of 5m and a
|
After this, a climb of 5m and a 42m pitch. Stops in a sand blockage
|
||||||
42m pitch. Stops in a sand blockage at -410m.
|
at -410m.</p>
|
||||||
|
<p>Over the 13m pitch a small passage goes to several climbs in a
|
||||||
<p>Over the 13m pitch a small passage goes to several climbs in a fossil
|
fossil series. There is a 25m pitch and two 10m pitches ending in
|
||||||
series. There is a 25m pitch and two 10m pitches ending in several very tight
|
several very tight chimneys.</p>
|
||||||
chimneys.
|
|
||||||
|
|
||||||
<h4>Participants :</h4>
|
<h4>Participants :</h4>
|
||||||
|
<dl lang="fr" xml:lang="fr">
|
||||||
<dl lang="fr">
|
<dt><acronym>GSAB</acronym>:</dt>
|
||||||
<dt><acronym>GSAB</acronym>:<dd>J P Braun, F Dechany, E Degrave
|
<dd>J P Braun, F Dechany, E Degrave (<span lang="en" xml:lang=
|
||||||
(<span lang="en">organiser</span>), J C Hans
|
"en">organiser</span>), J C Hans</dd>
|
||||||
<dt><acronym>GIPS</acronym>:<dd>F Spinoy
|
<dt><acronym>GIPS</acronym>:</dt>
|
||||||
<dt><acronym>SCUCL</acronym>:<dd>Y Dubois
|
<dd>F Spinoy</dd>
|
||||||
|
<dt><acronym>SCUCL</acronym>:</dt>
|
||||||
|
<dd>Y Dubois</dd>
|
||||||
</dl>
|
</dl>
|
||||||
|
<p>We noted the visit of six members of CARSS who had left their
|
||||||
<p>We noted the visit of six members of CARSS who had left their bag of
|
bag of bolts in the valley.</p>
|
||||||
bolts in the valley.
|
<p lang="fr" xml:lang="fr">Jean Pierre Braun.</p>
|
||||||
|
|
||||||
<p lang="fr">Jean Pierre Braun.
|
|
||||||
<hr />
|
<hr />
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="../index.htm"><acronym>GSAB</acronym> articles list</a></li>
|
<li><a href="../index.htm"><acronym>GSAB</acronym> articles
|
||||||
<li><b lang="de">Ahnenschacht</b> :
|
list</a></li>
|
||||||
<a href="../../../noinfo/1626/50.htm">description</a>, in English</li>
|
<li><b lang="de" xml:lang="de">Ahnenschacht</b> : <a href=
|
||||||
<li><a href="../../../1626/index.htm">Overview</a>
|
"../../../noinfo/1626/50.htm">description</a>, in English</li>
|
||||||
of area 1626, and index to caves</li>
|
<li><a href="../../../1626/index.htm">Overview</a> of area 1626,
|
||||||
<li>Back to <a href="../../../index.htm">Expedition Intro page</a></li>
|
and index to caves</li>
|
||||||
<li><a href="../../../../index.htm">Back to <acronym>CUCC</acronym> Home page</a></li>
|
<li>Back to <a href="../../../index.htm">Expedition Intro
|
||||||
|
page</a></li>
|
||||||
|
<li><a href="../../../../index.htm">Back to <acronym>CUCC</acronym>
|
||||||
|
Home page</a></li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
</html>
|
</html>
|
||||||
|
|||||||
@@ -1,233 +1,223 @@
|
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<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
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<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
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<html lang="fr">
|
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
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<head><meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
<html lang="fr" xmlns="http://www.w3.org/1999/xhtml" xml:lang="fr">
|
||||||
|
<head>
|
||||||
|
<meta http-equiv="Content-Type" content= "text/html; charset=iso-8859-1" />
|
||||||
<title>GSAB: CTS ref. 78.2008</title>
|
<title>GSAB: CTS ref. 78.2008</title>
|
||||||
<LINK rel="alternate" lang="en" href="../en/782008.htm"
|
<link rel="alternate" lang="en" href="../en/782008.htm" title= "Gouffre Ovni"
|
||||||
title="Gouffre Ovni">
|
xml:lang="en" />
|
||||||
<link rel="stylesheet" type="text/css" href="../../../css/main2.css" />
|
<link rel="stylesheet" type="text/css" href= "../../../css/main2.css" />
|
||||||
</head>
|
</head>
|
||||||
<body>
|
<body>
|
||||||
<center><font size=-1>(<acronym>GSAB</acronym>) <b>Spéalp</b> 2 (1978) pp 14-19</font>
|
<p style="text-align: center; font-size: 65%">(<acronym>GSAB</acronym>)
|
||||||
<h1>GOUFFRE OVNI</h1></center>
|
<b>Spéalp</b> 2 (1978) pp 14-19</p>
|
||||||
|
<h1>GOUFFRE OVNI</h1>
|
||||||
<p>L'expédition d'été du <acronym>GSAB</acronym> dans
|
<p>L'expédition d'été du
|
||||||
les <span lang="de">Totes Gebirge</span> à permis l'exploration de ce
|
<acronym>GSAB</acronym> dans les <span lang="de" xml:lang=
|
||||||
|
"de">Totes Gebirge</span> à permis l'exploration de ce
|
||||||
nouveau gouffre de 565m de profondeur. Certes quelque peu
|
nouveau gouffre de 565m de profondeur. Certes quelque peu
|
||||||
éclipsé par ses deux voisins <b lang="de">(Kelli</b> et
|
éclipsé par ses deux voisins <b lang="de" xml:lang=
|
||||||
<b>Empégadure)</b> il n'en reste pas moins une très belle
|
"de">(Kelli</b> et <b>Empégadure)</b> il n'en reste pas
|
||||||
réalisation pour une jeune équipe, peu rodée à la
|
moins une très belle réalisation pour une jeune
|
||||||
première de grande envergure !
|
équipe, peu rodée à la première de
|
||||||
|
grande envergure !</p>
|
||||||
<p>Pour la localisation et découverte on se reporters à
|
<p>Pour la localisation et découverte on se reporters
|
||||||
SPÉALP <acronym>GSAB-SSS</acronym> no. 1
|
à SPÉALP <acronym>GSAB-SSS</acronym> no. 1</p>
|
||||||
|
|
||||||
<h2>Description</h2>
|
<h2>Description</h2>
|
||||||
|
<p>L'entrée, un interstrate dégagé en raison
|
||||||
<p>L'entrée, un interstrate dégagé en raison du courant
|
du courant d'air, donne accès à une série de
|
||||||
d'air, donne accès à une série de puits courte et secs
|
puits courte et secs au debut, qui vont en s'agrandissant en
|
||||||
au debut, qui vont en s'agrandissant en profondeur et en diamètre et
|
profondeur et en diamètre et en s'humidifiant. La
|
||||||
en s'humidifiant. La première exploration de 1976 avait reconnu le
|
première exploration de 1976 avait reconnu le gouffre
|
||||||
gouffre jusqu'a -200, à la base de P.40 (Trou Noir). les explos de
|
jusqu'a -200, à la base de P.40 (Trou Noir). les explos de
|
||||||
cette année débutèrent par la descente d'un beau P.60
|
cette année débutèrent par la descente d'un
|
||||||
de forme constante et légèrement incliné. A le base de
|
beau P.60 de forme constante et légèrement
|
||||||
celui-ci on accède à la seule salle du gouffre: Salle
|
incliné. A le base de celui-ci on accède à la
|
||||||
Galactique où se séparent deux réseaux: l'actif et le
|
seule salle du gouffre: Salle Galactique où se
|
||||||
fossile.
|
séparent deux réseaux: l'actif et le fossile.</p>
|
||||||
|
|
||||||
<h3>Reseau Actif</h3>
|
<h3>Reseau Actif</h3>
|
||||||
|
<p>En aval de la salle, un ressaut mène à une petite
|
||||||
<p>En aval de la salle, un ressaut mène à une petite salle
|
salle entre les blocs, le Nid d'Amour... parce que <span lang="en"
|
||||||
entre les blocs, le Nid d'Amour... parce que <span lang="en">"Love</span>
|
xml:lang="en">"Love</span> Nid" !! (qui osera dire qu'on a pas
|
||||||
Nid" !! (qui osera dire qu'on a pas d'idée.) Entre les blocs s'ouvre
|
d'idée.) Entre les blocs s'ouvre un P.20
|
||||||
un P.20 immédiatement suivit d'un P.25. En fait on arrive dans les
|
immédiatement suivit d'un P.25. En fait on arrive dans les
|
||||||
flancs d'un immense puits remontant dont on descend les 25 derniers
|
flancs d'un immense puits remontant dont on descend les 25 derniers
|
||||||
mètres pour prendre pied sur un fond plat de graviers. Au fond une
|
mètres pour prendre pied sur un fond plat de graviers. Au
|
||||||
cheminée oblique amène un filet d'eau.
|
fond une cheminée oblique amène un filet d'eau.</p>
|
||||||
|
|
||||||
<p>Une fissure marque le départ du méandre
|
<p>Une fissure marque le départ du méandre
|
||||||
Anti-Matière, où l'on rejoint directement le torrent
|
Anti-Matière, où l'on rejoint directement le torrent
|
||||||
soutterain. Celui-ci est d'un débit moyen de deux litres seconde mais
|
soutterain. Celui-ci est d'un débit moyen de deux litres
|
||||||
peut rapidement passer de 10 à 15 litres en cas de crues. Le
|
seconde mais peut rapidement passer de 10 à 15 litres en cas
|
||||||
début du méandre est rectiligne et entrecoupé de 3
|
de crues. Le début du méandre est rectiligne et
|
||||||
petits puits et 2 ressauts. Au sommet du premier s'effectue, par les
|
entrecoupé de 3 petits puits et 2 ressauts. Au sommet du
|
||||||
plafonds, la jonction avec la réseau fossile. Rapidement le
|
premier s'effectue, par les plafonds, la jonction avec la
|
||||||
méandre se fait moins sympathique: haut et étroit, il est de
|
réseau fossile. Rapidement le méandre se fait moins
|
||||||
plus tapissé de boue (l'anti-matière) ce qui rend le
|
sympathique: haut et étroit, il est de plus tapissé
|
||||||
progression assez pénible. Trois puits P.5, P.14 et P.10 coupent la
|
de boue (l'anti-matière) ce qui rend le progression assez
|
||||||
progression. Ce dernier, suivit d'un ressaut de 3m, donne accès
|
pénible. Trois puits P.5, P.14 et P.10 coupent la
|
||||||
à une portion de galerie encombrée par l'argile. Au bout de
|
progression. Ce dernier, suivit d'un ressaut de 3m, donne
|
||||||
celle-ci le torrent se perd dans une fissure qui devient rapidement
|
accès à une portion de galerie encombrée par
|
||||||
impénétrable. La galerie, elle, se prolonge par une branche
|
l'argile. Au bout de celle-ci le torrent se perd dans une fissure
|
||||||
fossile peu large. Après une cinquintaine de mètres, le
|
qui devient rapidement impénétrable. La galerie,
|
||||||
courant d'air s'engage dans un orifice du sol, départ d'un grands
|
elle, se prolonge par une branche fossile peu large. Après
|
||||||
puits de 70m en plusieurs paliers.
|
une cinquintaine de mètres, le courant d'air s'engage dans
|
||||||
|
un orifice du sol, départ d'un grands puits de 70m en
|
||||||
<p>A la moitié on rejoint le torrent que l'on évite par un
|
plusieurs paliers.</p>
|
||||||
puits parallèle fossile. Immédiatement suit un autre puits de
|
<p>A la moitié on rejoint le torrent que l'on évite
|
||||||
55m totalement arrosé et caractérisé par sa section
|
par un puits parallèle fossile. Immédiatement suit un
|
||||||
elliptique et sa pente régulière. Au fond l'eau s'engouffre
|
autre puits de 55m totalement arrosé et
|
||||||
dans une fissure d'environ trois mètres de long, suivie d'un
|
caractérisé par sa section elliptique et sa pente
|
||||||
étroit méandre que nous n'avons pas pu forcer.
|
régulière. Au fond l'eau s'engouffre dans une fissure
|
||||||
|
d'environ trois mètres de long, suivie d'un étroit
|
||||||
|
méandre que nous n'avons pas pu forcer.</p>
|
||||||
<h3>Réseau Fossile</h3>
|
<h3>Réseau Fossile</h3>
|
||||||
|
|
||||||
<p>En amont de la Salle Galactique, une lucarne à quelques
|
<p>En amont de la Salle Galactique, une lucarne à quelques
|
||||||
mètres de hauteur, permet d'accéder à une galerie de
|
mètres de hauteur, permet d'accéder à une
|
||||||
belle dimensions (3x3 de moyenne). La Galerie des Petits Hommes Vertes. On
|
galerie de belle dimensions (3x3 de moyenne). La Galerie des Petits
|
||||||
bute sur un ressaut de 3m au bas duquel s'écoule un petit filet
|
Hommes Vertes. On bute sur un ressaut de 3m au bas duquel
|
||||||
d'eau, qui emprunte un méandre creusé en dessous de la galerie
|
s'écoule un petit filet d'eau, qui emprunte un
|
||||||
fossile (voir plus loin). Après un rétrécissement et un
|
méandre creusé en dessous de la galerie fossile (voir
|
||||||
ressaut, le galerie se termine sur un éboulis entre lequel il est
|
plus loin). Après un rétrécissement et un
|
||||||
encore possible de faire une dizaine de mètres.
|
ressaut, le galerie se termine sur un éboulis entre lequel
|
||||||
|
il est encore possible de faire une dizaine de mètres.</p>
|
||||||
<p>En suivent le méandre sous le galerie on aboutit au Puits de la
|
<p>En suivent le méandre sous le galerie on aboutit au Puits
|
||||||
Gomete (découvert par les Gaumais) P.60 arrosé dans sa
|
de la Gomete (découvert par les Gaumais) P.60 arrosé
|
||||||
dernière partie par le pipi. A la base du puits d'amorce le
|
dans sa dernière partie par le pipi. A la base du puits
|
||||||
méandre des Mutants. C'est le méandre pour masos par
|
d'amorce le méandre des Mutants. C'est le méandre
|
||||||
excellence: bas, étroit et accrochant... Il se termine par un
|
pour masos par excellence: bas, étroit et accrochant... Il
|
||||||
série de ressauts et un P.30 jonctionnant avec le réseau
|
se termine par un série de ressauts et un P.30 jonctionnant
|
||||||
actif.
|
avec le réseau actif.</p>
|
||||||
|
|
||||||
<h2>Géologie</h2>
|
<h2>Géologie</h2>
|
||||||
|
|
||||||
<h3>Generalité</h3>
|
<h3>Generalité</h3>
|
||||||
|
<p>Du point de vue géologique, le Gouffre Ovni est un
|
||||||
<p>Du point de vue géologique, le Gouffre Ovni est un exemple typique
|
exemple typique des phénomènes karstiques du massif
|
||||||
des phénomènes karstiques du massif et mêum;me de la plus
|
et même de la plus grande partie du karst Autrichien.
|
||||||
grande partie du karst Autrichien. On n'a pas ici de zone de puits donnant
|
On n'a pas ici de zone de puits donnant sur un collecteur au niveau
|
||||||
sur un collecteur au niveau imperméable (type Pyrénéen)
|
imperméable (type Pyrénéen) ni de gouffres
|
||||||
ni de gouffres étroits verticaux (type Vercors et Chartreuse). Les
|
étroits verticaux (type Vercors et Chartreuse). Les facteurs
|
||||||
facteurs primordiaux de formation sont la fracturation orogénique
|
primordiaux de formation sont la fracturation orogénique
|
||||||
intense doublée d'un climat très pluvieux et d'importantes
|
intense doublée d'un climat très pluvieux et
|
||||||
chutes de neige depuis le début de l'ère.
|
d'importantes chutes de neige depuis le début de
|
||||||
|
l'ère.</p>
|
||||||
<p>Ces gouffres s'ouvrent donc généralement au profit d'une
|
<p>Ces gouffres s'ouvrent donc généralement au profit
|
||||||
forme simple de discontinuité dans les calcaires (diaclase,
|
d'une forme simple de discontinuité dans les calcaires
|
||||||
stratification). Puis ils vont en s'élargissant de plus en plus pour
|
(diaclase, stratification). Puis ils vont en s'élargissant
|
||||||
rejoindre des phénomènes de grande envergure (faille,
|
de plus en plus pour rejoindre des phénomènes de
|
||||||
super-diaclase). Le collecteur, quand il existe, n'est
|
grande envergure (faille, super-diaclase). Le collecteur, quand il
|
||||||
généralement que très court et très près
|
existe, n'est généralement que très court et
|
||||||
de la resurgence.
|
très près de la resurgence.</p>
|
||||||
|
|
||||||
<h3>Le Gouffre Ovni</h3>
|
<h3>Le Gouffre Ovni</h3>
|
||||||
|
<p>L'Orifice du gouffre est un interstrate dégagé sur
|
||||||
<p>L'Orifice du gouffre est un interstrate dégagé sur deux
|
deux mètres environ. C'est ensuite une série de
|
||||||
mètres environ. C'est ensuite une série de puits, assez
|
puits, assez petits, formés dans une diaclase assez sinueuse
|
||||||
petits, formés dans une diaclase assez sinueuse s'élargissant
|
s'élargissant suivant le stratification et le pendage
|
||||||
suivant le stratification et le pendage très fort en cette zone. Aux
|
très fort en cette zone. Aux environs de -200, on commence
|
||||||
environs de -200, on commence à sentir l'influence d'un autre
|
à sentir l'influence d'un autre facteur. Les puits
|
||||||
facteur. Les puits deviennent de plus en plus grands et les parois de plus
|
deviennent de plus en plus grands et les parois de plus en plus
|
||||||
en plus nettes. La section devient caractéristique d'une faille
|
nettes. La section devient caractéristique d'une faille
|
||||||
orientée sommairement O-E (voir schéma no. 1)
|
orientée sommairement O-E (voir schéma no. 1)</p>
|
||||||
|
<div class="centre">
|
||||||
<p><center><img alt="schéma 1, 3k gif" width=512 height=128
|
<img alt="schéma 1, 3k gif" width="512" height="128"
|
||||||
src="../ovnif1.png"></center>
|
src="../ovnif1.png" /></div>
|
||||||
|
<p>Cette faille va déterminer la majeure partie de la
|
||||||
<p>Cette faille va déterminer la majeure partie de la formation du
|
formation du gouffre. En effet, la suite du réseau s'est
|
||||||
gouffre. En effet, la suite du réseau s'est creusée à
|
creusée à différents niveaux de cette faille.
|
||||||
différents niveaux de cette faille. (schéma no. 2)
|
(schéma no. 2)</p>
|
||||||
|
<p><img class="onleft" alt="Schéma 2, 3k gif" width="275" height="385"
|
||||||
<p><img alt="Schéma 2, 3k gif" width=275 height=385 align="left"
|
src="../ovnif2.png" />
|
||||||
hspace=10 vspace=10 src="../ovnif2.png">
|
<b>Schéma 2: Plan de la faille</b></p>
|
||||||
|
|
||||||
<b>Schéma 2: Plan de la faille</b>
|
|
||||||
|
|
||||||
<ul>
|
<ul>
|
||||||
<li>1e le puits Zorglub et les cheminées du Père Noël.
|
<li>1e le puits Zorglub et les cheminées du Père
|
||||||
|
Noël.</li>
|
||||||
<li>2e La Salle Galactique et le premier tiers de la Galerie des Petits Hommes
|
<li>2e La Salle Galactique et le premier tiers de la Galerie des
|
||||||
Vertes (les deux tiers restant sont en interstrates).
|
Petits Hommes Vertes (les deux tiers restant sont en
|
||||||
|
interstrates).</li>
|
||||||
<li>3e Le puits à Descendre le Temps et le puits de la Gaumette avec
|
<li>3e Le puits à Descendre le Temps et le puits de la
|
||||||
le méandre des Mutants.
|
Gaumette avec le méandre des Mutants.</li>
|
||||||
|
|
||||||
<li>4e La partie large du méandre Anti-Matière (Le
|
<li>4e La partie large du méandre Anti-Matière (Le
|
||||||
décalage de cette partie) par rapport au reste (plan) est du au fait
|
décalage de cette partie) par rapport au reste (plan) est du
|
||||||
que la faille est cassée en son milieu.
|
au fait que la faille est cassée en son milieu.</li>
|
||||||
|
|
||||||
</ul>
|
</ul>
|
||||||
<br clear="all">
|
<p style="clear: both">Suite à la partie large du méandre
|
||||||
|
Anti-Matière, une zone très étroite marque la
|
||||||
<p>Suite à la partie large du méandre Anti-Matière, une
|
jonction avec une seconde faille orientée SO-NE qui à
|
||||||
zone très étroite marque la jonction avec une seconde faille
|
elle seule déterminera toute la suite de gouffre. On
|
||||||
orientée SO-NE qui à elle seule déterminera toute la
|
pourrait croire en voyant la topo, qu'il s'agit d'un méandre
|
||||||
suite de gouffre. On pourrait croire en voyant la topo, qu'il s'agit d'un
|
en diaclase vu sa sinuosité. En fait la partie rectiligne et
|
||||||
méandre en diaclase vu sa sinuosité. En fait la partie
|
large de cette faille est impracticable car elle surplombe
|
||||||
rectiligne et large de cette faille est impracticable car elle surplombe
|
|
||||||
continuellement un à-pic de 6m dont les lèvres sont
|
continuellement un à-pic de 6m dont les lèvres sont
|
||||||
déversées et boueuses. L'on est donc obligé d'emprunter
|
déversées et boueuses. L'on est donc obligé
|
||||||
le fond en surcreusement. Plus loin on suit une partie plus large, bien
|
d'emprunter le fond en surcreusement. Plus loin on suit une partie
|
||||||
marquée par la faille, Elle est suivie par un décrochement
|
plus large, bien marquée par la faille, Elle est suivie par
|
||||||
où se perd le ruisseau. La galerie, elle, continue dans la
|
un décrochement où se perd le ruisseau. La galerie,
|
||||||
mêum;me direction, toujours déterminée par la fissuration.
|
elle, continue dans la même direction, toujours
|
||||||
La zone de puits qui fait suite se développe également dans la
|
déterminée par la fissuration. La zone de puits qui
|
||||||
partie inférieure de la faille; bien qu'elle ait l'apparence d'une
|
fait suite se développe également dans la partie
|
||||||
conduite forcée.
|
inférieure de la faille; bien qu'elle ait l'apparence d'une
|
||||||
|
conduite forcée.</p>
|
||||||
<h3>Possibilités de Continuation</h3>
|
<h3>Possibilités de Continuation</h3>
|
||||||
|
<p>Comme on le remarque à l'observation de la topo, la
|
||||||
<p>Comme on le remarque à l'observation de la topo, la Galerie
|
Galerie Principale se prolonge et n'a pas été
|
||||||
Principale se prolonge et n'a pas été explorée. Il
|
explorée. Il semble que l'on soit en présence d'un
|
||||||
semble que l'on soit en présence d'un simple phénomène
|
simple phénomène de régression et que
|
||||||
de régression et que logiquement on devrait trouver une autre
|
logiquement on devrait trouver une autre série de puits
|
||||||
série de puits fossiles permettant de rejoindre le niveau de base.
