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<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
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<html lang="en">
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<head><title>1626:117</title><link rel="stylesheet" type="text/css" href="../../css/main2.css" />
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<html>
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<head><meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
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</head>
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<body>
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<center><table border=0 width=100%>
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<head><meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
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<title>1626:120</title><link rel="stylesheet" type="text/css" href="../../css/main2.css" />
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</head>
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<body>
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<center><table border=0 width=100%>
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<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
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<html lang="en">
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<html>
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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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<title>1626:122</title>
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<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
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<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
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<html lang=en>
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<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN" "http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
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<html>
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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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<title>1626:5</title>
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<META name="ROBOTS" content="NOINDEX">
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<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
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</head>
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<body>
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<center><table border=0 width=100%>
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<tr><th align=left><font size=+2>5</font></th>
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<th align=center lang=de><font size=+2>Nagelsteghöhle</font></th>
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<th align=right><font size=+2>2/W +</font></th></tr>
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</table></center>
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<table id="cavepage">
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<tr><th id="kat_no">5</th><th id="name">Nagelsteghöhle</th><th id="status">2/W +</th></tr>
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</table>
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<p><b>Altitude</b>: 865m<br>
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<p><b>Altitude</b>: 865m</p>
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<b>Location</b>: Above Rettenbachtal (north side); about 20-25 minutes
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on foot from Blaa-Alm.
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<p><b>Location</b>: Above Rettenbachtal (north side); about 20-25 minutes on
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foot from Blaa-Alm.</p>
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<p>A resurgence cave of major importance, visited by CUCC in 1976 and 2002.
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Krenmayr gives it 278m long, seasonally active, very roomy water cave. The
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associated perennial resurgence is Naglbrünndl, putting out 50-100 l/s.
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associated perennial resurgence is Naglbrünndl, putting out 50-100
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l/s.</p>
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<p>Continue past the Blaa-Alm
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hostelry on the track to a crossroads of paths. Take the path to the right and
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then bear downhill and to the left at a fork by a small wooden hut.
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Follow the track until you end up walking parallel to the river; keep a
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lookout on the right for a small bridge across the river. Cross the bridge
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and take a small path to the left, which arrives at a further (smaller!)
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bridge over a stream. Just before the bridge, ascend up the hillside to
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the right through the undergrowth, keeping the large rocky gully to your
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right and the stream to your left. After a few minutes you will arrive
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at the resurgence (under tree-roots) to the left. At this point, cross
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into the gully on the right and climb up to the very top to reach the
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cave.
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<p>Continue past the Blaa-Alm hostelry on the track to a crossroads of paths.
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Take the path to the right and then bear downhill and to the left at a fork by
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a small wooden hut. Follow the track until you end up walking parallel to the
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river; keep a lookout on the right for a small bridge across the river. Cross
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the bridge and take a small path to the left, which arrives at a further
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(smaller!) bridge over a stream. Just before the bridge, ascend up the
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hillside to the right through the undergrowth, keeping the large rocky gully to
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your right and the stream to your left. After a few minutes you will arrive at
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the resurgence (under tree-roots) to the left. At this point, cross into the
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gully on the right and climb up to the very top to reach the cave.</p>
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<p>Entrance is at the head of a large, steeply-inclined stream bed (carries
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major flow in flood), and is reminiscent of Sleets Gill. A short climb
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@ -41,21 +38,22 @@ major flow in flood), and is reminiscent of Sleets Gill. A short climb
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to a short greasy climb. One soon emerges in the huge main passage, floored at
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the lower end by vast amounts of very unpleasant mud. The sump is reached by a
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right turn over some fine stratified sand, but CUCC's interest lay in some
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holes in the roof at the top end, with the hope of a high-level continuation.
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holes in the roof at the top end, with the hope of a high-level
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continuation.</p>
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<p>The mud eventually runs out to be replaced by more and more inclined
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slabs, which were very easy on the way up. The gradient steadily increases
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until the floor merges into the end wall, and the trickle of water enters
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from high up. At this point, a couple of holes in the roof have already
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been passed, but investigation revealed these to be beyond reasonable
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reach without some fairly serious bolting.