|
fossiles permettant de rejoindre le niveau de base. (Schéma
|
||||||
(Schéma no. 3 et 4)
|
no. 3 et 4)</p>
|
||||||
|
<div class="centre">
|
||||||
<center><p><img alt="Schéma 3 - 5k gif" width=480 height=480
|
<img style="border: 2px solid black" alt="Schéma 3 - 5k gif" width="480" height="480"
|
||||||
src="ovnif3.png"><p><img alt="Schéma 4 - 3k gif" width=325 height=340
|
src="ovnif3.png" />
|
||||||
src="ovnif4.png"></center>
|
<img style="border: 2px solid black" alt="Schéma 4 - 3k gif" width="325" height="340"
|
||||||
|
src="ovnif4.png" />
|
||||||
<p>La puissance du Dachsteinkalk (calcaire jurassique granuleux) avoisine
|
</div>
|
||||||
les 700 mètres à partir de l'entrée.
|
<p>La puissance du Dachsteinkalk (calcaire jurassique granuleux)
|
||||||
|
avoisine les 700 mètres à partir de
|
||||||
|
l'entrée.</p>
|
||||||
<h3>Météorologie</h3>
|
<h3>Météorologie</h3>
|
||||||
|
<p><img alt="Schéma 5 - 2k gif" width="265" height="435"
|
||||||
<p><img alt="Schéma 5 - 2k gif" width=265 height=435 align=right
|
class="onright" src="../ovnif5.png" />
|
||||||
hspace=10 vspace=0 src="../ovnif5.png">
|
<b>Schéma 5: Schéma du courant d'air aux principaux
|
||||||
<b>Schéma 5: Schéma du courant d'air aux principaux points de
|
points de perception:</b></p>
|
||||||
perception:</b>
|
<p>Comme nous l'avons déja dit, c'est un violent courant
|
||||||
|
d'air qui etire notre attention sur l'Ovni. Ce courant d'air
|
||||||
<p>Comme nous l'avons déja dit, c'est un violent courant d'air qui
|
étant soufflant et la période étant chause
|
||||||
etire notre attention sur l'Ovni. Ce courant d'air étant soufflant et
|
(été), nous devrions logiquement nous trouver en
|
||||||
la période étant chause (été), nous devrions
|
présence d'une entrée intermédiaire. Vu la
|
||||||
logiquement nous trouver en présence d'une entrée
|
violence du courant d'air froid chassé, l'existence d'une
|
||||||
intermédiaire. Vu la violence du courant d'air froid chassé,
|
entrée supérieure est quasi certaine. La prospection
|
||||||
l'existence d'une entrée supérieure est quasi certaine. La
|
du mamelon dominant l'entrée n'a pas donné resultats.
|
||||||
prospection du mamelon dominant l'entrée n'a pas donné
|
Il s'agit là d'un objectif à revoir car la
|
||||||
resultats. Il s'agit là d'un objectif à revoir car la
|
végétation et les aspics ne nous ont pas permis
|
||||||
végétation et les aspics ne nous ont pas permis d'operer un
|
d'operer un quadrillage efficace.</p>
|
||||||
quadrillage efficace.
|
<p>La jonction avec cet orofice supérieur devrait
|
||||||
|
s'effectuer au niveau de la galerie des Petits Hommes Vertes; soit
|
||||||
<p>La jonction avec cet orofice supérieur devrait s'effectuer au
|
par la cheminée arrosée de la fin de la faille I,
|
||||||
niveau de la galerie des Petits Hommes Vertes; soit par la cheminée
|
soit par les plafonds aux 2/3, là ou l'on perd le courant
|
||||||
arrosée de la fin de la faille I, soit par les plafonds aux 2/3,
|
d'air. D'autre part, la présence au fond d'un courant d'air
|
||||||
là ou l'on perd le courant d'air. D'autre part, la présence au
|
violent lui aussi, laissarait présumer d'une sortie
|
||||||
fond d'un courant d'air violent lui aussi, laissarait présumer d'une
|
inférieure, vraisemblablement d'une résurgence
|
||||||
sortie inférieure, vraisemblablement d'une résurgence fossile.
|
fossile. Cependant il ne s'agit là que de suppositions, les
|
||||||
Cependant il ne s'agit là que de suppositions, les caprices d'un
|
caprices d'un courant d'air sont trop délicats à
|
||||||
courant d'air sont trop délicats à traiter.
|
traiter.</p>
|
||||||
|
<h3 style="clear: both">Conclusions</h3>
|
||||||
<br clear="all">
|
<p>On voit par la brève analyse du gouffre que les chances
|
||||||
|
de continuation ne sont pas minimes. Or cette cavité n'est
|
||||||
<h3>Conclusions</h3>
|
pas extrèmement difficile d'accès, ni d'exploration.
|
||||||
|
Des travaux pourraient y être repris très
|
||||||
<p>On voit par la brève analyse du gouffre que les chances de
|
prochainement, mais il ne s'agit cependant que d'un objectif
|
||||||
continuation ne sont pas minimes. Or cette cavité n'est pas
|
secondaire comparé aux possibilités
|
||||||
extrèmement difficile d'accès, ni d'exploration. Des travaux
|
Autrichiennes.</p>
|
||||||
pourraient y êum;tre repris très prochainement, mais il ne s'agit
|
<p>G.Feller. GSAB.</p>
|
||||||
cependant que d'un objectif secondaire comparé aux
|
|
||||||
possibilités Autrichiennes.
|
|
||||||
|
|
||||||
<p>G.Feller. GSAB.
|
|
||||||
<hr />
|
<hr />
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<p lang="en"><ul>
|
<p lang="en" xml:lang="en"> </p>
|
||||||
|
<ul>
|
||||||
<li><a href="../index.htm">GSAB articles list</a></li>
|
<li><a href="../index.htm">GSAB articles list</a></li>
|
||||||
<li><span lang="fr">Gouffre Ovni</span> :
|
<li><span lang="fr" xml:lang="fr">Gouffre Ovni</span> : <a href=
|
||||||
<a href="../../../noinfo/1626/122.htm">description</a>, in English</li>
|
"../../../noinfo/1626/122.htm">description</a>, in English</li>
|
||||||
<li><a href="../../../1626/index.htm">Overview</a>
|
<li><a href="../../../1626/index.htm">Overview</a> of area 1626,
|
||||||
of area 1626, and index to caves</li>
|
and index to caves</li>
|
||||||
<li>Back to <a href="../../../index.htm">Expedition Intro page</a></li>
|
<li>Back to <a href="../../../index.htm">Expedition Intro
|
||||||
|
page</a></li>
|
||||||
<li><a href="../../../../index.htm">Back to CUCC Home page</a></li>
|
<li><a href="../../../../index.htm">Back to CUCC Home page</a></li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
|
|||||||
@@ -1,414 +1,401 @@
|
|||||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
|
||||||
<html lang="fr">
|
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
||||||
|
<html lang="fr" xmlns="http://www.w3.org/1999/xhtml" xml:lang="fr">
|
||||||
<head>
|
<head>
|
||||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
<meta http-equiv="Content-Type" content=
|
||||||
|
"text/html; charset=iso-8859-1" />
|
||||||
<title>GSAB: CTS ref. 78.2012 (en Français)</title>
|
<title>GSAB: CTS ref. 78.2012 (en Français)</title>
|
||||||
<LINK rel="alternate" lang="en" href="../en/782012.htm"
|
<link rel="alternate" lang="en" href="../en/782012.htm" title=
|
||||||
title="Description of the principal caves in the West of the massif">
|
"Description of the principal caves in the West of the massif"
|
||||||
<link rel="stylesheet" type="text/css" href="../../../css/main2.css" />
|
xml:lang="en" />
|
||||||
|
<link rel="stylesheet" type="text/css" href=
|
||||||
|
"../../../css/main2.css" />
|
||||||
</head>
|
</head>
|
||||||
<body>
|
<body>
|
||||||
<center><font size=-1>(<acronym>GSAB</acronym>) Spéalp 1
|
<p style="text-align: center; font-size: 65%">(<acronym>GSAB</acronym>) Spéalp 1
|
||||||
(Juin 1977) pp 33-49</font>
|
(Juin 1977) pp 33-49</p>
|
||||||
|
<h1 lang="de" xml:lang="de">TOTES GEBIRGE</h1>
|
||||||
<h1 lang="de">TOTES GEBIRGE</h1>
|
<h2 style="text-align: center">Description des principaux gouffres de la zone
|
||||||
|
ouest du massif</h2>
|
||||||
<h2>Description des principaux gouffres de la zone ouest du massif</h2></center>
|
<p><b>Introduction</b>: le choix de cette zone est tout à
|
||||||
|
fait arbitraire. En effet, il y a très peu de chance que
|
||||||
<p><b>Introduction</b>: le choix de cette zone est tout à fait
|
cette zone soit drainée par le même complexe
|
||||||
arbitraire. En effet, il y a très peu de chance que cette zone soit
|
hydrologique. Si pour certains réseaux la ou les resurgences
|
||||||
drainée par le même complexe hydrologique. Si pour certains
|
présumées sont pratiquement certaines, il n'en est
|
||||||
réseaux la ou les resurgences présumées sont
|
pas de même pour les autres qui peuvent prendre des
|
||||||
pratiquement certaines, il n'en est pas de même pour les autres qui
|
directions totalement opposées ! Notre choix est fonction
|
||||||
peuvent prendre des directions totalement opposées ! Notre choix est
|
des moyen d'accès: routes, telebenne, sentier, refuge etc.
|
||||||
fonction des moyen d'accès: routes, telebenne, sentier, refuge etc.
|
Les <span lang="de" xml:lang="de">Totes Gebirge</span> qui sont un
|
||||||
Les <span lang="de">Totes Gebirge</span> qui sont un des plus grands massifs
|
des plus grands massifs karstique d'Autriche n'est aisément
|
||||||
karstique d'Autriche n'est aisément accessible qu'en certains
|
accessible qu'en certains endroits, dont celoi que nous passons en
|
||||||
endroits, dont celoi que nous passons en revue. De cette zone il y a
|
revue. De cette zone il y a plusieurs kilomètres de lapiaz
|
||||||
plusieurs kilomètres de lapiaz totalement vierge. Plusieurs heures de
|
totalement vierge. Plusieurs heures de marche sont necessaire pour
|
||||||
marche sont necessaire pour y aller. De plus dans cette zone seule une infime
|
y aller. De plus dans cette zone seule une infime partie est plus
|
||||||
partie est plus ou moins prospectée. Il s'agit de la vallée de
|
ou moins prospectée. Il s'agit de la vallée de
|
||||||
<span lang="de">Raucherkar</span>, de la <span lang="de">Feuertal</span> et
|
<span lang="de" xml:lang="de">Raucherkar</span>, de la <span lang=
|
||||||
des abords du sentier qui y conduit ainsi que des parois nord du <span
|
"de" xml:lang="de">Feuertal</span> et des abords du sentier qui y
|
||||||
lang="de">Hagender Kogel</span> dans lesquelles s'ouvre la <span
|
conduit ainsi que des parois nord du <span lang="de" xml:lang=
|
||||||
lang="de">Tropfsteinhöhle</span> qui était extraordinairement
|
"de">Hagender Kogel</span> dans lesquelles s'ouvre la <span lang=
|
||||||
concrétionnée mais qui est complètement pillée
|
"de" xml:lang="de">Tropfsteinhöhle</span> qui était
|
||||||
aujourd'hui.
|
extraordinairement concrétionnée mais qui est
|
||||||
|
complètement pillée aujourd'hui.</p>
|
||||||
<p><b>Recherches Spéléo</b>: ont été
|
<p><b>Recherches Spéléo</b>: ont été
|
||||||
principalement menées par nos amis Autrichiens de Haute-Autriche, un
|
principalement menées par nos amis Autrichiens de
|
||||||
groupe Anglais, deux groupes Français et nous. Pour notre part nous
|
Haute-Autriche, un groupe Anglais, deux groupes Français et
|
||||||
n'avons pratiquement pas prospecté, sauf en 1976. Nous nous sommes
|
nous. Pour notre part nous n'avons pratiquement pas
|
||||||
contentés de descendre certains trous repérés et encore
|
prospecté, sauf en 1976. Nous nous sommes contentés
|
||||||
pas tous ( nous le regrettons amèrement aujourd'hui car d'autre ont
|
de descendre certains trous repérés et encore pas
|
||||||
trouvé à notre place ). Notre effort s'est surtout porté
|
tous ( nous le regrettons amèrement aujourd'hui car d'autre
|
||||||
sur l'<span lang="de">Ahnenschacht</span>, mais un manque chronique de
|
ont trouvé à notre place ). Notre effort s'est
|
||||||
spéléos valables et de pratique de pointe ( en 75 nous
|
surtout porté sur l'<span lang="de" xml:lang=
|
||||||
étions 4 ). ne nous ont pas permis d'avancer comme nous l'aurions
|
"de">Ahnenschacht</span>, mais un manque chronique de
|
||||||
désirée.
|
spéléos valables et de pratique de pointe ( en 75
|
||||||
|
nous étions 4 ). ne nous ont pas permis d'avancer comme nous
|
||||||
<p><b>Geologie-Hydrologie</b>: n'étant pas géologue et n'en
|
l'aurions désirée.</p>
|
||||||
ayant pas au groupe nous ne ferons qu'esquisser les grandes lignes. La grosse
|
<p><b>Geologie-Hydrologie</b>: n'étant pas géologue
|
||||||
majorité de la région est constituée de <span
|
et n'en ayant pas au groupe nous ne ferons qu'esquisser les grandes
|
||||||
lang="de">Dachsteinkalk</span> avec aussi certaines poches de Dolomie bien
|
lignes. La grosse majorité de la région est
|
||||||
visibles à certains endroits et notamment au nord de l'<span
|
constituée de <span lang="de" xml:lang=
|
||||||
lang="de">Ahnenschacht</span>. Un autre problème, la présence
|
"de">Dachsteinkalk</span> avec aussi certaines poches de Dolomie
|
||||||
d'une nappe de charriage entre -400 et -500 qui risque de créer des
|
bien visibles à certains endroits et notamment au nord de
|
||||||
ennuis au Gouffre des Aieux. Pour le <span lang="de">Raucherkar</span>, le
|
l'<span lang="de" xml:lang="de">Ahnenschacht</span>. Un autre
|
||||||
drainage est pratiquement certain: la resurgence de crue serait la <span
|
problème, la présence d'une nappe de charriage entre
|
||||||
lang="de">Nagelsteghöhle</span> au sud du trou et au nord d'<span
|
-400 et -500 qui risque de créer des ennuis au Gouffre des
|
||||||
lang="de">Altaussee</span>. La jonction entre les deux devrait être
|
Aieux. Pour le <span lang="de" xml:lang="de">Raucherkar</span>, le
|
||||||
possible soit directement soit par plongée. Le QUELLI devrait lui
|
drainage est pratiquement certain: la resurgence de crue serait la
|
||||||
aussi se diriger dans la même direction si du moins on en croit le
|
<span lang="de" xml:lang="de">Nagelsteghöhle</span> au sud du
|
||||||
pendage. Néanmoins le Quelli s'ouvrant à 2km au NE du <span
|
trou et au nord d'<span lang="de" xml:lang="de">Altaussee</span>.
|
||||||
lang="de">Raucherkar</span>, il faut être très
|
La jonction entre les deux devrait être possible soit
|
||||||
réservé.
|
directement soit par plongée. Le QUELLI devrait lui aussi se
|
||||||
|
diriger dans la même direction si du moins on en croit le
|
||||||
<p>L'<b lang="de">AHNENSCHACHT</b> se situé dans une zone
|
pendage. Néanmoins le Quelli s'ouvrant à 2km au NE du
|
||||||
limitée très complèxe, et peut très bien se
|
<span lang="de" xml:lang="de">Raucherkar</span>, il faut être
|
||||||
diriger dans plusieurs directions totalement opposées. Il est
|
très réservé.</p>
|
||||||
très possible que plusieurs directions sont valables. Les explorations
|
<p>L'<b lang="de" xml:lang="de">AHNENSCHACHT</b> se situé
|
||||||
ne sont pas suffisamment éloignées en plan pour pouvoir se
|
dans une zone limitée très complèxe, et peut
|
||||||
prononcer.
|
très bien se diriger dans plusieurs directions totalement
|
||||||
|
opposées. Il est très possible que plusieurs
|
||||||
<p>L'<b>EMPAGADURE</b> et le <b>Gouffre OVNI</b> devraient normalement se
|
directions sont valables. Les explorations ne sont pas suffisamment
|
||||||
diriger vers le nord ou de très nombreuses resurgences sont visibles.
|
éloignées en plan pour pouvoir se prononcer.</p>
|
||||||
Les autres directions ne sont cependant pas à négliger. De
|
<p>L'<b>EMPAGADURE</b> et le <b>Gouffre OVNI</b> devraient
|
||||||
toutes façons les explorations serons poussées beaucoup plus
|
normalement se diriger vers le nord ou de très nombreuses
|
||||||
loin cette année et nous y verrons peut-être plus clair.
|
resurgences sont visibles. Les autres directions ne sont cependant
|
||||||
|
pas à négliger. De toutes façons les
|
||||||
<p>Du point de vue Hydrologique il est très regrettable qu'aucunes
|
explorations serons poussées beaucoup plus loin cette
|
||||||
colorations n'aient pu être réalisées et cela par manque
|
année et nous y verrons peut-être plus clair.</p>
|
||||||
d'autorisation de collaboration et d'interet !!!
|
<p>Du point de vue Hydrologique il est très regrettable
|
||||||
|
qu'aucunes colorations n'aient pu être
|
||||||
|
réalisées et cela par manque d'autorisation de
|
||||||
<h2 lang="de"><a id="id55">RAUCHERKARHÖHLENSYSTEM</a></h2>
|
collaboration et d'interet !!!</p>
|
||||||
|
<h2 lang="de" xml:lang="de"><a id="id55" name=
|
||||||
<p>Styrie <span lang="de">Totes Gebirge</span> 1632m<br>
|
"id55">RAUCHERKARHÖHLENSYSTEM</a></h2>
|
||||||
|
<p>Styrie <span lang="de" xml:lang="de">Totes Gebirge</span>
|
||||||
Profondeur: -723m<br>
|
1632m<br />
|
||||||
|
Profondeur: -723m<br />
|
||||||
Développement: environ 20km<br>
|
Développement: environ 20km<br />
|
||||||
|
Fond: Siphon</p>
|
||||||
Fond: Siphon
|
<p><b>Situation</b>: partie Ouest du <span lang="de" xml:lang=
|
||||||
|
"de">Totes Gebirge</span>, au Sud de <span lang="de" xml:lang=
|
||||||
<p><b>Situation</b>: partie Ouest du <span lang="de">Totes Gebirge</span>, au
|
"de">Schönberg</span>, 2km au SO du <span lang="de" xml:lang=
|
||||||
Sud de <span lang="de">Schönberg</span>, 2km au SO du
|
"de">Ahnenschacht</span>.</p>
|
||||||
<span lang="de">Ahnenschacht</span>.
|
<p><b>Historique</b>: la première explo commence en 1961. En
|
||||||
|
65 la cavité comporte 6 km de galeries pour 246m de
|
||||||
<p><b>Historique</b>: la première explo commence en 1961. En 65 la
|
profondeur. L'expé fédérale Autrichienne de 65
|
||||||
cavité comporte 6 km de galeries pour 246m de profondeur.
|
permet d'atteindre -530m. En 73, le <span lang="de" xml:lang=
|
||||||
L'expé fédérale Autrichienne de 65 permet d'atteindre
|
"de"><acronym>LVfHK</acronym> Oberösterreich &
|
||||||
-530m. En 73, le <span lang="de"><acronym>LVfHK</acronym> Oberösterreich
|
Steiermark</span> touchent le siphon à -723m.
|
||||||
& Steiermark</span> touchent le siphon à -723m.
|
Développement 18km.</p>
|
||||||
Développement 18km.
|
<p><b>Description</b>: le gouffre ne comprend pas moins de 13
|
||||||
|
entrées étagées entre 1500 et 1632m
|
||||||
<p><b>Description</b>: le gouffre ne comprend pas moins de 13 entrées
|
d'altitude. Le réseau labyrinthique comporte plusieurs
|
||||||
étagées entre 1500 et 1632m d'altitude. Le réseau
|
étages se développant en grande partie vers le Sud en
|
||||||
labyrinthique comporte plusieurs étages se développant en
|
direction de la <b lang="de" xml:lang="de">NAGELSTEGHÖHLE</b>
|
||||||
grande partie vers le Sud en direction de la
|
( Resurgence probable, alt.: 850m ). Il est intéressant de
|
||||||
<b lang="de">NAGELSTEGHÖHLE</b> ( Resurgence probable, alt.: 850m ). Il
|
noter que le siphon terminal a pu être atteint en contournant
|
||||||
est intéressant de noter que le siphon terminal a pu être
|
systematiquement les puits de plus de 90-40m.</p>
|
||||||
atteint en contournant systematiquement les puits de plus de 90-40m.
|
<p><b>Auteur de la Fiche</b>: Etienne Degrave.</p>
|
||||||
|
<h2><a id="id120" name="id120">QUELLI</a> ou <span lang="de"
|
||||||
<p><b>Auteur de la Fiche</b>: Etienne Degrave.
|
xml:lang="de">KACHERLSCHACHT</span></h2>
|
||||||
|
<p><span lang="de" xml:lang="de">Totes Gebirge</span> Ouest -
|
||||||
|
<span lang="de" xml:lang="de">Feuertal -
|
||||||
<h2><a id="id120">QUELLI</a> ou
|
Schönberg</span><br />
|
||||||
<span lang="de">KACHERLSCHACHT</span></h2>
|
Profondeur: -708m<br />
|
||||||
|
Altitude: ~1950m</p>
|
||||||
<p><span lang="de">Totes Gebirge</span> Ouest - <span lang="de">Feuertal -
|
<p><b>Historique</b>: Découvert en 1973 par le
|
||||||
Schönberg</span><br>
|
<acronym>GSAB</acronym> sous le nom de T3. Redécouvert en
|
||||||
|
juilllet 76 par J.M.Piron exploré du 12 au 23 juillet par
|
||||||
Profondeur: -708m<br>
|
A.C.Toulon, S.C.Toulon, Lou Darboun et Spéléo
|
||||||
|
Ragaie.</p>
|
||||||
Altitude: ~1950m
|
<p><b>Description</b>: P8, p19, p83, p33, p24, p17, p5, p33, p24,
|
||||||
|
p9, p33, p27, p103. A -400m, on accède à une vaste
|
||||||
<p><b>Historique</b>: Découvert en 1973 par le <acronym>GSAB</acronym>
|
galerie avec amont et aval. La galerie aval débouche au
|
||||||
sous le nom de T3. Redécouvert en juilllet 76 par J.M.Piron
|
sommet d'un p84. Suit alors un méandre entrecoupé de
|
||||||
exploré du 12 au 23 juillet par A.C.Toulon, S.C.Toulon, Lou Darboun et
|
petits puits dont un p 15 terminus de l'exploration à
|
||||||
Spéléo Ragaie.
|
-708m.</p>
|
||||||
|
<p>Etienne Degrave</p>
|
||||||
<p><b>Description</b>: P8, p19, p83, p33, p24, p17, p5, p33, p24, p9, p33,
|
<h2><a id="id117" name="id117">EMPAGADURE</a></h2>
|
||||||
p27, p103. A -400m, on accède à une vaste galerie avec amont et
|
<p><span lang="de" xml:lang="de">Totes Gebirge</span> Ouest -
|
||||||
aval. La galerie aval débouche au sommet d'un p84. Suit alors un
|
<span lang="de" xml:lang="de">Hintergras</span><br />
|
||||||
méandre entrecoupé de petits puits dont un p 15 terminus de
|
Profondeur: -587m<br />
|
||||||
l'exploration à -708m.
|
Altitude: 1610m</p>
|
||||||
|
<p><b>Historique</b>: Découvert en juillet 1976 par
|
||||||
<p>Etienne Degrave
|
F.Vergier. Exploré du 12 au 23 juillet 76 par l'A.C.Toulon,
|
||||||
|
S.C.Toulon, Lou Darboun, Spéléo Ragaie.</p>
|
||||||
<h2><a id="id117">EMPAGADURE</a></h2>
|
<p><b>Description</b>: jusqu'à -287m, le gouffre est
|
||||||
|
constitué de puits modestes entrecoupés de
|
||||||
<p><span lang="de">Totes Gebirge</span> Ouest - <span lang="de">Hintergras</span><br>
|
méandres étroits : p8, p12, p17, p9, p20, p3, p12,
|
||||||
|
p30, p7, p6, p9, p8, p7, p5, p34, p6, p8, p5, p9. A -287m, un p21
|
||||||
Profondeur: -587m<br>
|
permet de déboucher dans une grande salle. L'eau disparait
|
||||||
|
dans les éboulis pour réapparaitre dans toute une
|
||||||
Altitude: 1610m
|
série de puits arrosés dont le plus profond mesure
|
||||||
|
30m. Les crues ont empéché l'exploration du fond de
|
||||||
<p><b>Historique</b>: Découvert en juillet 1976 par F.Vergier.
|
cette branche: à -456m, un puits d'vingtaine de
|
||||||
Exploré du 12 au 23 juillet 76 par l'A.C.Toulon, S.C.Toulon, Lou
|
mètres était vraiment trop arrosé pour
|
||||||
Darboun, Spéléo Ragaie.
|
être descendu. A -488m, un passage bas était aussi
|
||||||
|
trop humide. De plus le courant d'air y était faible ou nul.
|
||||||
<p><b>Description</b>: jusqu'à -287m, le gouffre est constitué
|
Dans la salle à -308m une remontée d'une quinzaine de
|
||||||
de puits modestes entrecoupés de méandres étroits : p8,
|
mètres permet d'accéder à un méandre
|
||||||
p12, p17, p9, p20, p3, p12, p30, p7, p6, p9, p8, p7, p5, p34, p6, p8, p5, p9.
|
fossile assez large ou souffle un courant d'air sensible. Au bout
|
||||||
A -287m, un p21 permet de déboucher dans une grande salle. L'eau
|
de 30m ce méandre s'ouvre sur l'énorme Puits de
|
||||||
disparait dans les éboulis pour réapparaitre dans toute une
|
Naufragés, d'une section moyenne de 15m sur 25m. Dans ce
|
||||||
série de puits arrosés dont le plus profond mesure 30m. Les
|
puits, plusieurs arrivées d'eau venaient vraisemblablement
|
||||||
crues ont empéché l'exploration du fond de cette branche:
|
de la première branche explorée. La bas de puits se
|
||||||
à -456m, un puits d'vingtaine de mètres était vraiment
|
rétrécit en diaclase, l'exploration s'étant
|
||||||
trop arrosé pour être descendu. A -488m, un passage bas
|
arretée au sommet d'un puits estimé à 40m.</p>
|
||||||
était aussi trop humide. De plus le courant d'air y était
|
<p>Etienne Degrave</p>
|
||||||
faible ou nul. Dans la salle à -308m une remontée d'une
|
<h2 lang="de" xml:lang="de"><a id="id50" name=
|
||||||
quinzaine de mètres permet d'accéder à un méandre
|
"id50">AHNENSCHACHT</a></h2>
|
||||||
fossile assez large ou souffle un courant d'air sensible. Au bout de 30m ce
|
<p>Situation: <span lang="de" xml:lang="de">Totes Gebirge</span>
|
||||||
méandre s'ouvre sur l'énorme Puits de Naufragés, d'une
|
Ouest - <span lang="de" xml:lang="de">Feuertal</span><br />
|
||||||
section moyenne de 15m sur 25m. Dans ce puits, plusieurs arrivées
|
Profondeur: -612m<br />
|
||||||
d'eau venaient vraisemblablement de la première branche
|
Développement: + de 5km.<br />
|
||||||
explorée. La bas de puits se rétrécit en diaclase,
|
Altitude: 1890m</p>
|
||||||
l'exploration s'étant arretée au sommet d'un puits
|
|
||||||
estimé à 40m.
|
|
||||||
|
|
||||||
<p>Etienne Degrave
|
|
||||||
|
|
||||||
<h2 lang="de"><a id="id50">AHNENSCHACHT</a></h2>
|
|
||||||
|
|
||||||
<p>Situation: <span lang="de">Totes Gebirge</span> Ouest - <span
|
|
||||||
lang="de">Feuertal</span><br>
|
|
||||||
|
|
||||||
Profondeur: -612m<br>
|
|
||||||
|
|
||||||
Développement: + de 5km.<br>
|
|
||||||
|
|
||||||
Altitude: 1890m
|
|
||||||
|
|
||||||
<p><b>Historique</b>: Découvert par nos collègues de
|
<p><b>Historique</b>: Découvert par nos collègues de
|
||||||
Haute-Autriche en 1856. La cote -320m est atteinte par ceux-ci en 1958. En
|
Haute-Autriche en 1856. La cote -320m est atteinte par ceux-ci en
|
||||||
1967 et 1968 le Bristol Exploration Club atteind -400m, le réseau
|
1958. En 1967 et 1968 le Bristol Exploration Club atteind -400m, le
|
||||||
horizontal, sur 1km, est découvert. En 1972, 73, 74 et 75, le
|
réseau horizontal, sur 1km, est découvert. En 1972,
|
||||||
<acronym>GSAB</acronym> "Les Gours" explore et découvre plus de 5km de
|
73, 74 et 75, le <acronym>GSAB</acronym> "Les Gours" explore et
|
||||||
galeries et explore environ 1500m de puits. Ce qui lui permet d'atteindre
|
découvre plus de 5km de galeries et explore environ 1500m de
|
||||||
-612m. On note également la participation, en 1974, de trois clubs
|
puits. Ce qui lui permet d'atteindre -612m. On note
|
||||||
Français de l'Est de la France: S.C.Vesoul, G.S.Clerval et S.S.Daules.
|
également la participation, en 1974, de trois clubs
|
||||||
En 1975 le <acronym>CARSS</acronym> a participé à la
|
Français de l'Est de la France: S.C.Vesoul, G.S.Clerval et
|
||||||
mini-expé de juillet ainsi que le <acronym>CASEO</acronym> en
|
S.S.Daules. En 1975 le <acronym>CARSS</acronym> a participé
|
||||||
Août.
|
à la mini-expé de juillet ainsi que le
|
||||||
|
<acronym>CASEO</acronym> en Août.</p>
|
||||||
<h3>Description: Puits d'entrée</h3>
|
<h3>Description: Puits d'entrée</h3>
|
||||||
|
<p>L'entrée s'ouvre dans une petite doline située sur
|
||||||
<p>L'entrée s'ouvre dans une petite doline située sur la
|
la crête limitant le <span lang="de" xml:lang=
|
||||||
crête limitant le <span lang="de">Feuertal</span> du <span
|
"de">Feuertal</span> du <span lang="de" xml:lang=
|
||||||
lang="de">Hintergras</span>. Le gouffre débute par quatre puits (p14,
|
"de">Hintergras</span>. Le gouffre débute par quatre puits
|
||||||
p11, p5 et p11) qui donnent accès sur une pente formée de gros
|
(p14, p11, p5 et p11) qui donnent accès sur une pente
|
||||||
blocs (corde souhaitable). Ensuite une autre série de petits puits (p9, p7, p6, p4, p10, p18, p11) d'où l'on accède à la
|
formée de gros blocs (corde souhaitable). Ensuite une autre
|
||||||
"Terrasse Suintante" à -141m de profondeur.
|
série de petits puits (p9, p7, p6, p4, p10, p18, p11)
|
||||||
|
d'où l'on accède à la "Terrasse Suintante"
|
||||||
<p>A partir de là, on a terminé la zone de petits puits et l'on
|
à -141m de profondeur.</p>
|
||||||
arrive dans une série de puits qui en réalité n'en
|
<p>A partir de là, on a terminé la zone de petits
|
||||||
constitue qu'un seul jusqu'à -400m.
|
puits et l'on arrive dans une série de puits qui en
|
||||||
|
réalité n'en constitue qu'un seul jusqu'à
|
||||||
|
-400m.</p>
|
||||||
<p>En effet, expérience faite avec un kid. tombé
|
<p>En effet, expérience faite avec un kid. tombé
|
||||||
malencontreusement, tout ce qui tombe de la "Terrasse Suintante" arrive
|
malencontreusement, tout ce qui tombe de la "Terrasse Suintante"
|
||||||
à -400. Les puits sont généralement arrosé,
|
arrive à -400. Les puits sont généralement
|
||||||
surtout après un orage... Voici la Liste de ces puits: p25, Puits
|
arrosé, surtout après un orage... Voici la Liste de
|
||||||
Ecailleux 30, p10, Puits Stable 32, Puits Fourchette 48, rampe de 10m, Puits
|
ces puits: p25, Puits Ecailleux 30, p10, Puits Stable 32, Puits
|
||||||
Josef 100m. Pour la Puits Josef, un pendule à 6m de l'entrée
|
Fourchette 48, rampe de 10m, Puits Josef 100m. Pour la Puits Josef,
|
||||||
permet d'atteindre la porte du réseau dit "Horizontal". Si
|
un pendule à 6m de l'entrée permet d'atteindre la
|
||||||
l'on descend le Puits Josef on peut, après deux puits de 6.5 et 10m,
|
porte du réseau dit "Horizontal". Si l'on descend le Puits
|
||||||
explorer un large méandre, actif dans le fond et se terminant sur
|
Josef on peut, après deux puits de 6.5 et 10m, explorer un
|
||||||
fissure. Ce méandre est fossile dans le haut et présente
|
large méandre, actif dans le fond et se terminant sur
|
||||||
certainement des possibilités de continuation.
|
fissure. Ce méandre est fossile dans le haut et
|
||||||
|
présente certainement des possibilités de
|
||||||
|
continuation.</p>
|
||||||
<h4>Réseau Horizontal</h4>
|
<h4>Réseau Horizontal</h4>
|
||||||
|
<p>Après avoir franchis la "Porte" et une courte
|
||||||
<p>Après avoir franchis la "Porte" et une courte étroiture, on
|
étroiture, on pénètre dans le réseau
|
||||||
pénètre dans le réseau proprement dit. Celui-ci
|
proprement dit. Celui-ci débute par une galerie couverte de
|
||||||
débute par une galerie couverte de concrétions assez
|
concrétions assez spéciales. Le premier embranchement
|
||||||
spéciales. Le premier embranchement permet d'accéder au
|
permet d'accéder au réseau... [ <span lang="en"
|
||||||
réseau... [ <span lang="en">line(s) lost at end of photocopy page
|
xml:lang="en">line(s) lost at end of photocopy page here</span>
|
||||||
here</span> ]
|
]</p>
|
||||||
|
|
||||||
<h4>Potager Fleuri</h4>
|
<h4>Potager Fleuri</h4>
|
||||||
|
<p>Ce réseau fossile, qui n'a été que
|
||||||
<p>Ce réseau fossile, qui n'a été que parcouru, contient
|
parcouru, contient encore de nombreuses possibilités. Trois
|
||||||
encore de nombreuses possibilités. Trois accés principaux nous
|
accés principaux nous y conduisent: le puits déja
|
||||||
y conduisent: le puits déja mentionné, un peu avant le
|
mentionné, un peu avant le "Belgica" une fissure descendante
|
||||||
"Belgica" une fissure descendante et une galerie en pente et
|
et une galerie en pente et concrétionnée, dans la
|
||||||
concrétionnée, dans la salle du "Puits Mammouth". Le
|
salle du "Puits Mammouth". Le réseau comporte une vaste
|
||||||
réseau comporte une vaste salle de nombreuses galeries et carrefours;
|
salle de nombreuses galeries et carrefours; il est très
|
||||||
il est très malconnu et pourrait réserver de grosses surprises.
|
malconnu et pourrait réserver de grosses surprises.</p>
|
||||||
|
<p>En continuant la galerie, on passe un seuil de 4m et l'on trouve
|
||||||
<p>En continuant la galerie, on passe un seuil de 4m et l'on trouve un
|
un carrefour sur la gauche qui sert de bivouac.</p>
|
||||||
carrefour sur la gauche qui sert de bivouac.
|
|
||||||
|
|
||||||
<h4>Réseau Belgica</h4>
|
<h4>Réseau Belgica</h4>
|
||||||
|
<p>Après le bivouac, il y a directement un p10 et au bas un
|
||||||
<p>Après le bivouac, il y a directement un p10 et au bas un nouveau
|
nouveau carrefour: à l'aval la galerie "Belgica" d'assez
|
||||||
carrefour: à l'aval la galerie "Belgica" d'assez petite dimension
|
petite dimension permet, après avoir laisser trois puits sur
|
||||||
permet, après avoir laisser trois puits sur le coté, de
|
le coté, de descendre un p8, un p17 et d'arriver sur des
|
||||||
descendre un p8, un p17 et d'arriver sur des étroitures franchies par
|
étroitures franchies par nos collègues
|
||||||
nos collègues Français. A revoir.
|
Français. A revoir.</p>
|
||||||
|
<p>A l'amont, découverte par D.Motte et
|
||||||
<p>A l'amont, découverte par D.Motte et <acronym>PIE</acronym>, au
|
<acronym>PIE</acronym>, au cours de l'expédition de 1974;
|
||||||
cours de l'expédition de 1974; s'ouvre la "Galerie des Francs
|
s'ouvre la "Galerie des Francs comtois". Grosse galerie fossile
|
||||||
comtois". Grosse galerie fossile remontante entrecoupée de
|
remontante entrecoupée de traversées, de ressauts et
|
||||||
traversées, de ressauts et de puits. Elle permet de remonter
|
de puits. Elle permet de remonter jusqu'à -90. A -150 un p20
|
||||||
jusqu'à -90. A -150 un p20 a permis de trouver le
|
a permis de trouver le "Résoméga".</p>
|
||||||
"Résoméga".
|
<p>Un peu avant le p20 un court méandre descendant permet
|
||||||
|
d'eviter le p20 et la série d'étroiture lui
|
||||||
<p>Un peu avant le p20 un court méandre descendant permet d'eviter le
|
succédant. Le "Résoméga" est une galerie
|
||||||
p20 et la série d'étroiture lui succédant. Le
|
alternativement descendante et remontante, très chaotique,
|
||||||
"Résoméga" est une galerie alternativement descendante et
|
entrecoupée de nombreuses carrefours et puits, qui
|
||||||
remontante, très chaotique, entrecoupée de nombreuses
|
mène au "Balcon du Visionnaire", offrant plusieurs
|
||||||
carrefours et puits, qui mène au "Balcon du Visionnaire", offrant
|
possibilités. Un p60 donnant sur un autre p60 non descendu.
|
||||||
plusieurs possibilités. Un p60 donnant sur un autre p60 non descendu.
|
|
||||||
Un autre grand puits de plus de 100m et une galerie remontante non
|
Un autre grand puits de plus de 100m et une galerie remontante non
|
||||||
terminée. Un peu avant le p10 a permis d'explorer une galerie
|
terminée. Un peu avant le p10 a permis d'explorer une
|
||||||
entrecoupée de trois carrefours et de 7 départs !!!! Ceci
|
galerie entrecoupée de trois carrefours et de 7
|
||||||
montre la complexité à laquelle nous nous heurtons.
|
départs !!!! Ceci montre la complexité à
|
||||||
|
laquelle nous nous heurtons.</p>
|
||||||
<p>C'est également au "Balcon du Visionnaire" qu'a eu lieu l'accident
|
<p>C'est également au "Balcon du Visionnaire" qu'a eu lieu
|
||||||
de 1975, qui a arreté l'exploration cette année là.
|
l'accident de 1975, qui a arreté l'exploration cette
|
||||||
|
année là.</p>
|
||||||
<p>En reprenant la galerie horizontale et après avoir passé une
|
<p>En reprenant la galerie horizontale et après avoir
|
||||||
petite montée encombrée de blocs, on rencontre une
|
passé une petite montée encombrée de blocs, on
|
||||||
arrivée d'eau, baptisée "Le Bain". Celle-ci a été
|
rencontre une arrivée d'eau, baptisée "Le Bain".
|
||||||
suivie sur une petite longeur, avec arret sur puits. A terminer.
|
Celle-ci a été suivie sur une petite longeur, avec
|
||||||
|
arret sur puits. A terminer.</p>
|
||||||
<p>L'embranchement suivant a été nommé "Carrefour du
|
<p>L'embranchement suivant a été nommé
|
||||||
Mammouth" car la galerie de droite donne sur le puits du même nom. Il
|
"Carrefour du Mammouth" car la galerie de droite donne sur le puits
|
||||||
faut d'ailleur faire très attention de ne pas glisser car se serait
|
du même nom. Il faut d'ailleur faire très attention de
|
||||||
alors la chute dans celui-ci.
|
ne pas glisser car se serait alors la chute dans celui-ci.</p>
|
||||||
|
<p>Les Puits Mammouth, Parapuits et probablement le Puits Negus,
|
||||||
<p>Les Puits Mammouth, Parapuits et probablement le Puits Negus, font partie
|
font partie d'un même réseau ( voir topo ) qui se
|
||||||
d'un même réseau ( voir topo ) qui se compose d'un p146, d'un
|
compose d'un p146, d'un p10 et d'un méandre étroit
|
||||||
p10 et d'un méandre étroit entrecoupé de nombreuses
|
entrecoupé de nombreuses cascades, finalement un p35 donne
|
||||||
cascades, finalement un p35 donne sur un siphon à -612m. Le
|
sur un siphon à -612m. Le "Parapuits" p106 est suivi de: p5,
|
||||||
"Parapuits" p106 est suivi de: p5, p10, p50 et tombe par celui-ci dans le
|
p10, p50 et tombe par celui-ci dans le "Méandre du
|
||||||
"Méandre du Mammouth".
|
Mammouth".</p>
|
||||||
|
<p>Le "Puits du Négus", non descendu, devrait donner
|
||||||
<p>Le "Puits du Négus", non descendu, devrait donner également
|
également dans le même méandre. Plusieurs
|
||||||
dans le même méandre. Plusieurs autres petits puits et
|
autres petits puits et méandres actifs devraient
|
||||||
méandres actifs devraient également rejoindre ce réseau.
|
également rejoindre ce réseau.</p>
|
||||||
|
<p>La cote -612m est sujette à caution car la méthode
|
||||||
<p>La cote -612m est sujette à caution car la méthode topo
|
topo employée ( hauteur d'homme ) est assez
|
||||||
employée ( hauteur d'homme ) est assez imprécise. La cote
|
imprécise. La cote pourrait se situer entre -580 et -630m.
|
||||||
pourrait se situer entre -580 et -630m. Le manque de temps ne nous a pas
|
Le manque de temps ne nous a pas permis de refaire ces topos.
|
||||||
permis de refaire ces topos. Peut-être cette année ????
|
Peut-être cette année ????</p>
|
||||||
|
<p>En prenant à gauche, la "Galerie Zipfer" se parcourt sur
|
||||||
<p>En prenant à gauche, la "Galerie Zipfer" se parcourt sur 150m avant
|
150m avant de rencontrer un embranchement important: à
|
||||||
de rencontrer un embranchement important: à gauche la "Galerie des
|
gauche la "Galerie des Cheminées", à droite la
|
||||||
Cheminées", à droite la galerie du "Courant d'air".
|
galerie du "Courant d'air".</p>
|
||||||
|
|
||||||
<h4>Galerie des Cheminées</h4>
|
<h4>Galerie des Cheminées</h4>
|
||||||
|
<p>Très vaste et d'une pente régulière, qui
|
||||||
<p>Très vaste et d'une pente régulière, qui est
|
est entrecoupée au milieu par une étroiture et deux
|
||||||
entrecoupée au milieu par une étroiture et deux petit
|
petit résseaux. On évite par une traversée le
|
||||||
résseaux. On évite par une traversée le "Puits Schnaps"
|
"Puits Schnaps" p40 avec méandre étroit non
|
||||||
p40 avec méandre étroit non exploré et on arrive sur un
|
exploré et on arrive sur un p25 dans lequel il faut penduler
|
||||||
p25 dans lequel il faut penduler à 5m du fond pour rejoindre une salle
|
à 5m du fond pour rejoindre une salle dans laquelle nous
|
||||||
dans laquelle nous retrouvons une petite rivière. Un peu en remontant
|
retrouvons une petite rivière. Un peu en remontant en face
|
||||||
en face trouver une courte galerie supérieure rejoignant la
|
trouver une courte galerie supérieure rejoignant la
|
||||||
rivière par un p20. Dans la salle, la descente d'un p10, permet de
|
rivière par un p20. Dans la salle, la descente d'un p10,
|
||||||
suivre la rivière jusqu'à une étroiture derrière
|
permet de suivre la rivière jusqu'à une
|
||||||
laquelle on entend gronder une grosse rivière ? Zone à revoir.
|
étroiture derrière laquelle on entend gronder une
|
||||||
|
grosse rivière ? Zone à revoir.</p>
|
||||||
<h4>Galerie du Courant d'Air</h4>
|
<h4>Galerie du Courant d'Air</h4>
|
||||||
|
|
||||||
<p>Fossile et étroite par endroit, a permis d'explorer un
|
<p>Fossile et étroite par endroit, a permis d'explorer un
|
||||||
réseau très complexe et se recoupant en divers endroit et qui
|
réseau très complexe et se recoupant en divers
|
||||||
pourrait réserver de très grosses surprises, car son
|
endroit et qui pourrait réserver de très grosses
|
||||||
exploration n'en est qu'ébauchée. On débouche par la
|
surprises, car son exploration n'en est qu'ébauchée.
|
||||||
galerie de courant d'air sur une zone d'éboulis ou deux
|
On débouche par la galerie de courant d'air sur une zone
|
||||||
possibilités existent;
|
d'éboulis ou deux possibilités existent;</p>
|
||||||
|
|
||||||
<p><b>à gauche</b>: un passage étroit et une conduite
|
<p><b>à gauche</b>: un passage étroit et une conduite
|
||||||
forcée en pente amène au Puits du Kit, magnifique p50 bien
|
forcée en pente amène au Puits du Kit, magnifique p50
|
||||||
large et plein vide. A sa base plusieurs possibilités. Un
|
bien large et plein vide. A sa base plusieurs possibilités.
|
||||||
méandre étroit et actif que l'on peut court-circuiter par une
|
Un méandre étroit et actif que l'on peut
|
||||||
galerie fossile, coupé par un ressaut terreux de 3m puis un vaste p15
|
court-circuiter par une galerie fossile, coupé par un
|
||||||
mène au siphon à -360m.