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<p>The mud eventually runs out to be replaced by more and more inclined slabs,
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which were very easy on the way up. The gradient steadily increases until the
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floor merges into the end wall, and the trickle of water enters from high up.
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At this point, a couple of holes in the roof have already been passed, but
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investigation revealed these to be beyond reasonable reach without some fairly
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serious bolting.</p>
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<p><b>Exploration</b>: LVHK Oberösterreich, 1972
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<p><b>Exploration</b>: LVHK Oberösterreich, 1972</p>
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<hr />
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<!-- LINKS -->
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<ul>
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<li><a href="../../1626/index.htm#id5">Index</a> and overview of 1626.</li>
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<li><a href="../../areas.htm">Overview</a> of area 1623<br>
|
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<li><a href="../../areas.htm">Overview</a> of area 1623</li>
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<!-- need link to LVHKO intro page - not yet written -->
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<li><a href="../../index.htm">Back to Expedition Intro page</a></li>
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<li><a href="../../../index.htm">CUCC Home page</a></li>
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|
@ -1,22 +1,21 @@
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<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
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<html lang="en">
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<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN" "http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd">
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<html>
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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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<title>1626:50</title>
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<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
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</head>
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<body>
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||||
<center><table border=0 width=100%>
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<tr><th align=left><font size=+2>50</font></th>
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<th align=center lang="de"><font size=+2>Ahnenschacht</font></th>
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<th align=right><font size=+2>3/S/T</font></th></tr>
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</table></center>
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<table id="cavepage">
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<tr><th id="kat_no">50</th><th id="name">Ahnenschacht</th><th id="status">3/S/T</th></tr>
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</table>
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<p><b>Altitude</b>: 1890m<br>
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<p><b>Altitude</b>: 1890m<br />
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<span lang="de">Frigoschacht</span> 1875m (enters at -130m at
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<span lang="de">Sinterterrasse)</span><br>
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<b>Location</b>: NW of <span lang="de">Wehrkogel</span> on the
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<span lang="de">Sinterterrasse)</span></p>
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<p><b>Location</b>: NW of <span lang="de">Wehrkogel</span> on the
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<span lang="de">Schönberg.</span> Marked and named on OAV map sheet
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15/1.
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15/1.</p>
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<h3>Entrance series</h3>
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@ -25,10 +24,10 @@
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cave starts with four pitches (p14, p11, p5 and p11) which drop onto a slope
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formed of big boulders (rope desirable). After this, another series of small
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pitches (p9, p7, p6, p4, p10, p18, p11) from which is reached the
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<span lang="de">Sinterterrasse</span> at -141m.
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<span lang="de">Sinterterrasse</span> at -141m.</p>
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<p>From this point, one has left the zone of small pitches and started a
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series of pitches which in reality are part of a single shaft down to -400m.
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series of pitches which in reality are part of a single shaft down to -400m.</p>
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<p>Indeed, if you had an unfortunate accident on the
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<span lang="de">Sinterterrasse,</span> you would fall all the way to -400m.
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@ -41,7 +40,7 @@ Schacht</span> 100m. On the <span lang="de">Josef Schacht,</span> a pendulum
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Descending the <span lang="de">Josef Schacht</span> a little further, after a
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6.5m and a 10m pitch, access can be gained to a wide canyon, active in the
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bottom, and which ends in a fissure. This canyon is fossil in the upper level
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and certainly presents possibilities for continuation.
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and certainly presents possibilities for continuation.</p>
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<h3>Lateral development from <span lang="de">Josef Schacht</span></h3>
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@ -49,7 +48,7 @@ and certainly presents possibilities for continuation.
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enters the network proper. At this point is a passage covered in rather
|
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special formations. The first junction gives access to a network ...
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[unfortunately there are lines missing in my photocopy of
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<span lang="fr">Spéalp</span> 1]
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<span lang="fr">Spéalp</span> 1]</p>
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<h3>The Vegetable Garden</h3>
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@ -60,20 +59,20 @@ and a sloping passage with formations in the Mammoth pitch chamber. The
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system is composed of a big chamber with numerous passages and junctions; it
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is very poorly known and no doubt houses many surprises. Continuing along
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the passage, one passes a step of 4m to find a junction, to the left at
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which lies the bivouac.