|
ressaut terreux de 3m puis un vaste p15 mène au siphon
|
||||||
|
à -360m.</p>
|
||||||
<p>Un ressaut de quelques mètres permet l'accès à une
|
<p>Un ressaut de quelques mètres permet l'accès
|
||||||
vaste galerie fossile ( 10 x 5 ). Le sol de celle-ci est sillonné d'un
|
à une vaste galerie fossile ( 10 x 5 ). Le sol de celle-ci
|
||||||
profond méandre qui n'a pas été exploré. Au bout
|
est sillonné d'un profond méandre qui n'a pas
|
||||||
d'une centaine de mètre la galerie s'achève sur un vaste puits
|
été exploré. Au bout d'une centaine de
|
||||||
arrosé. L'escalade d'un gros éboulis sur la droite permet
|
mètre la galerie s'achève sur un vaste puits
|
||||||
d'acceder à un autre puits remontant.
|
arrosé. L'escalade d'un gros éboulis sur la droite
|
||||||
|
permet d'acceder à un autre puits remontant.</p>
|
||||||
<p>Peu après la base du "Puits du kit" une galerie de 80m permet
|
<p>Peu après la base du "Puits du kit" une galerie de 80m
|
||||||
defaire la jonction avec la réseau du "Puits du décollement"
|
permet defaire la jonction avec la réseau du "Puits du
|
||||||
à la base du p40. Un méandre partant de la galerie de la
|
décollement" à la base du p40. Un méandre
|
||||||
jonction peut-être parcouru sur plus de 300m et débouche, en
|
partant de la galerie de la jonction peut-être parcouru sur
|
||||||
plusieurs endroits, dans le flanc de la grande galerie fossile, peu avant les
|
plus de 300m et débouche, en plusieurs endroits, dans le
|
||||||
puits remontants.
|
flanc de la grande galerie fossile, peu avant les puits
|
||||||
|
remontants.</p>
|
||||||
<p><b>à droite</b>: Le puits du "Décollement" avec à sa
|
<p><b>à droite</b>: Le puits du "Décollement" avec
|
||||||
base une salle en pente encombrée d'éboulis. A gauche un
|
à sa base une salle en pente encombrée
|
||||||
méandre remontant très profond non exploré. Dans le fond
|
d'éboulis. A gauche un méandre remontant très
|
||||||
s'ouvre le "Méandre Emeri" ainsi appelé parce que les
|
profond non exploré. Dans le fond s'ouvre le "Méandre
|
||||||
concrétions sont orientées dans le sens de la marche et du
|
Emeri" ainsi appelé parce que les concrétions sont
|
||||||
vent. Celui-ci rejoint un large puits avec une arrivée d'eau.
|
orientées dans le sens de la marche et du vent. Celui-ci
|
||||||
Après ce p15, un court méandre et un p40
|
rejoint un large puits avec une arrivée d'eau. Après
|
||||||
légèrement arrosé. A sa base, la vaste galerie
|
ce p15, un court méandre et un p40 légèrement
|
||||||
descendante devient soudain presque verticale. C'est le "Tobogan" necessitant
|
arrosé. A sa base, la vaste galerie descendante devient
|
||||||
20m de corde (Passage très spectaculaire). On recoupe à ce
|
soudain presque verticale. C'est le "Tobogan" necessitant 20m de
|
||||||
|
corde (Passage très spectaculaire). On recoupe à ce
|
||||||
niveau un nouveau ruisseau. La galerie se poursuit, puis se
|
niveau un nouveau ruisseau. La galerie se poursuit, puis se
|
||||||
rétrésit et queute à -385m
|
rétrésit et queute à -385m</p>
|
||||||
|
<p><b>Conclusion</b>: énormément à voir et
|
||||||
<p><b>Conclusion</b>: énormément à voir et à
|
à revoir completement. Plus nous avançons et plus
|
||||||
revoir completement. Plus nous avançons et plus nous trouvons ! Un
|
nous trouvons ! Un apport de spéléo nous permettrait
|
||||||
apport de spéléo nous permettrait de faire du travail
|
de faire du travail extraordinaire.</p>
|
||||||
extraordinaire.
|
<p style="text-align: right">J.C.Hans</p>
|
||||||
|
<h2><a id="id122" name="id122">GOUFFRE OVNI</a> = <span lang="de"
|
||||||
<p align=right>J.C.Hans
|
xml:lang="de">UFO SCHACHT</span></h2>
|
||||||
|
<p>Situation: <span lang="de" xml:lang="de">Totes Gebirge</span>
|
||||||
<h2><a id="id122">GOUFFRE OVNI</a> = <span lang="de">UFO SCHACHT</span></h2>
|
Ouest - <span lang="de" xml:lang="de">Hintergras</span><br />
|
||||||
|
Profondeur: -201m<br />
|
||||||
<p>Situation: <span lang="de">Totes Gebirge</span> Ouest - <span
|
Altitude: environ 1500m</p>
|
||||||
lang="de">Hintergras</span><br>
|
<p><b>Historique</b>: Découvert en Août 1974 par
|
||||||
|
D.Motte. Entrée désobstruée par le
|
||||||
Profondeur: -201m<br>
|
<acronym>GSAB</acronym> en 1975 et 76. Exploré au mois
|
||||||
|
d'Août 76 par F.Dechany et J.C.Hans.</p>
|
||||||
Altitude: environ 1500m
|
<p><b>Description</b>: L'entrée se constituait d'une fente
|
||||||
|
d'environ 20cm de hauteur, qui a d'abord été
|
||||||
<p><b>Historique</b>: Découvert en Août 1974 par D.Motte.
|
dégagée jusqu'à une salle close de toute part.
|
||||||
Entrée désobstruée par le <acronym>GSAB</acronym> en
|
Le courant d'air qui avait permis de trouver l'entrée, nous
|
||||||
1975 et 76. Exploré au mois d'Août 76 par F.Dechany et J.C.Hans.
|
indiquait le chemin à suivre. Après avoir
|
||||||
|
débouché une fissure, appelée "Sas" nous
|
||||||
<p><b>Description</b>: L'entrée se constituait d'une fente d'environ
|
arrivons sur un puits. Celui-ci est fractionné en 5
|
||||||
20cm de hauteur, qui a d'abord été dégagée
|
endroits. Un deuxième puits fractionné en trois
|
||||||
jusqu'à une salle close de toute part. Le courant d'air qui avait
|
mène à un court méandre puis à
|
||||||
permis de trouver l'entrée, nous indiquait le chemin à suivre.
|
plusieurs ressauts et puits entrecoupé de courtes
|
||||||
Après avoir débouché une fissure, appelée "Sas"
|
étroitures. On peut considérer les puits suivants
|
||||||
nous arrivons sur un puits. Celui-ci est fractionné en 5 endroits. Un
|
comme formant un seul de 80m, divisé en cinq et devient de
|
||||||
deuxième puits fractionné en trois mène à un
|
plus en plus grand aussi bien en profondeur qu'en largeur. Le
|
||||||
court méandre puis à plusieurs ressauts et puits
|
gouffre continue par une faille de deux à trois
|
||||||
entrecoupé de courtes étroitures. On peut considérer
|
mètres de large et s'enfonçant par crans successifs.
|
||||||
les puits suivants comme formant un seul de 80m, divisé en cinq et
|
L'exploration continuera en Août 1977</p>
|
||||||
devient de plus en plus grand aussi bien en profondeur qu'en largeur. Le
|
<p style="text-align: right">J.C.Hans</p>
|
||||||
gouffre continue par une faille de deux à trois mètres de large
|
|
||||||
et s'enfonçant par crans successifs. L'exploration continuera en
|
|
||||||
Août 1977
|
|
||||||
|
|
||||||
<p align=right>J.C.Hans
|
|
||||||
|
|
||||||
<hr />
|
<hr />
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<p lang="en">
|
<p lang="en" xml:lang="en"> </p>
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="../index.htm" lang="en"><acronym>GSAB</acronym> articles list</a></li>
|
<li><a href="../index.htm" lang="en" xml:lang=
|
||||||
|
"en"><acronym>GSAB</acronym> articles list</a></li>
|
||||||
<li><b>Cave descriptions</b> (in English translation):
|
<li><b>Cave descriptions</b> (in English translation):
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="../../../noinfo/1626/50.htm" lang="en"><span lang="de">Ahnenschacht</span></a></li>
|
<li><a href="../../../noinfo/1626/50.htm" lang="en" xml:lang=
|
||||||
<li><a href="../../../noinfo/1626/117.htm" lang="en"><span lang="de">Trunkemboldschacht</span></a></li>
|
"en"><span lang="de" xml:lang="de">Ahnenschacht</span></a></li>
|
||||||
<li><a href="../../../noinfo/1626/120.htm" lang="en"><span lang="de">Feuertalsystem</span></a></li>
|
<li><a href="../../../noinfo/1626/117.htm" lang="en" xml:lang=
|
||||||
<li><a href="../../../noinfo/1626/122.htm" lang="en"><span lang="fr">Gouffre Ovni</span></a></li>
|
"en"><span lang="de" xml:lang=
|
||||||
</ul></li>
|
"de">Trunkemboldschacht</span></a></li>
|
||||||
<li><a href="../../../1626/index.htm" lang="en">Overview</a>
|
<li><a href="../../../noinfo/1626/120.htm" lang="en" xml:lang=
|
||||||
of area 1626, and index to caves</li>
|
"en"><span lang="de" xml:lang="de">Feuertalsystem</span></a></li>
|
||||||
<li>Back to <a href="../../../index.htm" lang="en">Expedition Intro page</a></li>
|
<li><a href="../../../noinfo/1626/122.htm" lang="en" xml:lang=
|
||||||
<li><a href="../../../../index.htm" lang="en">Back to <acronym>CUCC</acronym> Home page</a></li>
|
"en"><span lang="fr" xml:lang="fr">Gouffre Ovni</span></a></li>
|
||||||
|
</ul>
|
||||||
|
</li>
|
||||||
|
<li><a href="../../../1626/index.htm" lang="en" xml:lang=
|
||||||
|
"en">Overview</a> of area 1626, and index to caves</li>
|
||||||
|
<li>Back to <a href="../../../index.htm" lang="en" xml:lang=
|
||||||
|
"en">Expedition Intro page</a></li>
|
||||||
|
<li><a href="../../../../index.htm" lang="en" xml:lang="en">Back to
|
||||||
|
<acronym>CUCC</acronym> Home page</a></li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
</html>
|
</html>
|
||||||
|
|||||||
@@ -1,109 +1,117 @@
|
|||||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
|
||||||
<html lang="fr">
|
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
||||||
|
<html lang="fr" xmlns="http://www.w3.org/1999/xhtml" xml:lang="fr">
|
||||||
<head>
|
<head>
|
||||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
<meta http-equiv="Content-Type" content=
|
||||||
|
"text/html; charset=iso-8859-1" />
|
||||||
<title>GSAB: CTS ref. 79.1855</title>
|
<title>GSAB: CTS ref. 79.1855</title>
|
||||||
<link rel="stylesheet" type="text/css" href="../../../css/main2.css" />
|
<link rel="stylesheet" type="text/css" href=
|
||||||
|
"../../../css/main2.css" />
|
||||||
</head>
|
</head>
|
||||||
<body>
|
<body>
|
||||||
<center><font size=-1>(<acronym>GSAB</acronym>)
|
<p style="text-align: center; font-size: 65%">
|
||||||
Spéalp 3 (Oct. 1978) pp 44-45</font>
|
(<acronym>GSAB</acronym>) Spéalp 3
|
||||||
<h1><span lang="de">AHNENSCHACHT</span> 77-78</h1></center>
|
(Oct. 1978) pp 44-45</p>
|
||||||
|
<h1><span lang="de" xml:lang="de">AHNENSCHACHT</span> 77-78</h1>
|
||||||
<p><b>Situation</b> : Totes Gebirge West - Feuertal<br>
|
|
||||||
|
|
||||||
<b>Profondeur</b> : -607m<br>
|
|
||||||
|
|
||||||
<b>Altitude</b> : 1890m; Frigoschacht 1875m<br>
|
|
||||||
|
|
||||||
<b>Historique</b> : voir <a href="782012.htm">Sp<EFBFBD>alp no. 1</a>
|
|
||||||
|
|
||||||
<p>Exp<EFBFBD>dition GSAB organis<69>e en 1977 du 5 au 29 Ao<41>t.
|
|
||||||
|
|
||||||
<p>Elle a regroup<75> plusieurs individuels venant de diff<66>rents clubs, et
|
|
||||||
parall<EFBFBD>lement <20> l'exploration du Gouffre Ovni (-565m), l'exp<78>dition du GSAB a
|
|
||||||
pu approfondir le Gouffre Ahnenschacht et r<>soudres quelques inconnues.
|
|
||||||
|
|
||||||
|
<p><b>Situation</b> : Totes Gebirge West - Feuertal<br />
|
||||||
|
<b>Profondeur</b> : -607m<br />
|
||||||
|
<b>Altitude</b> : 1890m; Frigoschacht 1875m<br />
|
||||||
|
<b>Historique</b> : voir <a href="782012.htm">Spéalp no.
|
||||||
|
1</a></p>
|
||||||
|
<p>Expédition GSAB organisée en 1977 du 5 au 29
|
||||||
|
Août.</p>
|
||||||
|
<p>Elle a regroupé plusieurs individuels venant de
|
||||||
|
différents clubs, et parallèlement à
|
||||||
|
l'exploration du Gouffre Ovni (-565m), l'expédition du GSAB
|
||||||
|
a pu approfondir le Gouffre Ahnenschacht et résoudres
|
||||||
|
quelques inconnues.</p>
|
||||||
<ul>
|
<ul>
|
||||||
<li>Jonction Frigoschacht (alt 1875m) <EFBFBD> -130m par
|
<li>Jonction Frigoschacht (alt 1875m) à -130m par P17, P5,
|
||||||
P17, P5, P9, P9, P5 et P18, P11 de l'Ahnenschacht.
|
P9, P9, P5 et P18, P11 de l'Ahnenschacht.</li>
|
||||||
<li>Topgraphie du r<EFBFBD>seau potager fleuri.
|
<li>Topgraphie du réseau potager fleuri.</li>
|
||||||
<li>Exploration du r<EFBFBD>seau Yodl (-607m).
|
<li>Exploration du réseau Yodl (-607m).</li>
|
||||||
<li>Exploration dans le r<EFBFBD>seau KGB.
|
<li>Exploration dans le réseau KGB.</li>
|
||||||
</ul>
|
</ul>
|
||||||
|
<h3>Réseau Yodl</h3>
|
||||||
<h3>R<EFBFBD>seau Yodl</h3>
|
<p>De la porte, après les 70m du puits Josef, on descend un
|
||||||
|
ressaut de 7m escalade sur un gros bloc et descente du 12m environ
|
||||||
<p>De la porte, apr<70>s les 70m du puits Josef, on descend un ressaut de 7m
|
dans le bas d'un méandre. Le progression se fait dans ce
|
||||||
escalade sur un gros bloc et descente du 12m environ dans le bas d'un
|
méandre, ensuite courte escalade dans une faille sur la
|
||||||
m<EFBFBD>andre. Le progression se fait dans ce m<EFBFBD>andre, ensuite courte escalade dans
|
gauche et un puits de 120m, par tronçons de 22m et 100m.
|
||||||
une faille sur la gauche et un puits de 120m, par tron<6F>ons de 22m et 100m.
|
Ensuite, un méandre étroit, P20 jusqu'à un
|
||||||
Ensuite, un m<>andre <20>troit, P20 jusqu'<27> un siphon <20> -607m (la derni<6E>re partie
|
siphon à -607m (la dernière partie du P100 est
|
||||||
du P100 est arros<6F>).
|
arrosé).</p>
|
||||||
|
|
||||||
<h4>Participants :</h4>
|
<h4>Participants :</h4>
|
||||||
|
|
||||||
<dl>
|
<dl>
|
||||||
<dt><acronym>GSAB</acronym> :<dd>F Dechany, E Degrave, D Ferrière, J C Hans
|
<dt><acronym>GSAB</acronym> :</dt>
|
||||||
<dt><acronym>GSAB-CASEO</acronym> :<dd>G Feller, J Kirsch
|
<dd>F Dechany, E Degrave, D Ferrière, J C Hans</dd>
|
||||||
<dt><acronym>SSSPA</acronym> :<dd>Pierre Dethier
|
<dt><acronym>GSAB-CASEO</acronym> :</dt>
|
||||||
<dt><acronym>GSREDAN</acronym> :<dd>J P Braun
|
<dd>G Feller, J Kirsch</dd>
|
||||||
<dt><acronym>ES GEODE</acronym> :<dd>F Saussus
|
<dt><acronym>SSSPA</acronym> :</dt>
|
||||||
<dt><acronym>SC</acronym> Calcaires :<dd>J M Piron
|
<dd>Pierre Dethier</dd>
|
||||||
<dt><span lang="en">no club affiliations</span> :<dd>T Disneur, H Weber
|
<dt><acronym>GSREDAN</acronym> :</dt>
|
||||||
|
<dd>J P Braun</dd>
|
||||||
|
<dt><acronym>ES GEODE</acronym> :</dt>
|
||||||
|
<dd>F Saussus</dd>
|
||||||
|
<dt><acronym>SC</acronym> Calcaires :</dt>
|
||||||
|
<dd>J M Piron</dd>
|
||||||
|
<dt><span lang="en" xml:lang="en">no club affiliations</span>
|
||||||
|
:</dt>
|
||||||
|
<dd>T Disneur, H Weber</dd>
|
||||||
</dl>
|
</dl>
|
||||||
|
<h3>Mini Expedition du 25 Juin au 5 Juillet (Inter
|
||||||
<h3>Mini Expedition du 25 Juin au 5 Juillet (Inter individuels)</h3>
|
individuels)</h3>
|
||||||
|
<p>La possibilité d'une jonction avec l'Empagédure
|
||||||
<p>La possibilit<69> d'une jonction avec l'Empag<61>dure avait am<61>ne les sp<73>l<EFBFBD>os
|
avait amène les spéléos Belges à
|
||||||
Belges <20> organiser une mini-exp<EFBFBD> inter-individuels.
|
organiser une mini-expé inter-individuels.</p>
|
||||||
|
<p>La jonction ne fut pas réalisée, une couche de
|
||||||
<p>La jonction ne fut pas r<>alis<69>e, une couche de Dolomie semble <EFBFBD>liminer tout
|
Dolomie semble éliminer tout espoir. Cette expé a
|
||||||
espoir. Cette exp<78> a permis <20> quelques sp<73>l<EFBFBD>os Belges de d<>couvrir une cavit<69>
|
permis à quelques spéléos Belges de
|
||||||
Autrichienne.
|
découvrir une cavité Autrichienne.</p>
|
||||||
|
<p>Le Bilan : -500m de première, plusieurs réseaux
|
||||||
<p>Le Bilan : -500m de premi<6D>re, plusieurs r<>seaux termin<69>s et de nouvelles
|
terminés et de nouvelles hypothèses de suite de
|
||||||
hypoth<EFBFBD>ses de suite de gouffre.
|
gouffre.</p>
|
||||||
|
<p>-150m dans le réseau amont du Josef : arrêt sur
|
||||||
<p>-150m dans le r<>seau amont du Josef : arr<72>t sur tremis et fissure (m<>andre
|
tremis et fissure (méandre étroit et haut).</p>
|
||||||
<EFBFBD>troit et haut).
|
<p>Différente réseaux revus: Enigmatique, KGB,
|
||||||
|
Gruyère et Schnaps.</p>
|
||||||
<p>Diff<EFBFBD>rente r<>seaux revus: Enigmatique, KGB, Gruy<75>re et Schnaps.
|
<p>Visite et exploration du réseau Belgica.</p>
|
||||||
|
<p>Après le Bivouac : un P10, on prend à gauche une
|
||||||
<p>Visite et exploration du r<>seau Belgica.
|
galerie de petite dimension, on laisse 3 puits sur le coté
|
||||||
|
et on descend un P8, P13 arrivée sur des étroitures
|
||||||
<p>Apr<EFBFBD>s le Bivouac : un P10, on prend <20> gauche une galerie de petite dimension,
|
faciles à gauche. Ensuite R5 et P42. Arrêt sur boyau
|
||||||
on laisse 3 puits sur le cot<6F> et on descend un P8, P13 arriv<69>e sur des
|
de sable à -410m.</p>
|
||||||
<EFBFBD>troitures faciles <20> gauche. Ensuite R5 et P42. Arr<72>t sur boyau de sable <20>
|
<p>Par dessus le P13 : une petite galerie permet par quelques
|
||||||
-410m.
|
ressauts dans un réseau fossile: P25 et deux puits de 10m;
|
||||||
|
très étroit et plusieurs cheminées.</p>
|
||||||
<p>Par dessus le P13 : une petite galerie permet par quelques ressauts dans un
|
|
||||||
r<EFBFBD>seau fossile: P25 et deux puits de 10m; tr<74>s <20>troit et plusieurs chemin<69>es.
|
|
||||||
|
|
||||||
<h4>Participants :</h4>
|
<h4>Participants :</h4>
|
||||||
|
|
||||||
<dl>
|
<dl>
|
||||||
<dt><acronym>GSAB</acronym>:<dd>J P Braun, F Dechany, E Degrave
|
<dt><acronym>GSAB</acronym>:</dt>
|
||||||
(organisateur), J C Hans
|
<dd>J P Braun, F Dechany, E Degrave (organisateur), J C Hans</dd>
|
||||||
<dt><acronym>GIPS</acronym>:<dd>F Spinoy
|
<dt><acronym>GIPS</acronym>:</dt>
|
||||||
<dt><acronym>SCUCL</acronym>:<dd>Y Dubois
|
<dd>F Spinoy</dd>
|
||||||
|
<dt><acronym>SCUCL</acronym>:</dt>
|
||||||
|
<dd>Y Dubois</dd>
|
||||||
</dl>
|
</dl>
|
||||||
|
<p>Notons la visite de six membres du CARSS, qui avaient
|
||||||
<p>Notons la visite de six membres du CARSS, qui avaient oubli<6C>s leur trousse <20>
|
oubliés leur trousse à spits dans la
|
||||||
spits dans la vall<6C>e.
|
vallée.</p>
|
||||||
|
<p>Jean Pierre Braun</p>
|
||||||
<p>Jean Pierre Braun
|
|
||||||
|
|
||||||
<hr />
|
<hr />
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<p lang="en"><ul>
|
<p lang="en" xml:lang="en"> </p>
|
||||||
<li><a href="../index.htm"><acronym>GSAB</acronym> articles list</a></li>
|
<ul>
|
||||||
<li><b lang="de">Ahnenschacht</b> :
|
<li><a href="../index.htm"><acronym>GSAB</acronym> articles
|
||||||
<a href="../../../noinfo/1626/50.htm">description</a>, in English</li>
|
list</a></li>
|
||||||
<li><a href="../../../1626/index.htm">Overview</a>
|
<li><b lang="de" xml:lang="de">Ahnenschacht</b> : <a href=
|
||||||
of area 1626, and index to caves</li>
|
"../../../noinfo/1626/50.htm">description</a>, in English</li>
|
||||||
<li>Back to <a href="../../../index.htm">Expedition Intro page</a></li>
|
<li><a href="../../../1626/index.htm">Overview</a> of area 1626,
|
||||||
<li><a href="../../../../index.htm">Back to <acronym>CUCC</acronym> Home page</a></li>
|
and index to caves</li>
|
||||||
|
<li>Back to <a href="../../../index.htm">Expedition Intro
|
||||||
|
page</a></li>
|
||||||
|
<li><a href="../../../../index.htm">Back to <acronym>CUCC</acronym>
|
||||||
|
Home page</a></li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
</html>
|
</html>
|
||||||
|
|||||||
@@ -1,102 +1,119 @@
|
|||||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
|
||||||
<html>
|
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
||||||
<head><meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
<html xmlns="http://www.w3.org/1999/xhtml">
|
||||||
<title>GSAB</title><link rel="stylesheet" type="text/css" href="../../css/main2.css" />
|
<head>
|
||||||
|
<meta http-equiv="Content-Type" content=
|
||||||
|
"text/html; charset=iso-8859-1" />
|
||||||
|
<title>GSAB</title>
|
||||||
|
<link rel="stylesheet" type="text/css" href=
|
||||||
|
"../../css/main2.css" />
|
||||||
</head>
|
</head>
|
||||||
<body>
|
<body>
|
||||||
<h1 lang="fr">Groupe Spéléo Alpin Belge</h1>
|
|
||||||
|
|
||||||
<p>The <acronym lang="fr">GSAB</acronym> was (I believe, and if anyone knows
|
<h1 lang="fr" xml:lang="fr">Groupe Spéléo Alpin Belge</h1>
|
||||||
different then I'd love to hear from them) an umbrella organisation for club
|
|
||||||
cavers in Belgium visiting deep and serious caving areas in the 1970's. It
|
|
||||||
would appear to have evolved from a group <span lang="fr">"Les Gours"</span>,
|
|
||||||
part of the <span lang="fr">Club d'Archaeologie, de Spéléologie
|
|
||||||
et d'Escalade de Huy-Andenne (<acronym>CASE-HA</acronym>)</span>, though this
|
|
||||||
is conjecture based on the fact that the journal of
|
|
||||||
<span lang="fr">Les Gours</span> had the same name,
|
|
||||||
"<span lang="fr">Spéalp</span>", as the later journal of
|
|
||||||
<acronym lang="fr">GSAB</acronym>, and from an odd reference to
|
|
||||||
'<span lang="fr"><acronym>GSAB</acronym> "Les Gours"</span>' in a later
|
|
||||||
journal.
|
|
||||||
|
|
||||||
<p>Members of these groups, and associated club cavers, visited the north of
|
<p>The <acronym lang="fr" xml:lang="fr">GSAB</acronym> was (I
|
||||||
the western massif of the <span lang="de">Totes Gebirge</span> every summer
|
believe, and if anyone knows different then I'd love to hear from
|
||||||
(sometimes apparently on more than one trip) from 1972 to 1978. At least one
|
them) an umbrella organisation for club cavers in Belgium visiting
|
||||||
of these trips was an international expedition, and others seem also to have
|
deep and serious caving areas in the 1970's. It would appear to
|
||||||
worked with various French groups. Much of the work was apparently reported
|
have evolved from a group <span lang="fr" xml:lang="fr">"Les
|
||||||
in various club journals, but there are also a series of good reports in both
|
Gours"</span>, part of the <span lang="fr" xml:lang="fr">Club
|
||||||
of the journals <span lang="fr">Spéalp</span>. These are now quite
|
d'Archaeologie, de Spéléologie et d'Escalade de
|
||||||
hard to obtain (since the group no longer exists), but we found that the
|
Huy-Andenne (<acronym>CASE-HA</acronym>)</span>, though this is
|
||||||
librarian of the <span lang="fr">Féderation Belgique de
|
conjecture based on the fact that the journal of <span lang="fr"
|
||||||
Spéléologie</span> was one of the world's most helpful people,
|
xml:lang="fr">Les Gours</span> had the same name, "<span lang="fr"
|
||||||
and he photocopied the relevant articles from the later <acronym
|
xml:lang="fr">Spéalp</span>", as the later journal of
|
||||||
lang="fr">GSAB</acronym> publications for us for free, for which go many
|
<acronym lang="fr" xml:lang="fr">GSAB</acronym>, and from an odd
|
||||||
thanks.
|
reference to '<span lang="fr" xml:lang="fr"><acronym>GSAB</acronym>
|
||||||
|
"Les Gours"</span>' in a later journal.</p>
|
||||||
|
|
||||||
<p>Included in these pages are English translations (by Andy Waddington and
|
<p>Members of these groups, and associated club cavers, visited the
|
||||||
Jill Gates) of articles from <span lang="fr"><acronym>GSAB</acronym>
|
north of the western massif of the <span lang="de" xml:lang=
|
||||||
Spéalp</span> 1, 2 and 3. If you can read French, I reccommend getting
|
"de">Totes Gebirge</span> every summer (sometimes apparently on
|
||||||
hold of copies of the original journals, as the diagrams are quite helpful to
|
more than one trip) from 1972 to 1978. At least one of these trips
|
||||||
understanding some of the explanations !
|
was an international expedition, and others seem also to have
|
||||||
|
worked with various French groups. Much of the work was apparently
|
||||||
|
reported in various club journals, but there are also a series of
|
||||||
|
good reports in both of the journals <span lang="fr" xml:lang=
|
||||||
|
"fr">Spéalp</span>. These are now quite hard to obtain
|
||||||
|
(since the group no longer exists), but we found that the librarian
|
||||||
|
of the <span lang="fr" xml:lang="fr">Féderation Belgique de
|
||||||
|
Spéléologie</span> was one of the world's most
|
||||||
|
helpful people, and he photocopied the relevant articles from the
|
||||||
|
later <acronym lang="fr" xml:lang="fr">GSAB</acronym> publications
|
||||||
|
for us for free, for which go many thanks.</p>
|
||||||
|
|
||||||
<dl lang="fr">
|
<p>Included in these pages are English translations (by Andy
|
||||||
<dt>73.2295<dd>
|
Waddington and Jill Gates) of articles from <span lang="fr"
|
||||||
<cite>(<acronym>CASE HA</acronym>) Spéalp 2 (1972) pp 3-21, <span
|
xml:lang="fr"><acronym>GSAB</acronym> Spéalp</span> 1, 2 and
|
||||||
lang="en">surveys</span></cite>, <b>Expédition
|
3. If you can read French, I reccommend getting hold of copies of
|
||||||
Spéléologique à Autriche (Gouffre des Aieux)</b>, Jean
|
the original journals, as the diagrams are quite helpful to
|
||||||
Claude Hans et Pierre Gobbels
|
understanding some of the explanations!</p>
|
||||||
|
|
||||||
<dt>74.1210<dd>
|
|
||||||
<cite>(<acronym>CASE HA</acronym>) Spéalp 4 (1973) pp 1-25, <span
|
|
||||||
lang="en">surveys</span></cite>, <b>Expédition 1973 à l'<span
|
|
||||||
lang="de">Ahnenschacht</span> (-612m)</b>, Etienne Degrave et al
|
|
||||||
|
|
||||||
<dt>78.2012<dd>
|
|
||||||
<cite>(<acronym>GSAB</acronym>) Spéalp 1 (Juin 1977) pp 33-49</cite>,
|
|
||||||
<b><span lang="de">Totes Gebirge</span> : Description des principaux gouffres
|
|
||||||
de la zone ouest du massif</b>, Jean Claude Hans & Etienne Degrave<br>
|
|
||||||
<a href="fr/782012.htm" lang="fr">en Français</a> /
|
|
||||||
<a href="en/782012.htm" lang="en"><span lang="en">English Translation</span></a>
|
|
||||||
|
|
||||||
<dt>78.2008<dd>
|
|
||||||
<cite>(<acronym>GSAB</acronym>) Spéalp 2 (1978) pp 14-19, <span
|
|
||||||
lang="en">figures, surveys</span></cite>, <b>Gouffre Ovni</b>, Georges
|
|
||||||
Feller<br>
|
|
||||||
<a href="fr/782008.htm" lang="fr">en Français</a> /
|
|
||||||
<a href="en/782008.htm" lang="en"><span lang="en">English Translation</span></a>
|
|
||||||
|
|
||||||
<dt>78.2003<dd>
|
|
||||||
<cite>(<acronym>GSAB</acronym>) Spéalp 2 (1978) p64, <span
|
|
||||||
lang="en">survey</span></cite>, <b lang="de">Trunkemboldschacht</b>, Jean Pierre
|
|
||||||
Braun<br>
|
|
||||||
<a href="782003.htm" lang="fr">en Français</a> / (the English
|
|
||||||
translation is essentially identical to the kataster
|
|
||||||
<a href="../../noinfo/1626/117.htm">cave description</a>)
|
|
||||||
|
|
||||||
<dt>78.2013<dd>
|
|
||||||
<cite>(<acronym>GSAB</acronym>) Spéalp 2 (1978) pp 66-67, <span
|
|
||||||
lang="en">survey</span></cite>, <b lang="de">Feuertalsystem</b>, Jean Claude
|
|
||||||
Hans<br><a href="782013.htm" lang="fr">en Français</a> / (the English
|
|
||||||
translation is essentially identical to the kataster
|
|
||||||
<a href="../../noinfo/1626/120.htm">cave description</a>)
|
|
||||||
|
|
||||||
<dt>79.1855<dd>
|
|
||||||
<cite>(<acronym>GSAB</acronym>) Spéalp 3 (Oct. 1978) pp 44-45, <span
|
|
||||||
lang="en">survey</span></cite>, <b><span lang="de">Ahnenschacht</span> 77/78</b>,
|
|
||||||
Jean Pierre Braun<br>
|
|
||||||
<a href="fr/791855.htm" lang="fr">en Français</a> /
|
|
||||||
<a href="en/791855.htm" lang="en"><span lang="en">English Translation</span></a>
|
|
||||||
|
|
||||||
|
<dl lang="fr" xml:lang="fr">
|
||||||
|
<dt>73.2295</dt>
|
||||||
|
<dd><cite>(<acronym>CASE HA</acronym>) Spéalp 2 (1972) pp
|
||||||
|
3-21, <span lang="en" xml:lang="en">surveys</span></cite>,
|
||||||
|
<b>Expédition Spéléologique à Autriche
|
||||||
|
(Gouffre des Aieux)</b>, Jean Claude Hans et Pierre Gobbels</dd>
|
||||||
|
<dt>74.1210</dt>
|
||||||
|
<dd><cite>(<acronym>CASE HA</acronym>) Spéalp 4 (1973) pp
|
||||||
|
1-25, <span lang="en" xml:lang="en">surveys</span></cite>,
|
||||||
|
<b>Expédition 1973 à l'<span lang="de" xml:lang=
|
||||||
|
"de">Ahnenschacht</span> (-612m)</b>, Etienne Degrave et al</dd>
|
||||||
|
<dt>78.2012</dt>
|
||||||
|
<dd><cite>(<acronym>GSAB</acronym>) Spéalp 1 (Juin 1977) pp
|
||||||
|
33-49</cite>, <b><span lang="de" xml:lang="de">Totes Gebirge</span>
|
||||||
|
: Description des principaux gouffres de la zone ouest du
|
||||||
|
massif</b>, Jean Claude Hans & Etienne Degrave<br />
|
||||||
|
<a href="fr/782012.htm" lang="fr" xml:lang="fr">en
|
||||||
|
Français</a> / <a href="en/782012.htm" lang="en" xml:lang=
|
||||||
|
"en"><span lang="en" xml:lang="en">English
|
||||||
|
Translation</span></a></dd>
|
||||||
|
<dt>78.2008</dt>
|
||||||
|
<dd><cite>(<acronym>GSAB</acronym>) Spéalp 2 (1978) pp
|
||||||
|
14-19, <span lang="en" xml:lang="en">figures,
|
||||||
|
surveys</span></cite>, <b>Gouffre Ovni</b>, Georges Feller<br />
|
||||||
|
<a href="fr/782008.htm" lang="fr" xml:lang="fr">en
|
||||||
|
Français</a> / <a href="en/782008.htm" lang="en" xml:lang=
|
||||||
|
"en"><span lang="en" xml:lang="en">English
|
||||||
|
Translation</span></a></dd>
|
||||||
|
<dt>78.2003</dt>
|
||||||
|
<dd><cite>(<acronym>GSAB</acronym>) Spéalp 2 (1978) p64,
|
||||||
|
<span lang="en" xml:lang="en">survey</span></cite>, <b lang="de"
|
||||||
|
xml:lang="de">Trunkemboldschacht</b>, Jean Pierre Braun<br />
|
||||||
|
<a href="782003.htm" lang="fr" xml:lang="fr">en Français</a>
|
||||||
|
/ (the English translation is essentially identical to the kataster
|
||||||
|
<a href="../../noinfo/1626/117.htm">cave description</a>)</dd>
|
||||||
|
<dt>78.2013</dt>
|
||||||
|
<dd><cite>(<acronym>GSAB</acronym>) Spéalp 2 (1978) pp
|
||||||
|
66-67, <span lang="en" xml:lang="en">survey</span></cite>, <b lang=
|
||||||
|
"de" xml:lang="de">Feuertalsystem</b>, Jean Claude Hans<br />
|
||||||
|
<a href="782013.htm" lang="fr" xml:lang="fr">en Français</a>
|
||||||
|
/ (the English translation is essentially identical to the kataster
|
||||||
|
<a href="../../noinfo/1626/120.htm">cave description</a>)</dd>
|
||||||
|
<dt>79.1855</dt>
|
||||||
|
<dd><cite>(<acronym>GSAB</acronym>) Spéalp 3 (Oct. 1978) pp
|
||||||
|
44-45, <span lang="en" xml:lang="en">survey</span></cite>,
|
||||||
|
<b><span lang="de" xml:lang="de">Ahnenschacht</span> 77/78</b>,
|
||||||
|
Jean Pierre Braun<br />
|
||||||
|
<a href="fr/791855.htm" lang="fr" xml:lang="fr">en
|
||||||
|
Français</a> / <a href="en/791855.htm" lang="en" xml:lang=
|
||||||
|
"en"><span lang="en" xml:lang="en">English
|
||||||
|
Translation</span></a></dd>
|
||||||
</dl>
|
</dl>
|
||||||
<hr />
|
<hr />
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="../../1626/index.htm">Overview</a>
|
<li><a href="../../1626/index.htm">Overview</a> of area 1626, and
|
||||||
of area 1626, and index to caves</li>
|
index to caves</li>
|
||||||
<li><a href="../../areas.htm">Overview</a> of area 1623</li>
|
<li><a href="../../areas.htm">Overview</a> of area 1623</li>
|
||||||
<li>Back to <a href="../../index.htm">Expedition Intro page</a></li>
|
<li>Back to <a href="../../index.htm">Expedition Intro
|
||||||
<li><a href="../../../index.htm">Back to <acronym>CUCC</acronym> Home page</a></li>
|
page</a></li>
|
||||||
<li><a href="../index.htm">Other groups</a> who have worked in the area
|
<li><a href="../../../index.htm">Back to <acronym>CUCC</acronym>
|
||||||
|
Home page</a></li>
|
||||||
|
<li><a href="../index.htm">Other groups</a> who have worked in the
|
||||||
|
area</li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
</html>
|
</html>
|
||||||
|
|||||||
@@ -1,72 +1,79 @@
|
|||||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
|
||||||
<html>
|
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
||||||
|
<html xmlns="http://www.w3.org/1999/xhtml">
|
||||||
<head>
|
<head>
|
||||||
<title lang="fr">Groupe Spéléologique de Clerval -
|
<meta http-equiv="Content-Type" content=
|
||||||
Baume les Dames</title>
|
"text/html; charset=iso-8859-1" />
|
||||||
<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
|
<title lang="fr" xml:lang="fr">Groupe Spéléologique
|
||||||
|
de Clerval - Baume les Dames</title>
|
||||||
|
<link rel="stylesheet" type="text/css" href=
|
||||||
|
"../../css/main2.css" />
|
||||||
</head>
|
</head>
|
||||||
<body>
|
<body>
|
||||||
<center><h2 lang="fr">Groupe Spéléologique de Clerval -
|
<h1 lang="fr" xml:lang="fr">Groupe Spéléologique de
|
||||||
Baume les Dames</h2></center>
|
Clerval - Baume les Dames</h1>
|
||||||
|
<p>From the earliest days of CUCC's involvement in Austria, we
|
||||||
<p>From the earliest days of CUCC's involvement in Austria, we heard reports
|
heard reports of deep caves being explored by French Group(s). We
|
||||||
of deep caves being explored by French Group(s). We were aware that several
|
were aware that several caves explored by the Belgian <a href=
|
||||||
caves explored by the Belgian <a href="../gsab/index.htm" lang="fr">Groupe
|
"../gsab/index.htm" lang="fr" xml:lang="fr">Groupe
|
||||||
Spéléo Alpin Belge</a> had been found by French, including
|
Spéléo Alpin Belge</a> had been found by French,
|
||||||
<span lang="fr">Denis Motte</span>, whose name seemed to crop up in various
|
including <span lang="fr" xml:lang="fr">Denis Motte</span>, whose
|
||||||
places.
|
name seemed to crop up in various places.</p>
|
||||||
|
<p>This group worked in the 1626 area (<b lang="de" xml:lang=
|
||||||
<p>This group worked in the 1626 area (<b lang="de">Feuertal</b>) in 1974
|
"de">Feuertal</b>) in 1974 (<b lang="de" xml:lang=
|
||||||
(<b lang="de">Ahnenschacht</b> with <span lang="fr">GS Doubs & SC
|
"de">Ahnenschacht</b> with <span lang="fr" xml:lang="fr">GS Doubs
|
||||||
Vesoul</span>), and later (1975,77) worked in the <b lang="de">Tauplitz</b>
|
& SC Vesoul</span>), and later (1975,77) worked in the <b lang=
|
||||||
area to our east with finds including the impressive
|
"de" xml:lang="de">Tauplitz</b> area to our east with finds
|
||||||
<b lang="de">Nordwandschacht</b>, containing a huge chamber (320x80x60m).
|
including the impressive <b lang="de" xml:lang=
|
||||||
|
"de">Nordwandschacht</b>, containing a huge chamber
|
||||||
<p>During the eighties, they visited the
|
(320x80x60m).</p>
|
||||||
<b lang="de">Elmhöhlensystem</b> (touristed by CUCC in
|
<p>During the eighties, they visited the <b lang="de" xml:lang=
|
||||||
<a href="../../years/1976/report.htm#elmh">1976</a> and
|
"de">Elmhöhlensystem</b> (touristed by CUCC in <a href=
|
||||||
<a href="../../years/1977/report.htm#elmh">1977</a>). The results of this
|
"../../years/1976/report.htm#elmh">1976</a> and <a href=
|
||||||
work are described in <b lang="fr">Spelunca</b> number 26 (April/June
|
"../../years/1977/report.htm#elmh">1977</a>). The results of this
|
||||||
1987) pp 10-11 (CTS 88.1407).
|
work are described in <b lang="fr" xml:lang="fr">Spelunca</b>
|
||||||
|
number 26 (April/June 1987) pp 10-11 (CTS 88.1407).</p>
|
||||||
<p>Towards the end of this period, the group also had some members exploring
|
<p>Towards the end of this period, the group also had some members
|
||||||
on the <b lang="de">Vorderer Schwarzmooskogel</b>, who found
|
exploring on the <b lang="de" xml:lang="de">Vorderer
|
||||||
<b lang="de">Larchenschacht</b>
|
Schwarzmooskogel</b>, who found <b lang="de" xml:lang=
|
||||||
(<a href="../../noinfo/smkridge/88.htm">1623/88</a>).
|
"de">Larchenschacht</b> (<a href=
|
||||||
The whole expedition worked in this area (from 1987?). Various important
|
"../../noinfo/smkridge/88.htm">1623/88</a>). The whole expedition
|
||||||
connections were made, of which we have very little information to date. We
|
worked in this area (from 1987?). Various important connections
|
||||||
do know that they also explored various entrances further north towards
|
were made, of which we have very little information to date. We do
|
||||||
<b lang="de">Hinterer Schwarzmooskogel</b>, including one of the entrances to
|
know that they also explored various entrances further north
|
||||||
<b lang="de">Kaninchenhöhle</b>
|
towards <b lang="de" xml:lang="de">Hinterer Schwarzmooskogel</b>,
|
||||||
(<a href="../../smkridge/161/top.htm">1623/161</a>), into the area CUCC now
|
including one of the entrances to <b lang="de" xml:lang=
|
||||||
knows as "France". However, they abandoned this particular cave on the
|
"de">Kaninchenhöhle</b> (<a href=
|
||||||
assumption that it would connect into CUCC's caves. From 1991, the group
|
"../../smkridge/161/top.htm">1623/161</a>), into the area CUCC now
|
||||||
returned to the <span lang="de">Elmhöhlensystem</span>.
|
knows as "France". However, they abandoned this particular cave on
|
||||||
|
the assumption that it would connect into CUCC's caves. From 1991,
|
||||||
<p>The group publish a journal "<b lang="fr">Beaunes et Empoues</b>"
|
the group returned to the <span lang="de" xml:lang=
|
||||||
(issue number 10 was published in 1993), from which the above summary is
|
"de">Elmhöhlensystem</span>.</p>
|
||||||
derived.
|
<p>The group publish a journal "<b lang="fr" xml:lang="fr">Beaunes
|
||||||
|
et Empoues</b>" (issue number 10 was published in 1993), from which
|
||||||
<p>Contact was finally made with <span lang="fr">Denis Motte</span> at the
|
the above summary is derived.</p>
|
||||||
International Speleological Congress in the Swiss Jura in 1997, so CUCC are
|
<p>Contact was finally made with <span lang="fr" xml:lang=
|
||||||
looking forward to an era of cooperation in connecting the
|
"fr">Denis Motte</span> at the International Speleological Congress
|
||||||
<b lang="de">Kaninchenhöhle</b>
|
in the Swiss Jura in 1997, so CUCC are looking forward to an era of
|
||||||
(<a href="../../smkridge/161/top.htm">1623/161</a>)
|
cooperation in connecting the <b lang="de" xml:lang=
|
||||||
area caves through GSCB's finds to the
|
"de">Kaninchenhöhle</b> (<a href=
|
||||||
<b lang="de">Stellerweghöhlensystem</b>
|
"../../smkridge/161/top.htm">1623/161</a>) area caves through
|
||||||
(<a href="../../smkridge/41.htm">1623/41</a>).