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which lies the bivouac.</p>
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<h3>Belgica system</h3>
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<p>Directly after the bivouac, there is a 10m pitch, and at the bottom, a new
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junction: downhill the Belgica passage, of fairly small dimensions, which
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leads, after traversing past three holes, to a descent of an 8m and a 17m
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pitch and to the squeezes passed by our French colleagues.
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pitch and to the squeezes passed by our French colleagues.</p>
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<p>Uphill, discovered by D.Motte and PIE, in the course of the expedition in
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1974, is the <span lang="fr">Galerie de Francs Comtois.</span> This is a
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large ascending fossil passage interspersed with traverses, dips and pitches.
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It reascends to -90m. At -150m, a 20m pitch reaches the <span
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lang="fr">Résomega.</span>
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lang="fr">Résomega.</span></p>
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<p>A little before the 20m pitch, a short descending canyon passage avoids
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the 20m pitch and the series of squeezes following it. The <span
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@ -84,30 +83,30 @@ possibilities. A 60m pitch gives onto another 60m pitch which is undescended.
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There is another big pitch in excess of 100m and an unfinished ascending
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passage. A little before, a 10m pitch allows one to reach a passage
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interspersed with 3 junctions and 7 exits ! This shows the level of
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complexity which we ran into.
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complexity which we ran into.</p>
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<p>It was also at the <span lang="fr">Balcon du Visionnaire</span> that an
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accident occurred in 1975, which terminated exploration in that year.
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accident occurred in 1975, which terminated exploration in that year.</p>
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<p>Back in the Horizontal network, and after passing a little bouldery climb
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an inlet is encountered, named The Bath. The passage continues a little
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longer, to end in a pitch. [ exploration incomplete ]
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longer, to end in a pitch. [ exploration incomplete ]</p>
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<p>The following junction has been named Mammoth Junction because the
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passage to the right leads onto the pitch of the same name. It is necessary
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to exercise great care and attention not to slip hereabouts, because a fall
|
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would drop you into same.
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would drop you into same.</p>
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<p>The Mammoth Pitch, Para-pitch and probably the Negus pitch, form part of
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the same system (see survey) which is composed of a 146m pitch, a 10m
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pitch and a narrow canyon interspersed with several cascades leading finally
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to a 35m pitch giving onto the sump at -612m. The Para-pitch, p106, is
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followed by pitches of 5, 10 and 50m and drops via the latter into the
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Mammoth Canyon.
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Mammoth Canyon.</p>
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<p>The Negus pitch, which is undescended, should also drop into the same
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canyon. Several other small pitches and active streamways should also rejoin
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this system.
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this system.</p>
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<p>The depth of 612m should be treated cautiously because the method of
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survey used (based on the height of a man) is fairly imprecise. The bottom
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@ -116,11 +115,11 @@ from redoing our survey. [The depth quoted in <span lang="fr">Atlas des
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Grandes Gouffres</span> is -607m, which is shown as the bottom of this
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system. However, a Belgian survey shows the Yodl system (which is supposed to
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end at -607m) to be somewhere else entirely, so it is rather unclear which
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survey is wrong.]
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survey is wrong.]</p>
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<p>Turning left, the Zipfer passage is followed for 150m before reaching an
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important junction: to the left Chimneys passage, to the right Draughting
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passage.
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passage.</p>
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<h3>Chimneys Passage</h3>
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@ -131,7 +130,7 @@ pitch in which you must pendulum 5m from the bottom in order to reach a
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chamber in which is met a small stream. Climbing up a little opposite, a
|
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short upper passage rejoins the stream by a 20m pitch. In the chamber, the
|
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descent of a 10m pitch allows the stream to be followed to a squeeze beyond
|
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which one can hear the grumble of a large river ? A place to go back to.