|
GSCB's finds to the <b lang="de" xml:lang=
|
||||||
|
"de">Stellerweghöhlensystem</b> (<a href=
|
||||||
|
"../../smkridge/41.htm">1623/41</a>).</p>
|
||||||
<hr />
|
<hr />
|
||||||
|
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="../../indxal.htm">Index</a> of all caves documented in 1623.</li>
|
<li><a href="../../indxal.htm">Index</a> of all caves documented in
|
||||||
|
1623.</li>
|
||||||
<li><a href="../../areas.htm">Overview</a> of area 1623</li>
|
<li><a href="../../areas.htm">Overview</a> of area 1623</li>
|
||||||
<li><a href="../../1626/index.htm">Overview</a>
|
<li><a href="../../1626/index.htm">Overview</a> of area 1626, and
|
||||||
of area 1626, and index to caves</li>
|
index to caves</li>
|
||||||
<li>Back to <a href="../../index.htm">Expedition Intro page</a></li>
|
<li>Back to <a href="../../index.htm">Expedition Intro
|
||||||
|
page</a></li>
|
||||||
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
||||||
<li><a href="../index.htm">Other groups</a> who have worked in the area
|
<li><a href="../index.htm">Other groups</a> who have worked in the
|
||||||
|
area</li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
</html>
|
</html>
|
||||||
|
|||||||
294
others/index.htm
294
others/index.htm
@@ -1,156 +1,208 @@
|
|||||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
|
||||||
<html>
|
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
||||||
|
|
||||||
|
<html xmlns="http://www.w3.org/1999/xhtml">
|
||||||
<head>
|
<head>
|
||||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
<meta http-equiv="Content-Type" content=
|
||||||
<title>Totes Gebirge: groups</title>
|
"text/html; charset=us-ascii" />
|
||||||
<link rel="stylesheet" type="text/css" href="../css/main2.css" />
|
|
||||||
|
<title>Totes Gebirge: groups</title>
|
||||||
|
<link rel="stylesheet" type="text/css" href="../css/main2.css" />
|
||||||
</head>
|
</head>
|
||||||
|
|
||||||
<body>
|
<body>
|
||||||
<h2>Groups known to have worked in <span lang="de-at">Totes Gebirge</span> caves</h2>
|
<h1>Groups known to have worked in <span lang="de-at" xml:lang=
|
||||||
|
"de-at">Totes Gebirge</span> caves</h1>
|
||||||
|
|
||||||
<p>As well as local cavers (who were very few in number in the early years),
|
<p>As well as local cavers (who were very few in number in the
|
||||||
many cavers from outside Austria have worked in the <span lang="de-at">Totes
|
early years), many cavers from outside Austria have worked in the
|
||||||
Gebirge</span>. Those who have been to the western massif (1623 and 1626) are
|
<span lang="de-at" xml:lang="de-at">Totes Gebirge</span>. Those
|
||||||
listed here. Following the links will lead to a description of the group and
|
who have been to the western massif (1623 and 1626) are listed
|
||||||
a list of all the publications about the area (with their reference number
|
here. Following the links will lead to a description of the group
|
||||||
from Current Titles in Speleology). This is under research, and is very far
|
and a list of all the publications about the area (with their
|
||||||
from complete. However, some articles are here in the archive, in the
|
reference number from Current Titles in Speleology). This is
|
||||||
original language, and a very few are here in english translation. Where
|
under research, and is very far from complete. However, some
|
||||||
these exist, you can follow links to them.
|
articles are here in the archive, in the original language, and a
|
||||||
|
very few are here in english translation. Where these exist, you
|
||||||
|
can follow links to them.</p>
|
||||||
|
|
||||||
<p>A few groups are still active and have their own web pages - you can
|
<p>A few groups are still active and have their own web pages -
|
||||||
follow links to these from here, or there is a page specifically for
|
you can follow links to these from here, or there is a page
|
||||||
<a href="../links.htm">links to web sites</a> which includes other relevant
|
specifically for <a href="../links.htm">links to web sites</a>
|
||||||
organisations too.
|
which includes other relevant organisations too.</p>
|
||||||
|
|
||||||
<h4>Local Austrian Groups</h4>
|
<h4>Local Austrian Groups</h4>
|
||||||
|
|
||||||
<ul>
|
<ul>
|
||||||
<li><span lang="de-at">Höhlenforschervereinigung Altaussee</span>
|
<li><span lang="de-at" xml:lang=
|
||||||
(up to 1949 ?)
|
"de-at">Höhlenforschervereinigung Altaussee</span> (up to
|
||||||
|
1949?)</li>
|
||||||
|
|
||||||
<li><span lang="de-at">Sektion Ausseerland (des Landesvereines für
|
<li><span lang="de-at" xml:lang="de-at">Sektion Ausseerland
|
||||||
Höhlenkunde in Steiermark)</span> (up to early 80's ?)
|
(des Landesvereines für Höhlenkunde in
|
||||||
|
Steiermark)</span> (up to early 80's?)</li>
|
||||||
|
|
||||||
<li><span lang="de-at">Vereines für Höhlenkunde in OberSteier
|
<li><span lang="de-at" xml:lang="de-at">Vereines für
|
||||||
(VfHO)</span><br>
|
Höhlenkunde in OberSteier (VfHO)</span>:
|
||||||
This is the group who are responsible for the kataster in our area, and
|
This is the group who are responsible for the kataster in our
|
||||||
which several CUCC members have also joined. There are two articles
|
area, and which several CUCC members have also joined. There
|
||||||
about diving in Liägerhöhle (1623/1) in
|
are two articles about diving in Liägerhöhle (1623/1)
|
||||||
<a href="obsteier/dive1.htm" lang="de-at">1985</a> and
|
in <a href="obsteier/dive1.htm" lang="de-at" xml:lang=
|
||||||
<a href="obsteier/dive2.htm" lang="de-at">1988</a>, on the site. Also from
|
"de-at">1985</a> and <a href="obsteier/dive2.htm" lang="de-at"
|
||||||
their journal is the German translation of CUCC's
|
xml:lang="de-at">1988</a>, on the site. Also from their journal
|
||||||
<a href="../years/1996/bcra-d.htm" lang="de">1996 report</a>.
|
is the German translation of CUCC's <a href=
|
||||||
|
"../years/1996/bcra-d.htm" lang="de" xml:lang="de">1996
|
||||||
|
report</a>.</li>
|
||||||
|
|
||||||
<li><span lang="de-at">Landesverein für Höhlenkunde in
|
<li><span lang="de-at" xml:lang="de-at">Landesverein für
|
||||||
Oberösterreich (LVHO)</span> (with a website in
|
Höhlenkunde in Oberösterreich (LVHO)</span>:
|
||||||
<a href="http://alpha.aec.at/cave/cave.html" lang="en">English</a> or
|
This is the group responsible for exploration of the <b lang=
|
||||||
<a href="http://alpha.aec.at/cave/" lang="de-at">German</a>).<br>
|
"de-at" xml:lang="de-at">Raucherkarhöhle</b>, and for the
|
||||||
This is the group responsible for exploration of the
|
kataster in nearby area 1626.</li>
|
||||||
<b lang="de-at">Raucherkarhöhle</b>, and for the kataster in nearby area
|
</ul>
|
||||||
1626.
|
|
||||||
|
|
||||||
</ul>
|
<h4>Other Austrian Groups and individuals</h4>
|
||||||
|
|
||||||
<h4>Other Austrian Groups and individuals</h4>
|
<ul>
|
||||||
|
<li><span lang="de-at" xml:lang="de-at">Edith
|
||||||
|
Bednarik</span></li>
|
||||||
|
</ul>
|
||||||
|
|
||||||
<ul>
|
<h4>British Groups</h4>
|
||||||
<li><span lang="de-at">Edith Bednarik</span>
|
|
||||||
</ul>
|
|
||||||
|
|
||||||
<h4>British Groups</h4>
|
<ul>
|
||||||
|
<li><a href="bec/index.htm">BEC</a>: Bristol Exploration Club
|
||||||
|
[1967, 1968, 1969] (<a href=
|
||||||
|
"http://web.ukonline.co.uk/john/">Home page</a>)</li>
|
||||||
|
|
||||||
<ul>
|
<li><a href="../../index.htm">CUCC</a>: Cambridge University
|
||||||
<li><a href="bec/index.htm">BEC</a>: Bristol Exploration Club [1967, 1968, 1969] (<a href="http://web.ukonline.co.uk/john/">Home page</a>)
|
Caving Club [1976-97]</li>
|
||||||
<li><a href="../../index.htm">CUCC</a>: Cambridge University Caving Club [1976-97]
|
|
||||||
<li><a href="ubss/index.htm">UBSS</a>: University of Bristol Speleological Society [with CUCC 1981, 1982, independently in 1989, 1990 ?]
|
|
||||||
<li><a href="luss/index.htm">LUSS</a>: Lancaster University Speleological Society [1987-89] (<a href="http://www.comp.lancs.ac.uk/rec-and-travel/luss/">Home page</a>)
|
|
||||||
<li><a href="ulsa/index.htm">ULSA</a>: University of Leeds Speleological Association [Tauplitz, 1985 (or 86?)] (<a href="http://www.leeds.ac.uk/union/socs/speleological/home.htm">Home page</a>)
|
|
||||||
</ul>
|
|
||||||
|
|
||||||
<h4>Belgian Groups</h4>
|
<li><a href="ubss/index.htm">UBSS</a>: University of Bristol
|
||||||
|
Speleological Society [with CUCC 1981, 1982, independently in
|
||||||
|
1989, 1990 ?]</li>
|
||||||
|
|
||||||
<ul>
|
<li><a href="luss/index.htm">LUSS</a>: Lancaster University
|
||||||
<li><span lang="fr-be">CASE HA (Club d'Archaeologie, de
|
Speleological Society [1987-89] (<a href=
|
||||||
Spéléologie et d'Escalade de Huy Andenne)</span> [1972,1973]
|
"http://www.comp.lancs.ac.uk/rec-and-travel/luss/">Home
|
||||||
|
page</a>)</li>
|
||||||
|
|
||||||
<li><span lang="fr-be"><a href="gsab/index.htm" lang="en">GSAB</a>: Groupe
|
<li><a href="ulsa/index.htm">ULSA</a>: University of Leeds
|
||||||
Spéléo Alpin Belge</span>
|
Speleological Association [Tauplitz, 1985 (or 86?)] (<a href=
|
||||||
[1972,1973,1974,1975,1976,1977,1978]<br>
|
"http://www.leeds.ac.uk/union/socs/speleological/home.htm">Home
|
||||||
(people of other club affiliations out with GSAB in 1977, CASEO, SSSPA,
|
page</a>)</li>
|
||||||
GSREDAN, ES GEODE, SC Calcaires, similarly GIPS, SCUCL in 1978)
|
</ul>
|
||||||
|
|
||||||
<li>CASEO 1975
|
<h4>Belgian Groups</h4>
|
||||||
</ul>
|
|
||||||
|
|
||||||
<h4>French Groups</h4>
|
<ul>
|
||||||
|
<li><span lang="fr-be" xml:lang="fr-be">CASE HA (Club
|
||||||
|
d'Archaeologie, de Spéléologie et d'Escalade de
|
||||||
|
Huy Andenne)</span> [1972,1973]</li>
|
||||||
|
|
||||||
<ul>
|
<li><span lang="fr-be" xml:lang="fr-be"><a href=
|
||||||
<li><span lang="fr">G.S.Clerval</span>,
|
"gsab/index.htm" lang="en" xml:lang="en">GSAB</a>: Groupe
|
||||||
now <span lang="fr">G.S.Clerval - Baume les Dames</span>
|
Spéléo Alpin Belge</span>
|
||||||
(<a href="gscb/index.htm">GSCB</a>) 1974, 75, 77, 83-87, 88-90?, 91-...
|
[1972,1973,1974,1975,1976,1977,1978]<br />
|
||||||
<li><span lang="fr">S.C. Vesoul</span> \
|
(people of other club affiliations out with GSAB in 1977,
|
||||||
<li><span lang="fr">G.S. Doubs</span> } 1974
|
CASEO, SSSPA, GSREDAN, ES GEODE, SC Calcaires, similarly GIPS,
|
||||||
<li><span lang="fr">S.S. Daules</span> /
|
SCUCL in 1978)</li>
|
||||||
<li><span lang="fr">A.C. Toulon</span> \
|
|
||||||
<li><span lang="fr">S.C. Toulon</span> } 1976, 1977?
|
|
||||||
<li><span lang="fr">Lou Darboun</span> /
|
|
||||||
<li><span lang="fr">Spéléo Ragaie</span> /
|
|
||||||
</ul>
|
|
||||||
|
|
||||||
<h4>not quite sure, French or Belgian ?</h4>
|
<li>CASEO 1975</li>
|
||||||
|
</ul>
|
||||||
|
|
||||||
<ul>
|
<h4>French Groups</h4>
|
||||||
<li><span lang="fr">CARSS 1975, 1978 (Centre d'Activité et
|
|
||||||
Récherches Subaquatique et Souterrainne)</span>
|
|
||||||
</ul>
|
|
||||||
|
|
||||||
<h4>German Groups and individuals</h4>
|
<ul>
|
||||||
|
<li><span lang="fr" xml:lang="fr">G.S.Clerval</span>, now
|
||||||
|
<span lang="fr" xml:lang="fr">G.S.Clerval - Baume les
|
||||||
|
Dames</span> (<a href="gscb/index.htm">GSCB</a>) 1974, 75, 77,
|
||||||
|
83-87, 88-90?, 91-...</li>
|
||||||
|
|
||||||
<ul>
|
<li><span lang="fr" xml:lang="fr">S.C. Vesoul</span>,</li>
|
||||||
<li><span lang="de">Vereines für Höhlenkunde in München
|
|
||||||
e.V.</span> 1983 and others. The site contains one article from this group
|
|
||||||
which is CTS ref.
|
|
||||||
<a lang="de" href="muenchen/de/841642.htm">84.1642</a>, also now included
|
|
||||||
in <a href="muenchen/en/841642.htm">English translation.</a>
|
|
||||||
|
|
||||||
<li>A group from <span lang="de">Nürnberg</span> who worked with the
|
<li><span lang="fr" xml:lang="fr">G.S. Doubs</span>,</li>
|
||||||
above, but also worked independently - they have some survey data we need !
|
|
||||||
<li><span lang="de"><a href="http://arge.itvd.uni-stuttgart.de/"
|
|
||||||
lang="de">Arbeitsgemeinschaft Höhle und Karst Grabenstetten
|
|
||||||
e.V.</a></span>
|
|
||||||
<li><span lang="de">Vred Vischer</span> 1980 (worked/s with above)
|
|
||||||
</ul>
|
|
||||||
|
|
||||||
<h4>Polish</h4>
|
<li><span lang="fr" xml:lang="fr">S.S. Daules</span> (all in 1974)</li>
|
||||||
|
|
||||||
<ul>
|
<li><span lang="fr" xml:lang="fr">A.C. Toulon</span>,</li>
|
||||||
<li><span lang="pl">Speleo Krakow</span><br>
|
|
||||||
An article in a Polish journal has misled the authors of the English version
|
|
||||||
of the world deep caves atlas into thinking that Poles worked with CUCC. In
|
|
||||||
fact, the article was commissioned by <span lang="pl">Krzysztof
|
|
||||||
Kleszynski</span> who had done a lot of work in the Salzburg area. It was
|
|
||||||
written by Andy Waddington, covering 1976-79 (and particularly the
|
|
||||||
exploration of <span lang="de-at">Eislufthöhle</span>), and concerns
|
|
||||||
only work done by CUCC. It appeared in the Polish journal purely as part of
|
|
||||||
an effort to give some context to other reports about Austria. Andy never got
|
|
||||||
a copy (but then he can't read the Polish translation anyway). The
|
|
||||||
<a href="../years/1979/811412.htm">english original</a> is published in these
|
|
||||||
pages for the first time !
|
|
||||||
|
|
||||||
</ul>
|
<li><span lang="fr" xml:lang="fr">S.C. Toulon</span>,</li>
|
||||||
|
|
||||||
<h4>Italian, Hungarian, Slovak ...</h4>
|
<li><span lang="fr" xml:lang="fr">Lou Darboun</span>,</li>
|
||||||
|
|
||||||
<ul>
|
<li><span lang="fr" xml:lang="fr">Spéléo
|
||||||
<li>We think there may have been some...
|
Ragaie</span> (all in 1976, 77?)</li>
|
||||||
</ul>
|
</ul>
|
||||||
|
|
||||||
|
<h4>not quite sure, French or Belgian ?</h4>
|
||||||
|
|
||||||
|
<ul>
|
||||||
|
<li><span lang="fr" xml:lang="fr">CARSS 1975, 1978 (Centre
|
||||||
|
d'Activité et Récherches Subaquatique et
|
||||||
|
Souterrainne)</span></li>
|
||||||
|
</ul>
|
||||||
|
|
||||||
|
<h4>German Groups and individuals</h4>
|
||||||
|
|
||||||
|
<ul>
|
||||||
|
<li><span lang="de" xml:lang="de">Vereines für
|
||||||
|
Höhlenkunde in München e.V.</span> 1983 and others.
|
||||||
|
The site contains one article from this group which is CTS ref.
|
||||||
|
<a lang="de" href="muenchen/de/841642.htm" xml:lang=
|
||||||
|
"de">84.1642</a>, also now included in <a href=
|
||||||
|
"muenchen/en/841642.htm">English translation.</a></li>
|
||||||
|
|
||||||
|
<li>A group from <span lang="de" xml:lang=
|
||||||
|
"de">Nürnberg</span> who worked with the above, but also
|
||||||
|
worked independently - they have some survey data we need
|
||||||
|
!</li>
|
||||||
|
|
||||||
|
<li><span lang="de" xml:lang="de"><a href=
|
||||||
|
"http://arge.itvd.uni-stuttgart.de/" lang="de" xml:lang=
|
||||||
|
"de">Arbeitsgemeinschaft Höhle und Karst Grabenstetten
|
||||||
|
e.V.</a></span></li>
|
||||||
|
|
||||||
|
<li><span lang="de" xml:lang="de">Vred Vischer</span> 1980
|
||||||
|
(worked/s with above)</li>
|
||||||
|
</ul>
|
||||||
|
|
||||||
|
<h4>Polish</h4>
|
||||||
|
|
||||||
|
<ul>
|
||||||
|
<li><span lang="pl" xml:lang="pl">Speleo Krakow</span><br />
|
||||||
|
An article in a Polish journal has misled the authors of the
|
||||||
|
English version of the world deep caves atlas into thinking
|
||||||
|
that Poles worked with CUCC. In fact, the article was
|
||||||
|
commissioned by <span lang="pl" xml:lang="pl">Krzysztof
|
||||||
|
Kleszynski</span> who had done a lot of work in the Salzburg
|
||||||
|
area. It was written by Andy Waddington, covering 1976-79 (and
|
||||||
|
particularly the exploration of <span lang="de-at" xml:lang=
|
||||||
|
"de-at">Eislufthöhle</span>), and concerns only work done
|
||||||
|
by CUCC. It appeared in the Polish journal purely as part of an
|
||||||
|
effort to give some context to other reports about Austria.
|
||||||
|
Andy never got a copy (but then he can't read the Polish
|
||||||
|
translation anyway). The <a href=
|
||||||
|
"../years/1979/811412.htm">english original</a> is published in
|
||||||
|
these pages for the first time !</li>
|
||||||
|
</ul>
|
||||||
|
|
||||||
|
<h4>Italian, Hungarian, Slovak ...</h4>
|
||||||
|
|
||||||
|
<ul>
|
||||||
|
<li>We think there may have been some...</li>
|
||||||
|
</ul>
|
||||||
|
|
||||||
|
<hr />
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<ul>
|
|
||||||
<li><a href="../index.htm">Back to Expedition Intro page</a></li>
|
<ul>
|
||||||
<li><a href="../indxal.htm">Full Index</a></li>
|
<li><a href="../index.htm">Back to Expedition Intro
|
||||||
<li><a href="../../index.htm">Back to CUCC Home page</a></li>
|
page</a></li>
|
||||||
</ul>
|
|
||||||
|
<li><a href="../indxal.htm">Full Index</a></li>
|
||||||
|
|
||||||
|
<li><a href="../../index.htm">Back to CUCC Home page</a></li>
|
||||||
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
</html>
|
</html>
|
||||||
|
|||||||
@@ -1,86 +1,94 @@
|
|||||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
|
||||||
<html>
|
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
||||||
|
<html xmlns="http://www.w3.org/1999/xhtml">
|
||||||
<head>
|
<head>
|
||||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
<meta name="generator" content=
|
||||||
|
"HTML Tidy for Linux/x86 (vers 1st March 2004), see www.w3.org" />
|
||||||
|
<meta http-equiv="Content-Type" content=
|
||||||
|
"text/html; charset=us-ascii" />
|
||||||
<title>1623 and 1626: LUSS Reports</title>
|
<title>1623 and 1626: LUSS Reports</title>
|
||||||
<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
|
<link rel="stylesheet" type="text/css" href=
|
||||||
|
"../../css/main2.css" />
|
||||||
</head>
|
</head>
|
||||||
<body>
|
<body>
|
||||||
<h1>Lancaster University Speleological Society</h1>
|
<h1>Lancaster University Speleological Society</h1>
|
||||||
|
<p>LUSS, and its graduate offspring, the Society of Lancaster
|
||||||
<p>LUSS, and its graduate offspring, the Society of Lancaster University
|
University Graduate Speleologists (SLUGS), is based on campus in
|
||||||
Graduate Speleologists (SLUGS), is based on campus in Lancaster, within very
|
Lancaster, within very easy reach of the Yorkshire Dales. Hence it
|
||||||
easy reach of the Yorkshire Dales. Hence it has become one of the more
|
has become one of the more active clubs over the years, with young
|
||||||
active clubs over the years, with young cavers trained on weekends in
|
cavers trained on weekends in Yorkshire travelling further afield
|
||||||
Yorkshire travelling further afield each summer. Best known for major
|
each summer. Best known for major explorations in the Picos de
|
||||||
explorations in the Picos de Europa of Northern Spain, it has a reputation
|
Europa of Northern Spain, it has a reputation for high quality (if
|
||||||
for high quality (if infrequent) publication.
|
infrequent) publication.</p>
|
||||||
|
<p>LUSS have their <a href=
|
||||||
<p>LUSS have their
|
"http://www.ednet.lancs.ac.uk/luss/index.html">own web pages</a>,
|
||||||
<a href="http://www.ednet.lancs.ac.uk/luss/index.html">
|
or may be contacted via their <a href=
|
||||||
own web pages</a>, or may be contacted via their
|
"http://www.ednet.lancs.ac.uk/luss/contact.html">contact page</a>
|
||||||
<a href="http://www.ednet.lancs.ac.uk/luss/contact.html">contact page</a>
|
or maybe directly through email. Their web page gives:<br /></p>
|
||||||
or maybe directly through email. Their web page gives:<br>
|
<p style="text-align: center"><img src=
|
||||||
<center>
|
"../../../icons/email.png" alt="" /> LUSS@lancaster.ac.uk <i>(but I
|
||||||
<img src="../../../icons/email.png"> LUSS@lancaster.ac.uk
|
get a bounce from this address)</i></p>
|
||||||
but I get a bounce from this address
|
<p>Lancaster University Speleological Society worked in an area out
|
||||||
</center>
|
to the north of CUCC's home turf, between Wildensee, Hohes
|
||||||
|
Augst-Eck and Gr. Scheibling Kogel, on three expeditions in 1987,
|
||||||
<p>Lancaster University Speleological Society worked in an area out to the
|
1988 and 1989. Some of the caves they explored lie within the 1623
|
||||||
north of CUCC's home turf, between Wildensee, Hohes Augst-Eck and Gr.
|
area, although the boundaries between areas are not very
|
||||||
Scheibling Kogel, on three expeditions in 1987, 1988 and 1989. Some of the
|
well-defined hereabouts.</p>
|
||||||
caves they explored lie within the 1623 area, although the boundaries
|
<p>The descriptions included in our pages are taken (with
|
||||||
between areas are not very well-defined hereabouts.
|
permission, for which our thanks) directly from their reports,
|
||||||
|
published in the UK:</p>
|
||||||
<p>The descriptions included in our pages are taken (with permission, for
|
<p><cite><b>CTS 88.1467</b> <a href=
|
||||||
which our thanks) directly from their reports, published in the UK:
|
"http://www.ednet.lancs.ac.uk/luss/Exploration/Austria/are87.html">Austria
|
||||||
|
Reconnaissance Expedition 1987</a>, Lancaster University
|
||||||
<p><cite><b>CTS 88.1467</b> <a href="http://www.ednet.lancs.ac.uk/luss/Exploration/Austria/are87.html">Austria Reconnaissance Expedition 1987</a>,
|
Speleological Society</cite><br />
|
||||||
Lancaster University Speleological Society</cite><br>
|
<cite><b>CTS 89.1866</b> Dead Mountains Expedition 1988,
|
||||||
|
L.U.S.S.</cite> 24pp illus.<br /></p>
|
||||||
<cite><b>CTS 89.1866</b> Dead Mountains Expedition 1988, L.U.S.S.</cite> 24pp illus.<br>
|
<p>I only have an incomplete pre-publication report from 1989 (the
|
||||||
|
full report was never published), which means that there is no
|
||||||
<p>I only have an incomplete pre-publication report from 1989 (the full
|
description of the 1989 extensions to LA11 in these pages.</p>
|
||||||
report was never published), which means that there is no description of the
|
<p>Copies of these reports (if still in print) are available
|
||||||
1989 extensions to LA11 in these pages.
|
from:</p>
|
||||||
|
<p>Lancaster University Speleological Society,<br />
|
||||||
<p>Copies of these reports (if still in print) are available from:
|
c/o Neil Turton,<br />
|
||||||
|
34, Williamson Rd.<br />
|
||||||
<p>Lancaster University Speleological Society,<br>
|
Lancaster.<br />
|
||||||
c/o Neil Turton,<br>
|
United Kingdom</p>
|
||||||
34, Williamson Rd.<br>
|
<p>(note that the Bailrigg campus Pigeon Holes address, given in
|
||||||
Lancaster.<br>
|
many LUSS publications and in old versions of this page, is now
|
||||||
United Kingdom
|
unlikely to reach the Society).</p>
|
||||||
|
<p>As they <i>may</i> still be in print, these reports are not in
|
||||||
<p>(note that the Bailrigg campus Pigeon Holes address, given in many
|
our web pages at present, though the descriptions of caves in 1623,
|
||||||
LUSS publications and in old versions of this page, is now unlikely to reach
|
and the more significant ones in 1626 are. <b>Stoppress</b>: from
|
||||||
the Society).
|
1999, some of this material is appearing on the LUSS website (see
|
||||||
|
link above). Expect the C&C 38 article to appear shortly, but
|
||||||
<p>As they <i>may</i> still be in print, these reports are not in our web
|
currently the link in LUSS's own index page is broken, so I don't
|
||||||
pages at present, though the descriptions of caves in 1623, and the more
|
know the URL.</p>
|
||||||
significant ones in 1626 are. <b>Stoppress</b>: from 1999, some of this
|
<p>Other reports of the LUSS work appear in:<br />
|
||||||
material is appearing on the LUSS website (see link above). Expect the
|
<cite><b>CTS 87.1514</b> LUSS Austria Reconnaissance
|
||||||
C&C 38 article to appear shortly, but currently the link in LUSS's own
|
Expedition<br />
|
||||||
index page is broken, so I don't know the URL.
|
BCRA Caves & Caving 38 (Winter 1987), pp 27-30</cite><br />
|
||||||
|
<cite><b>CTS 88.1468</b> LUSS The Dead Mountains Expedition<br />
|
||||||
<p>Other reports of the LUSS work appear in:<br>
|
BCRA Caves & Caving 42 (Winter 1988), pp 20-21</cite><br />
|
||||||
|
<cite><b>CTS 89.1844</b> The Dead Mountains Expedition 1988, P
|
||||||
<cite><b>CTS 87.1514</b> LUSS Austria Reconnaissance Expedition<br> BCRA Caves & Caving 38 (Winter 1987), pp 27-30</cite><br>
|
Ibberson<br />
|
||||||
<cite><b>CTS 88.1468</b> LUSS The Dead Mountains Expedition<br> BCRA Caves & Caving 42 (Winter 1988), pp 20-21</cite><br>
|
Expeditions Yearbook 1988, pp 91-92</cite> (obtainable from the
|
||||||
<cite><b>CTS 89.1844</b> The Dead Mountains Expedition 1988, P Ibberson<br> Expeditions Yearbook 1988, pp 91-92</cite>
|
Expeditions Advisory Centre, London.)<br />
|
||||||
(obtainable from the Expeditions Advisory Centre, London.)<br>
|
<cite><b>CTS 90.1298</b> The Dead Mountains Expedition 1989, P
|
||||||
<cite><b>CTS 90.1298</b> The Dead Mountains Expedition 1989, P Ibberson</cite><br> BCRA Caves & Caving 47 (Spring 1990), pp 25-28
|
Ibberson</cite><br />
|
||||||
|
BCRA Caves & Caving 47 (Spring 1990), pp 25-28</p>
|
||||||
<hr /><p>
|
<hr />
|
||||||
<!-- LINKS -->
|
<p><!-- LINKS --></p>
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="../../indxal.htm">Index</a> of all caves documented in 1623.</li>
|
<li><a href="../../indxal.htm">Index</a> of all caves documented in
|
||||||
|
1623.</li>
|
||||||
<li><a href="../../areas.htm">Overview</a> of area 1623</li>
|
<li><a href="../../areas.htm">Overview</a> of area 1623</li>
|
||||||
<li><a href="../../1626/index.htm">Overview</a>
|
<li><a href="../../1626/index.htm">Overview</a> of area 1626, and
|
||||||
of area 1626, and index to caves</li>
|
index to caves</li>
|
||||||
<li>Back to <a href="../../index.htm">Expedition Intro page</a></li>
|
<li>Back to <a href="../../index.htm">Expedition Intro
|
||||||
|
page</a></li>
|
||||||
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
||||||
<li><a href="../index.htm">Other groups</a> who have worked in the area
|
<li><a href="../index.htm">Other groups</a> who have worked in the
|
||||||
|
area</li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
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|
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|
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<html lang=de-at>
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"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
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<html lang="de-at" xmlns="http://www.w3.org/1999/xhtml" xml:lang=
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"de-at">
|
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<head>
|
<head>
|
||||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
<meta http-equiv="Content-Type" content=
|
||||||
<title>
|
"text/html; charset=iso-8859-1" />
|
||||||
1623-1: dive 1985
|
<title>1623-1: dive 1985</title>
|
||||||
</title>
|
<link rel="stylesheet" type="text/css" href=
|
||||||
<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
|
"../../css/main2.css" />
|
||||||
</head>
|
</head>
|
||||||
<body>
|
<body>
|
||||||
<h2>TAUCHEINSATZ IN DER LIAGER-HÖHLE BEI ALTAUSSEE (1623/1)</h2>
|
<h1>TAUCHEINSATZ IN DER LIAGER-HÖHLE BEI ALTAUSSEE
|
||||||
|
(1623/1)</h1>
|
||||||
Sepp Steinberger
|
<p style="text-align: right"><b>Sepp Steinberger</b></p>
|
||||||
|
<p><i>(Mitteilungen des Vereines für Höhlenkunde in
|
||||||
<p><i>(Mitteilungen des Vereines für Höhlenkunde in Obersteier 4(2) 1985 pp 26-27)</i>
|
Obersteier 4(2) 1985 pp 26-27)</i></p>
|
||||||
|
<p>Nachdem die Redaktion über ein Jahr vergeblich versucht
|
||||||
<p>Nachdem die Redaktion über ein Jahr vergeblich versucht hat, von den
|
hat, von den Hauptakteuren (Tauchern) einen Bericht über
|
||||||
Hauptakteuren (Tauchern) einen Bericht über dieses sehr aufwendige
|
dieses sehr aufwendige Unternehmen zu erhalten, erlaube ich mir, da
|
||||||
Unternehmen zu erhalten, erlaube ich mir, da Dokumentation doch eine der
|
Dokumentation doch eine der Hauptaufgaben unserer
|
||||||
Hauptaufgaben unserer Höhlenkundlichen Tätigkeit ist, ein paar
|
Höhlenkundlichen Tätigkeit ist, ein paar Zeilen über
|
||||||
Zeilen über die Ereignisse zu verlieren.
|
die Ereignisse zu verlieren.</p>
|
||||||
|
<p>Am 5 August 1984 wurde von Mitgliedern unseres Vereines eine
|
||||||
<p>Am 5 August 1984 wurde von Mitgliedern unseres Vereines eine Tauchaktion
|
Tauchaktion in der Liager-Höhle bei Altaussee unternommen.
|
||||||
in der Liager-Höhle bei Altaussee unternommen. Ziel des Einsatzes war
|
Ziel des Einsatzes war es, in Quelltopf, dessen Tiefe auf 16 Meter
|
||||||
es, in Quelltopf, dessen Tiefe auf 16 Meter gelotet worden war, zu tauchen,
|
gelotet worden war, zu tauchen, und somit über seine Tiefe,
|
||||||
und somit über seine Tiefe, Gestalt und etwaige Fortsetzungen Kenntnis
|
Gestalt und etwaige Fortsetzungen Kenntnis zu erhalten. Es ist in
|
||||||
zu erhalten. Es ist in einer "zeitweilig aktiven Wasserhöhle", wie sie
|
einer "zeitweilig aktiven Wasserhöhle", wie sie die
|
||||||
die Liager-Höhle darstellt, sehr wichtig, die äußeren
|
Liager-Höhle darstellt, sehr wichtig, die äußeren
|
||||||
Umstände - sprich Wetter und Schneelage - zu beachten. Schon zu
|
Umstände - sprich Wetter und Schneelage - zu beachten. Schon
|
||||||
Pfingsten 1984 war diese Aktion geplant gewesen, wurde aber abgesagt, weil
|
zu Pfingsten 1984 war diese Aktion geplant gewesen, wurde aber
|
||||||
man befürchten mußte, daß durch die Schneeschmelze eine
|
abgesagt, weil man befürchten mußte, daß durch die
|
||||||
überraschende Aktivität eintreten könnte. So einigten wir uns
|
Schneeschmelze eine überraschende Aktivität eintreten
|
||||||
auf diesen Termin und begannen auch gleich mit umfangreichen
|
könnte. So einigten wir uns auf diesen Termin und begannen
|
||||||
Vorbereitungsarbeiten.
|
auch gleich mit umfangreichen Vorbereitungsarbeiten.</p>
|
||||||
|
<p>Um nicht die Taucher allein in die Höhle schicken zu
|
||||||
<p>Um nicht die Taucher allein in die Höhle schicken zu müssen,
|
müssen, sollte ser Wasserspiegel im "Ostsiphon" gesenkt
|
||||||
sollte ser Wasserspiegel im "Ostsiphon" gesenkt werden, sodaß auch die
|
werden, sodaß auch die Begleitmannschaft und das Reporterteam
|
||||||
Begleitmannschaft und das Reporterteam (ORF-Fernsehen und Bayerischer
|
(ORF-Fernsehen und Bayerischer Rundfunk) samt allen empfindlichen
|
||||||
Rundfunk) samt allen empfindlichen Geräten an Ort und Stelle gelangen
|
Geräten an Ort und Stelle gelangen konnten. Dies geschah mit
|
||||||
konnten. Dies geschah mit einem 20 Meter langen Kunnststoffschlauch (50 mm
|
einem 20 Meter langen Kunnststoffschlauch (50 mm Dm.), den uns der
|
||||||
Dm.), den uns der Salzbergbau Altaussee zur Verfügung gestellt hatte.
|
Salzbergbau Altaussee zur Verfügung gestellt hatte. Mit diesem
|
||||||
Mit diesem sollte das Wasser des Siphones abgeherbert werden, was erst nach
|
sollte das Wasser des Siphones abgeherbert werden, was erst nach
|
||||||
mehreren kräfteraubenden Versuchen gelang. Die Schwierigkeit dabei war,
|
mehreren kräfteraubenden Versuchen gelang. Die Schwierigkeit
|
||||||
den sperrigen Schlauch mit Wasser zu füllen und so den Abhebevorgang zu
|
dabei war, den sperrigen Schlauch mit Wasser zu füllen und so
|
||||||
starten. Außerdem ist die Höhendifferenz von der Ansaugstelle zum
|
den Abhebevorgang zu starten. Außerdem ist die
|
||||||
Abfluß eher gering. Am 4 August fand dann die Einsatzbesprechung mit
|
Höhendifferenz von der Ansaugstelle zum Abfluß eher
|
||||||
allen Teilnehmern statt, bei welcher alle Einzelheiten besprochen und
|
gering. Am 4 August fand dann die Einsatzbesprechung mit allen
|
||||||
diverse Schwierigkeiten erörtert wurden.
|
Teilnehmern statt, bei welcher alle Einzelheiten besprochen und
|
||||||
|
diverse Schwierigkeiten erörtert wurden.</p>
|
||||||
<p>Am Sonntag, 5 August 1985, ist es schließlich so weit: Um 9 Uhr
|
<p>Am Sonntag, 5 August 1985, ist es schließlich so weit: Um
|
||||||
vormittag treffen alle Teilnehmer in Altaussee ein. Die gesamte
|
9 Uhr vormittag treffen alle Teilnehmer in Altaussee ein. Die
|
||||||
Ausrüstung wird auf das Schnellboot der Wasserrettung Altaussee
|
gesamte Ausrüstung wird auf das Schnellboot der Wasserrettung
|
||||||
verladen und in einigen Fahrten zusammen mit der Mannschaft in die Seewiese
|
Altaussee verladen und in einigen Fahrten zusammen mit der
|
||||||
befördert. Von Seeufer bis zur Höhle betätigen sich alle
|
Mannschaft in die Seewiese befördert. Von Seeufer bis zur
|
||||||
Teilnehmer als "Sherpas" und tragen in mehreren Gängen die einige
|
Höhle betätigen sich alle Teilnehmer als "Sherpas" und
|
||||||
hundert Kilo schwere Ausrüstung zum Höhleneingang: Scheinwerfer,
|
tragen in mehreren Gängen die einige hundert Kilo schwere
|
||||||
Akkus, Video-Aufzeichnungsgerät, Preßluftflaschen, Helme,
|
Ausrüstung zum Höhleneingang: Scheinwerfer, Akkus,
|
||||||
Tauchanzüge, Schlauchtboot, Sicherungsseile, Drahtseilleitern und
|
Video-Aufzeichnungsgerät, Preßluftflaschen, Helme,
|
||||||
vieles mehr. R.Mascha, R.Seebacher und H.Segl bilden den Vortrupp und sehen
|
Tauchanzüge, Schlauchtboot, Sicherungsseile, Drahtseilleitern
|
||||||
nach, wie weit der Wasserspiegel im Ostsiphon gesunken ist (der
|
und vieles mehr. R.Mascha, R.Seebacher und H.Segl bilden den
|
||||||
Abhebeversuch war erst am Vortag geglückt), und ob der Siphon auch
|
Vortrupp und sehen nach, wie weit der Wasserspiegel im Ostsiphon
|
||||||
für "Nichttaucher" zu befahren ist. Nun beginnt der Transport der
|
gesunken ist (der Abhebeversuch war erst am Vortag geglückt),
|
||||||
Ausrüstung. Die Mitglieder der Mannschaft bilden immer wieder eine
|
und ob der Siphon auch für "Nichttaucher" zu befahren ist. Nun
|
||||||
Kette und schaffen in schweißtreibender Arbeit die Ausrüstung
|
beginnt der Transport der Ausrüstung. Die Mitglieder der
|
||||||
durch die teilweise engen Höhlenteile des "Ostganges". Der letzte
|
Mannschaft bilden immer wieder eine Kette und schaffen in
|
||||||
Höhlenteil vor dem Quelltopf ("Schragschacht") erweist sich wegen des
|
schweißtreibender Arbeit die Ausrüstung durch die
|
||||||
glitschigen Lehmes und seiner Steilheit als sehr schwierig zu befahren und
|
teilweise engen Höhlenteile des "Ostganges". Der letzte
|
||||||
muß an einigen Stellen mit Seilsicherungen versehen werden. Endlich am
|
Höhlenteil vor dem Quelltopf ("Schragschacht") erweist sich
|
||||||
eigentlichen Ziel angelangt, wird der etwa 15 Meter hohe Senkrechtabstieg
|
wegen des glitschigen Lehmes und seiner Steilheit als sehr
|
||||||
zum See für die Taucher gesichert und ein Schlauchboot zu Wasser
|
schwierig zu befahren und muß an einigen Stellen mit
|
||||||
gelassen. Das boot ist für den Techniker gedacht, der mit dem Taucher
|
Seilsicherungen versehen werden. Endlich am eigentlichen Ziel
|
||||||
über ein Kabel verbunden ist und sogar mit ihm sprechen kann. Ein
|
angelangt, wird der etwa 15 Meter hohe Senkrechtabstieg zum See
|
||||||
Taucher schließlich (Manfred Pichler) wagt sich in das eisige Wasser
|
für die Taucher gesichert und ein Schlauchboot zu Wasser
|
||||||
(nur wenige Grad über Null) des Quelltopfes und entschwindet tief
|
gelassen. Das boot ist für den Techniker gedacht, der mit dem
|
||||||
unterhalb der Betrachter dem Licht der Scheinwerfer. Reporter und
|
Taucher über ein Kabel verbunden ist und sogar mit ihm
|
||||||
Begleitmannschaft starren gebannt in den bereits nebligen Höhlenraum,
|
sprechen kann. Ein Taucher schließlich (Manfred Pichler) wagt
|
||||||
in dem der fast kreisrunde Höhlensee - Durchmesser etwa 20 Meter -
|
sich in das eisige Wasser (nur wenige Grad über Null) des
|
||||||
liegt. Ursprünglich hätten die Gespräche des Tauchers mit dem
|
Quelltopfes und entschwindet tief unterhalb der Betrachter dem
|
||||||
Techniker mittels Verstärker und Lautsprecher für alle hörbar
|
Licht der Scheinwerfer. Reporter und Begleitmannschaft starren
|
||||||
gemacht werden sollen, doch irgend ein technisches Gebrechen hat das
|
gebannt in den bereits nebligen Höhlenraum, in dem der fast
|
||||||
verhindert. Der Quelltopf wird bis auf einen Tiefe von 20 Meter erforscht.
|
kreisrunde Höhlensee - Durchmesser etwa 20 Meter - liegt.
|
||||||
Auch einige Fortsetzungen bestehen, doch wegen der starken
|
Ursprünglich hätten die Gespräche des Tauchers mit
|
||||||
Wassertrübung ist es nicht möglich, weiter als ein paar Meter in
|
dem Techniker mittels Verstärker und Lautsprecher für
|
||||||
sie vorzudringen.
|
alle hörbar gemacht werden sollen, doch irgend ein technisches
|
||||||
|
Gebrechen hat das verhindert. Der Quelltopf wird bis auf einen
|
||||||
<p>H.Segl und R.Seebacher nützen die Zeit während des Tauchganges,
|
Tiefe von 20 Meter erforscht. Auch einige Fortsetzungen bestehen,
|
||||||
um am gegenüberliegenden Ufer des Quelltopfes Fortsetzungen zu erkunden
|
doch wegen der starken Wassertrübung ist es nicht
|
||||||
und gelangen nach überwindung einer ca. 10 Meter hohen Wandstufe erneut
|
möglich, weiter als ein paar Meter in sie vorzudringen.</p>
|
||||||
in einen Höhlenraum, der mit Wasser erfüllt ist und mit dem
|
<p>H.Segl und R.Seebacher nützen die Zeit während des
|
||||||
großen See in Verbindung steht. Eine weitere Fortsetzung kann nicht
|
Tauchganges, um am gegenüberliegenden Ufer des Quelltopfes
|
||||||
erkundet werden.
|
Fortsetzungen zu erkunden und gelangen nach überwindung einer
|
||||||
|
ca. 10 Meter hohen Wandstufe erneut in einen Höhlenraum, der
|
||||||
<p>Nach Ende des Tauchganges klettert der Taucher, zitternd vor Kälte,
|
mit Wasser erfüllt ist und mit dem großen See in
|
||||||
mit letzter Kraft über die Drahtseilleiter aus dem Dom zurück.
|
Verbindung steht. Eine weitere Fortsetzung kann nicht erkundet
|
||||||
Nachdem einige (übliche) Reporterfragen beantwortet sind, tritt die
|
werden.</p>
|
||||||
Mannschaft, die stundenlang mit nassen Füßen ausgeharrt hatte,
|
<p>Nach Ende des Tauchganges klettert der Taucher, zitternd vor
|
||||||
den Rückweg an und erreicht (der Siphon hatte sich nicht wieder
|
Kälte, mit letzter Kraft über die Drahtseilleiter aus dem
|
||||||
aufgefüllt) neun Stunden nach dem Einstieg in die Höhle das
|
Dom zurück. Nachdem einige (übliche) Reporterfragen
|
||||||
Tageslicht.
|
beantwortet sind, tritt die Mannschaft, die stundenlang mit nassen
|
||||||
|
Füßen ausgeharrt hatte, den Rückweg an und erreicht
|
||||||
<p>Minuten später entlädt sich über der Seewiese ein heftiges
|
(der Siphon hatte sich nicht wieder aufgefüllt) neun Stunden
|
||||||
Gewitter mit wolkenbruchartigen Regenfällen, und alles, was bis zu
|
nach dem Einstieg in die Höhle das Tageslicht.</p>
|
||||||
diesem Zeitpunkt noch einigermaßen trocken ist, wird vom
|
<p>Minuten später entlädt sich über der Seewiese ein
|
||||||
strömenden Regen durchnäßt. Dank der Altausseer
|
heftiges Gewitter mit wolkenbruchartigen Regenfällen, und
|
||||||
Wasserrettung funktioniert der Rücktransport klaglos, und
|
alles, was bis zu diesem Zeitpunkt noch einigermaßen trocken
|
||||||
anschließend treffen sich die Mitglieder unseres Vereines zu einem
|
ist, wird vom strömenden Regen durchnäßt. Dank der
|
||||||
wohlverdienten Abendessen in einem Altauseer Gasthof.
|
Altausseer Wasserrettung funktioniert der Rücktransport
|
||||||
|
klaglos, und anschließend treffen sich die Mitglieder unseres
|
||||||
<p>Einige Tage später wird in der Fernsehsendung "österreich
|
Vereines zu einem wohlverdienten Abendessen in einem Altauseer
|
||||||
heute" ein lächerlicher Drei-Minuten-Bericht (!) über diese
|
Gasthof.</p>
|
||||||
spektakuläre Neun-Stunden-Expedition ausgestrahlt. über Reportagen
|
<p>Einige Tage später wird in der Fernsehsendung
|
||||||
anderer Art ist der Redaktion der "Mitteilungen" bisher nichts bekannt.