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which one can hear the grumble of a large river ? A place to go back to.</p>
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<h3>Draughting passage</h3>
|
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@ -139,26 +138,26 @@ which one can hear the grumble of a large river ? A place to go back to.
|
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complex network which intersects itself in various places and which could
|
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hold very great surprises, since its exploration has only been sketchily
|
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outlined. The exit from this passage is in an area of boulders where two
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possibilities exist:
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possibilities exist:</p>
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<p><b>To the left</b>: a tight passage has been forced on a slope to
|
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<span lang="de">Kitschacht</span> (Tackle Bag Shaft) a magnificent 50m drop,
|
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very wide and completely free hanging. At its base, several possibilities. A
|
||||
tight active canyon which can be bypassed by a fossil passage, broken by an
|
||||
earthy drop of 3m to a huge 15m pitch leading to a sump at -360m.
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earthy drop of 3m to a huge 15m pitch leading to a sump at -360m.</p>
|
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|
||||
<p>A drop of a few metres gives access to a huge fossil passage (10
|
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× 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 vast wet
|
||||
pitch. Climbing over a big boulder on the right gives access to another pitch
|
||||
upwards.
|
||||
upwards.</p>
|
||||
|
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<p>Just after the base of <span lang="de">Kitschacht,</span> a passage of 80m
|
||||
makes a connection with the system of the
|
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<span lang="fr">Décollement</span> pitch at the bottom of the 40m
|
||||
shaft. A canyon leaving the junction passage can be followed for more than
|
||||
300m, and exits, in several places, into the side of the big fossil passage,
|
||||
just before the pitch upwards.
|
||||
just before the pitch upwards.</p>
|
||||
|
||||
<p><b>To the right</b>: The <span lang="fr">Décollement</span> pitch,
|
||||
with, at its base, a sloping chamber full of boulders. To the left a very
|
||||
@ -169,18 +168,18 @@ a wide pitch with an inlet. After this 15m pitch is a short canyon and a damp
|
||||
40m pitch. At the bottom, a huge descending passage suddenly turns almost
|
||||
vertical. This is the Toboggan, needing 20m of rope (a very spectacular
|
||||
passage). At this level one again cuts a new streamway. The passage
|
||||
continues, then contracts, and chokes at -385m.
|
||||
continues, then contracts, and chokes at -385m.</p>
|
||||
|
||||
<h3>Extensions to the Belgica system (various Belgians, June/July 1977)</h3>
|
||||
|
||||
<p><b>After the Bivouac</b>: a 10m pitch, then turn left into a small
|
||||
passage, ignore three pitches to the side, then descend pitches of 8 and 13m
|
||||
to arrive at some easy squeezes on the left. After this, a climb of 5m and a
|
||||
42m pitch. Stops in a sand blockage at -410m.
|
||||
42m pitch. Stops in a sand blockage at -410m.</p>
|
||||
|
||||
<p>Over the 13m pitch a small passage goes to several climbs in a fossil
|
||||
series. There is a 25m pitch and two 10m pitches ending in several very
|
||||
tight chimneys.
|
||||
tight chimneys.</p>
|
||||
|
||||
<h3>Yodl system (explored GSAB, August 1977)</h3>
|
||||
|
||||
@ -189,52 +188,73 @@ climb down 7m over a large block and descend about 12m in the bottom of a
|
||||
meander. Progress is then in the meander, with a short climb in a fault on
|
||||
the left and a 120m pitch, in sections of 22m and 100m. Beyond is a tight
|
||||
canyon with a 20m pitch to a sump at -607m (the last part of the 100m pitch
|
||||
is wet).
|
||||
is wet).</p>
|
||||
|
||||
<p><span lang="fr">Atlas des Grands Gouffres du Monde</span> 1979 says that
|
||||
the original -395m route goes on to c-470m (unsurveyed) and there are also
|
||||
routes ending at -385m and -386m.