|
"österreich heute" ein lächerlicher Drei-Minuten-Bericht
|
||||||
|
(!) über diese spektakuläre Neun-Stunden-Expedition
|
||||||
<p>Liste der beteiligten Personen:
|
ausgestrahlt. über Reportagen anderer Art ist der Redaktion
|
||||||
|
der "Mitteilungen" bisher nichts bekannt.</p>
|
||||||
|
<p>Liste der beteiligten Personen:</p>
|
||||||
<ul>
|
<ul>
|
||||||
<li> Verein für Höhlenkunde in Obersteier
|
<li>Verein für Höhlenkunde in Obersteier
|
||||||
<ul><li>Alois Deubelli (Taucher)
|
<ul>
|
||||||
<li>Günter Pichler (Taucher)
|
<li>Alois Deubelli (Taucher)</li>
|
||||||
<li>Manfred Pichler (Taucher)
|
<li>Günter Pichler (Taucher)</li>
|
||||||
<li>Karl Gaisberger
|
<li>Manfred Pichler (Taucher)</li>
|
||||||
<li>Gottfried Geweßler
|
<li>Karl Gaisberger</li>
|
||||||
<li>Rudolf Mascha
|
<li>Gottfried Geweßler</li>
|
||||||
<li>Robert Seebacher
|
<li>Rudolf Mascha</li>
|
||||||
<li>Hans Segl
|
<li>Robert Seebacher</li>
|
||||||
<li>Sepp Steinberger
|
<li>Hans Segl</li>
|
||||||
|
<li>Sepp Steinberger</li>
|
||||||
</ul>
|
</ul>
|
||||||
<li>ORF-Fernsehen (3 Mann)
|
</li>
|
||||||
<li>Bayrischer Rundfunk (1 Mann)
|
<li>ORF-Fernsehen (3 Mann)</li>
|
||||||
<li>Tauchschule Zauner/Hallstatt (2 Mann)
|
<li>Bayrischer Rundfunk (1 Mann)</li>
|
||||||
|
<li>Tauchschule Zauner/Hallstatt (2 Mann)</li>
|
||||||
</ul>
|
</ul>
|
||||||
<hr />
|
<hr />
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<p lang=en>
|
<p lang="en" xml:lang="en"> </p>
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="../../noinfo/aaussee/1.htm">Cave description</a></li>
|
<li><a href="../../noinfo/aaussee/1.htm">Cave description</a></li>
|
||||||
<li><a href="../../aaussee/index.htm">Area description</a></li>
|
<li><a href="../../aaussee/index.htm">Area description</a></li>
|
||||||
<li><a href="../../areas.htm">Other Areas</a></li>
|
<li><a href="../../areas.htm">Other Areas</a></li>
|
||||||
<li><a href="../../index.htm">Back to Expedition Intro page</a>
|
<li><a href="../../index.htm">Back to Expedition Intro
|
||||||
|
page</a></li>
|
||||||
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
||||||
<li><a href="../index.htm">Other groups</a> who have worked in the area
|
<li><a href="../index.htm">Other groups</a> who have worked in the
|
||||||
|
area</li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
</html>
|
</html>
|
||||||
|
|||||||
@@ -1,72 +1,74 @@
|
|||||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
|
||||||
<html lang=de-at>
|
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
||||||
|
<html lang="de-at" xmlns="http://www.w3.org/1999/xhtml" xml:lang=
|
||||||
|
"de-at">
|
||||||
<head>
|
<head>
|
||||||
<title lang=en>1623-1: dive 1988</title>
|
<meta http-equiv="Content-Type" content=
|
||||||
<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
|
"text/html; charset=iso-8859-1" />
|
||||||
|
<title lang="en" xml:lang="en">1623-1: dive 1988</title>
|
||||||
|
<link rel="stylesheet" type="text/css" href=
|
||||||
|
"../../css/main2.css" />
|
||||||
</head>
|
</head>
|
||||||
<body>
|
<body>
|
||||||
<h2>BERICHT ÜBER TAUCHGÄNGE IN DER LIAGER-HÖHLE (1623/1 a-b) IM SEPTEMBER 1988</h2>
|
<h1>BERICHT ÜBER TAUCHGÄNGE IN DER LIAGER-HÖHLE
|
||||||
|
(1623/1 a-b) IM SEPTEMBER 1988</h1>
|
||||||
<p>Lieber Leser !
|
<p>Lieber Leser !</p>
|
||||||
|
<p>Die Liager Höhle bei Altaussee mit ihren Siphonen und dem
|
||||||
<p>Die Liager Höhle bei Altaussee mit ihren Siphonen und dem Quelltopf
|
Quelltopf hat schon in den sechziger Jahren Höhlentaucher in
|
||||||
hat schon in den sechziger Jahren Höhlentaucher in ihren Bann gezogen.
|
ihren Bann gezogen. Berühmte Namen wie Hasenmayr und Matz
|
||||||
Berühmte Namen wie Hasenmayr und Matz scheinen in der Forschungschronik
|
scheinen in der Forschungschronik auf. Auch Mitglieder des Vereines
|
||||||
auf. Auch Mitglieder des Vereines fü Höhlenkunde in Obersteier (M.
|
fü Höhlenkunde in Obersteier (M. und G. Pichler, A.
|
||||||
und G. Pichler, A. Deubelli) unternahmen 1984 einen neunstündigen
|
Deubelli) unternahmen 1984 einen neunstündigen
|
||||||
Tauchvorstoß, der jedoch trotz eines geqaltigen Aufgebotes an Material
|
Tauchvorstoß, der jedoch trotz eines geqaltigen Aufgebotes an
|
||||||
und - vor allem - Presseleuten außer einem dreiminütigen ORF
|
Material und - vor allem - Presseleuten außer einem
|
||||||
Fernseh-Spot(t) keine Ergebnisse brachte (Siehe Mitteilungen 1985, 2. Folge).
|
dreiminütigen ORF Fernseh-Spot(t) keine Ergebnisse brachte
|
||||||
|
(Siehe Mitteilungen 1985, 2. Folge).</p>
|
||||||
<p>Als sich im Frühjar 1988 eine Höhlentauchergruppe aus Heidelberg
|
<p>Als sich im Frühjar 1988 eine Höhlentauchergruppe aus
|
||||||
bei unserem Katasterwart meldete, waren wir angesichts der tragischen
|
Heidelberg bei unserem Katasterwart meldete, waren wir angesichts
|
||||||
Ereignisse im Pießling Ursprung über deren Vorhaben nicht
|
der tragischen Ereignisse im Pießling Ursprung über
|
||||||
Hocherfreut, obgleich es sicher jeden von uns interessiert, ob und wie es
|
deren Vorhaben nicht Hocherfreut, obgleich es sicher jeden von uns
|
||||||
hinter dem See "weitergeht".
|
interessiert, ob und wie es hinter dem See "weitergeht".</p>
|
||||||
|
<p>Die Sorgfalt der Berichterstattung war schließlich
|
||||||
<p>Die Sorgfalt der Berichterstattung war schließlich ausschlaggebend
|
ausschlaggebend dafür, daß der Bericht ungekürzt
|
||||||
dafür, daß der Bericht ungekürzt abgedrukt wurde.
|
abgedrukt wurde.</p>
|
||||||
|
<p style="text-align: right"><i>Die Redaktion.</i></p>
|
||||||
<p align=right>Die Redaktion.
|
<p>Vorbereitungen:</p>
|
||||||
|
<p>Als die Wettervorhersage, nach einer Woche Regen, für die
|
||||||
<p>Vorbereitungen:
|
kommeden Tage relativ gut ausfiel, entschlossen wir uns, die
|
||||||
|
Befahrung der Liager Höhle in Angriff zu nehmen.</p>
|
||||||
<p>Als die Wettervorhersage, nach einer Woche Regen, für die kommeden
|
<p>Von der letzten Parkmöglichkeit in Altaussee aus
|
||||||
Tage relativ gut ausfiel, entschlossen wir uns, die Befahrung der Liager
|
transportierten wir under Gepäck 8.9.1988 auf alten
|
||||||
Höhle in Angriff zu nehmen.
|
Kinderwagen den Uferweg des Altausseer Sees entlang zur Seewiese.
|
||||||
|
Eine Tour dauerte etwa 1.5 Stunden. Nach 6 Stunden hatten wir das
|
||||||
<p>Von der letzten Parkmöglichkeit in Altaussee aus transportierten wir
|
für die Befahrung nötige Material, sowie Verpflegung und
|
||||||
under Gepäck 8.9.1988 auf alten Kinderwagen den Uferweg des Altausseer
|
und Schlafsäcke etc. in diw Nähe der Höhle
|
||||||
Sees entlang zur Seewiese. Eine Tour dauerte etwa 1.5 Stunden. Nach 6 Stunden
|
transportiert.</p>
|
||||||
hatten wir das für die Befahrung nötige Material, sowie Verpflegung
|
<p>Nach dem Abendbrot schleppten Achim, Bettina und ich noch eben
|
||||||
und und Schlafsäcke etc. in diw Nähe der Höhle transportiert.
|
vier 41 und zwei 71 Pressluftflaschen die Steilwand zum Liagern
|
||||||
|
hinauf.</p>
|
||||||
<p>Nach dem Abendbrot schleppten Achim, Bettina und ich noch eben vier 41 und
|
<p>Die 41 Pressluftflaschen sollten in den nächsten Tagen dazu
|
||||||
zwei 71 Pressluftflaschen die Steilwand zum Liagern hinauf.
|
dienen, den Siphon im westlichen Wassergang zu durchtauchen.</p>
|
||||||
|
<p>Sie blieben immer auf der jeweiligen Seite direkt am Siphon
|
||||||
<p>Die 41 Pressluftflaschen sollten in den nächsten Tagen dazu dienen,
|
liegen.</p>
|
||||||
den Siphon im westlichen Wassergang zu durchtauchen.
|
<p>Die 71 Flaschen sollten am See zu einem Doppelgerät
|
||||||
|
zusammengebaut werden, um damit den See unter Wasser zu
|
||||||
<p>Sie blieben immer auf der jeweiligen Seite direkt am Siphon liegen.
|
erforschen.</p>
|
||||||
|
<p lang="en" xml:lang="en">[that's the first page...]</p>
|
||||||
<p>Die 71 Flaschen sollten am See zu einem Doppelgerät zusammengebaut
|
<p lang="en" xml:lang="en">A follow up article by Achim Bayer,
|
||||||
werden, um damit den See unter Wasser zu erforschen.
|
Michael Meyberg and Bettina Rinne in <i lang="de" xml:lang=
|
||||||
|
"de">(Mitteilungen des Vereines für Höhlenkunde in
|
||||||
<p lang=en>[that's the first page...]
|
Obersteier 7(2) 1988 pp 39-45)</i> is waiting to be typed in :-)
|
||||||
|
<!-- LINKS --></p>
|
||||||
<p lang=en>A follow up article by Achim Bayer, Michael Meyberg and Bettina
|
<p lang="en" xml:lang="en"> </p>
|
||||||
Rinne in <i lang=de>(Mitteilungen des Vereines für Höhlenkunde in
|
|
||||||
Obersteier 7(2) 1988 pp 39-45)</i> is waiting to be typed in :-)
|
|
||||||
|
|
||||||
<!-- LINKS -->
|
|
||||||
<p lang=en>
|
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="../../noinfo/aaussee/1.htm">Cave description</a></li>
|
<li><a href="../../noinfo/aaussee/1.htm">Cave description</a></li>
|
||||||
<li><a href="../../aaussee/index.htm">Area description</a></li>
|
<li><a href="../../aaussee/index.htm">Area description</a></li>
|
||||||
<li><a href="../../areas.htm">Other Areas</a></li>
|
<li><a href="../../areas.htm">Other Areas</a></li>
|
||||||
<li><a href="../../index.htm">Back to Expedition Intro page</a>
|
<li><a href="../../index.htm">Back to Expedition Intro
|
||||||
|
page</a></li>
|
||||||
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
||||||
<li><a href="../index.htm">Other groups</a> who have worked in the area
|
<li><a href="../index.htm">Other groups</a> who have worked in the
|
||||||
|
area</li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
</html>
|
</html>
|
||||||
|
|||||||
@@ -1,70 +1,77 @@
|
|||||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
|
||||||
<html>
|
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
||||||
|
<html xmlns="http://www.w3.org/1999/xhtml">
|
||||||
<head>
|
<head>
|
||||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
<meta name="generator" content=
|
||||||
|
"HTML Tidy for Linux/x86 (vers 1st March 2004), see www.w3.org" />
|
||||||
|
<meta http-equiv="Content-Type" content=
|
||||||
|
"text/html; charset=iso-8859-1" />
|
||||||
<title>UBSS</title>
|
<title>UBSS</title>
|
||||||
<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
|
<link rel="stylesheet" type="text/css" href=
|
||||||
|
"../../css/main2.css" />
|
||||||
</head>
|
</head>
|
||||||
<body>
|
<body>
|
||||||
<center><h2>University of Bristol Speleological Society</h2></center>
|
<h1>University of Bristol Speleological Society</h1>
|
||||||
|
|
||||||
The UBSS is the oldest of the existing British University caving clubs.
|
|
||||||
Most famous for its work in the caves of County Clare, and also much
|
|
||||||
involved in Mendip caving, the UBSS also venture further afield.
|
|
||||||
|
|
||||||
<p>Steve Perry (once dubbed "the fittest man on Mendip") was a CUCC member
|
|
||||||
with UBSS connections, who was on the 1977 expedition. Other UBSS members
|
|
||||||
first joined CUCC's Austria expedition as guests in 1980, and UBSS was a
|
|
||||||
"guest club" on the CUCC expedition in both 1981 and 1982, after which their
|
|
||||||
involvement declined. The work done by UBSS members was written up in the
|
|
||||||
prestigious Proceedings of UBSS.
|
|
||||||
<p>Sadly we have been asked to remove these pieces
|
|
||||||
of documentation, which are relevant to CUCCs exploration of the area. We are currently
|
|
||||||
trying to contact the orginal authors of the articles to ask for their
|
|
||||||
permission to publish the articles.</p>
|
|
||||||
|
|
||||||
|
<p>The UBSS is the oldest of the existing British University caving
|
||||||
|
clubs. Most famous for its work in the caves of County Clare, and
|
||||||
|
also much involved in Mendip caving, the UBSS also venture further
|
||||||
|
afield.</p>
|
||||||
|
<p>Steve Perry (once dubbed "the fittest man on Mendip") was a CUCC
|
||||||
|
member with UBSS connections, who was on the 1977 expedition. Other
|
||||||
|
UBSS members first joined CUCC's Austria expedition as guests in
|
||||||
|
1980, and UBSS was a "guest club" on the CUCC expedition in both
|
||||||
|
1981 and 1982, after which their involvement declined. The work
|
||||||
|
done by UBSS members was written up in the prestigious Proceedings
|
||||||
|
of UBSS.</p>
|
||||||
|
<p>Sadly we have been asked to remove these pieces of
|
||||||
|
documentation, which are relevant to CUCCs exploration of the area.
|
||||||
|
We are currently trying to contact the orginal authors of the
|
||||||
|
articles to ask for their permission to publish the articles.</p>
|
||||||
<dl>
|
<dl>
|
||||||
<dt><!-- a href="811427.htm" -->81.1427<dd>
|
<dt><!-- a href="811427.htm" -->81.1427</dt>
|
||||||
<cite>Proceedings of the University of Bristol Speleological Society 16(1)
|
<dd><cite>Proceedings of the University of Bristol Speleological
|
||||||
(1981) pp 5-10</cite>, <b>An introduction to Austrian karst</b>, Steve Perry
|
Society 16(1) (1981) pp 5-10</cite>, <b>An introduction to Austrian
|
||||||
|
karst</b>, Steve Perry</dd>
|
||||||
<dt><!-- a href="811309.htm" -->81.1309<dd>
|
<dt><!-- a href="811309.htm" -->81.1309</dt>
|
||||||
<cite>Proceedings of the University of Bristol Speleological Society 16(1)
|
<dd><cite>Proceedings of the University of Bristol Speleological
|
||||||
(1981) pp 11-20</cite>, <b>A description of some caves...</b>, Julian
|
Society 16(1) (1981) pp 11-20</cite>, <b>A description of some
|
||||||
Griffiths
|
caves...</b>, Julian Griffiths</dd>
|
||||||
|
<dt><!-- a href="831621.htm" -->83.1621</dt>
|
||||||
<dt><!-- a href="831621.htm" -->83.1621<dd>
|
<dd><cite>Proceedings of the University of Bristol Speleological
|
||||||
<cite>Proceedings of the University of Bristol Speleological Society 16(2)
|
Society 16(2) (Nov 1982) pp 77-83</cite>, <b>The
|
||||||
(Nov 1982) pp 77-83</cite>, <b>The Stellerweghöhle system, Totes
|
Stellerweghöhle system, Totes Gebirge, Austria</b>, Rich
|
||||||
Gebirge, Austria</b>, Rich Barker et al
|
Barker et al</dd>
|
||||||
|
|
||||||
</dl>
|
</dl>
|
||||||
|
|
||||||
<hr />
|
<hr />
|
||||||
|
<p>Unknown to CUCC (and very much to our embarassment in 1989), a
|
||||||
<p>Unknown to CUCC (and very much to our embarassment in 1989), a few UBSS
|
few UBSS members staged independent expeditions to an area north of
|
||||||
members staged independent expeditions to an area north of the plateau. We
|
the plateau. We believe there were two trips (in 1989 and 1990),
|
||||||
believe there were two trips (in 1989 and 1990), though information is still
|
though information is still hard to come by, as the whole thing was
|
||||||
hard to come by, as the whole thing was clandestine. The local Austrian
|
clandestine. The local Austrian cavers found it hard to believe
|
||||||
cavers found it hard to believe that CUCC had no knowledge of the trips
|
that CUCC had no knowledge of the trips whilst CUCC found it hard
|
||||||
whilst CUCC found it hard to believe that no-one at the BCRA Conference would
|
to believe that no-one at the BCRA Conference would admit to being
|
||||||
admit to being with the "English group camped on Augst-Eck" found by the
|
with the "English group camped on Augst-Eck" found by the
|
||||||
helicopter during Becka's 1989 rescue. This upset an already delicate
|
helicopter during Becka's 1989 rescue. This upset an already
|
||||||
political situation, with the risk that all English groups might be banned
|
delicate political situation, with the risk that all English groups
|
||||||
from the area permanently. It would appear that the officers and committee
|
might be banned from the area permanently. It would appear that the
|
||||||
of the UBSS itself were unaware that their members were visiting the area
|
officers and committee of the UBSS itself were unaware that their
|
||||||
without permission and had not bothered to research the political situation
|
members were visiting the area without permission and had not
|
||||||
before giving grant money for the trip.
|
bothered to research the political situation before giving grant
|
||||||
|
money for the trip.</p>
|
||||||
<hr />
|
<hr />
|
||||||
<!-- LINKS -->
|
<!-- LINKS -->
|
||||||
<ul>
|
<ul>
|
||||||
<li><a href="../../indxal.htm">Index</a> of all caves documented in 1623.</li>
|
<li><a href="../../indxal.htm">Index</a> of all caves documented in
|
||||||
|
1623.</li>
|
||||||
<li><a href="../../areas.htm">Overview</a> of area 1623</li>
|
<li><a href="../../areas.htm">Overview</a> of area 1623</li>
|
||||||
<li><a href="../../1626/index.htm">Overview</a>
|
<li><a href="../../1626/index.htm">Overview</a> of area 1626, and
|
||||||
of area 1626, and index to caves</li>
|
index to caves</li>
|
||||||
<li>Back to <a href="../../index.htm">Expedition Intro page</a></li>
|
<li>Back to <a href="../../index.htm">Expedition Intro
|
||||||
|
page</a></li>
|
||||||
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
||||||
<li><a href="../index.htm">Other groups</a> who have worked in the area
|
<li><a href="../index.htm">Other groups</a> who have worked in the
|
||||||
|
area</li>
|
||||||
</ul>
|
</ul>
|
||||||
</body>
|
</body>
|
||||||
</html>
|
</html>
|
||||||
|
|||||||
@@ -1,45 +1,50 @@
|
|||||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
|
||||||
<html>
|
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
|
||||||
|
<html xmlns="http://www.w3.org/1999/xhtml">
|
||||||
<head>
|
<head>
|
||||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
<meta name="generator" content=
|
||||||
|
"HTML Tidy for Linux/x86 (vers 1st March 2004), see www.w3.org" />
|
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|
<meta http-equiv="Content-Type" content=
|
||||||
|
"text/html; charset=iso-8859-1" />
|
||||||
<title>ULSA</title>
|
<title>ULSA</title>
|
||||||
<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
|
<link rel="stylesheet" type="text/css" href=
|
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<center><h2>University of Leeds Speleological Association</h2></center>
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<h1>University of Leeds Speleological Association</h1>
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<p>ULSA is one of the bigger and more active of the UK's University
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<p>ULSA is one of the bigger and more active of the UK's University caving
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caving organisations, and incorporates the (strictly undergraduate)
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organisations, and incorporates the (strictly undergraduate) Leeds University
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Leeds University Union Speleological Society. Most famous for the
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Union Speleological Society. Most famous for the large amount of new
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large amount of new exploration arising out of an ambitious program
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exploration arising out of an ambitious program to resurvey many of
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to resurvey many of Yorkshire's significant caves in the 1960's,
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Yorkshire's significant caves in the 1960's, the club has continued to find
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the club has continued to find and survey new cave at home and
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and survey new cave at home and abroad. The club also has a deserved
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abroad. The club also has a deserved reputation for high quality
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reputation for high quality publication.
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publication.</p>
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<p>Encouraged by contact with Gunther Graf, ULSA visited the
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<p>Encouraged by contact with Gunther Graf, ULSA visited the Tauplitz area
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Tauplitz area (east of CUCC's area) in the early eighties. A great
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(east of CUCC's area) in the early eighties. A great deal of shaft bashing
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deal of shaft bashing was done, but none of the small
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was done, but none of the small sub-horizontal draughting entrances which are
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sub-horizontal draughting entrances which are the most promising on
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the most promising on Loser were investigated. The expedition high camp was
|
Loser were investigated. The expedition high camp was flattened by
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flattened by a snow storm, and a degree of demoralisation set in. The trip
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a snow storm, and a degree of demoralisation set in. The trip was
|
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was written up in <b>ULSA Review 16</b> (CTS ref. 86.1980), but no return
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written up in <b>ULSA Review 16</b> (CTS ref. 86.1980), but no
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trip ever took place.
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return trip ever took place.</p>
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<p>ULSA has its <a href=
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<p>ULSA has its
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"http://www.leeds.ac.uk/union/socs/speleological/home.htm">own
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<a href="http://www.leeds.ac.uk/union/socs/speleological/home.htm">own
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website</a>, upon which old publications are being put as and when
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website</a>, upon which old publications are being put as and when they
|
they go out of print.</p>
|
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go out of print.
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<hr />
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<hr />
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<!-- LINKS -->
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<!-- LINKS -->
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<ul>
|
<ul>
|
||||||
<li><a href="../../indxal.htm">Index</a> of all caves documented in 1623.</li>
|
<li><a href="../../indxal.htm">Index</a> of all caves documented in
|
||||||
|
1623.</li>
|
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<li><a href="../../areas.htm">Overview</a> of area 1623</li>
|
<li><a href="../../areas.htm">Overview</a> of area 1623</li>
|
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<li><a href="../../1626/index.htm">Overview</a>
|
<li><a href="../../1626/index.htm">Overview</a> of area 1626, and
|
||||||
of area 1626, and index to caves</li>
|
index to caves</li>
|
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<li>Back to <a href="../../index.htm">Expedition Intro page</a></li>
|
<li>Back to <a href="../../index.htm">Expedition Intro
|
||||||
|
page</a></li>
|
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<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
<li><a href="../../../index.htm">Back to CUCC Home page</a></li>
|
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<li><a href="../index.htm">Other groups</a> who have worked in the area
|
<li><a href="../index.htm">Other groups</a> who have worked in the
|
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|
area</li>
|
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</ul>
|
</ul>
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</body>
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</html>
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Reference in New Issue
Block a user