|
||||
routes ending at -385m and -386m.</p>
|
||||
|
||||
<b>Exploration</b>: Discovered by Upper Austrians in 1856.<br>
|
||||
<p><b>Exploration</b>: Discovered by Upper Austrians in 1856.</p>
|
||||
|
||||
The point -320m was reached by them in 1958.<br>
|
||||
<p>The point -320m was reached by them in 1958.</p>
|
||||
|
||||
In 1967 and 1968 the <a href="../../others/bec/index.htm">Bristol Exploration
|
||||
<p>In 1967 and 1968 the <a href="../../others/bec/index.htm">Bristol Exploration
|
||||
Club</a> reached -395m, the Horizontal network, with a length of 1 km, was
|
||||
discovered.<br>
|
||||
discovered.</p>
|
||||
|
||||
In 1972, 73, 74 and 75, the GSAB <span lang="fr">"Les Gours"</span> explored
|
||||
<p>In 1972, 73, 74 and 75, the GSAB <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 clubs from
|
||||
Eastern France: <span lang="fr">S.C.Vesoul, G.S.Clerval &
|
||||
S.S.Daules.</span> In 1975 CARSS joined a mini-expedition in July and
|
||||
likewise, CASEO in August.<br>
|
||||
likewise, CASEO in August.</p>
|
||||
|
||||
A GSAB expedition in August 1977 connected a new entrance
|
||||
<p>A GSAB expedition in August 1977 connected a new entrance
|
||||
<span lang="de">(Frigoschacht)</span> at -130m, surveyed the Vegetable Garden
|
||||
and explored the new areas Yodl and KGB.
|
||||
and explored the new areas Yodl and KGB.</p>
|
||||
|
||||
<p><cite>Descent 176</cite> (Feb/Mar 2004) p18 states:</p>
|
||||
|
||||
<blockquote><p>
|
||||
Meanwhile, on the other side of the range, Upper Austrian cavers have
|
||||
undertaken some homework that others left behind a quarter of a century ago.
|
||||
<b>Ahnenschacht</b> (Ancestors' Shaft) was discovered in the 1950s and pushed
|
||||
to -395m. In the 1970s, Belgian cavers found vast horizontal passages amounting
|
||||
to about 5km in total – and a continuation to -602m. Their pushes came to
|
||||
an abrupt halt, however, when in 1975 a caver fractured his pelvis and had to
|
||||
be transported out of the cave. It was Austria's biggest cave rescue operation
|
||||
in the 20th century.</p>
|
||||
<p>Since documentation of the Belgian finds was fragmentary and of very poor
|
||||
quality, some members of the <span lang="de">Verein für Höhlenkunde
|
||||
in Oberösterreich</span> decided to fill in the gaps in the maps and
|
||||
resume surveying activities. So far, 1.7km have been accurately surveyed.</p>
|
||||
<div style="text-align: right">Correspondent: Theo Pfarr</div>
|
||||
</blockquote>
|
||||
|
||||
<p>(I fear attempting to reconcile the chronology of the above snippet with the
|
||||
information above is a hopeless task.)</p>
|
||||
|
||||
<p><b>References :</b>
|
||||
<dl>
|
||||
<dt>78.2012<dd><cite>(GSAB) <span lang="fr">Spéalp</span>
|
||||
<dt>78.2012</dt><dd><cite>(GSAB) <span lang="fr">Spéalp</span>
|
||||
1 (June 1977) pp 33-49</cite>, <b>Totes Gebirge :
|
||||
<span lang="fr">Description des principaux gouffres de la
|
||||
zone ouest du massif</span></b>,
|
||||
<span lang="fr">Jean Claude Hans & Etienne Degrave</span><br>
|
||||
<span lang="fr">Jean Claude Hans & Etienne Degrave</span><br />
|
||||
|
||||
<a href="../../others/gsab/en/782012.htm#id117">English Translation</a><br>
|
||||
<a href="../../others/gsab/fr/782012.htm#id117" lang="fr">En Français</a>
|
||||
<a href="../../others/gsab/en/782012.htm#id117">English Translation</a><br />
|
||||
<a href="../../others/gsab/fr/782012.htm#id117" lang="fr">En Français</a></dd>
|
||||
|
||||
<dt>79.1855<dd><cite>(GSAB) <span lang="fr">Spéalp</span> 3 (Oct.
|
||||
<dt>79.1855</dt><dd><cite>(GSAB) <span lang="fr">Spéalp</span> 3 (Oct.
|
||||
1978) pp 44-45, survey</cite>, <b lang="de">Ahnenschacht 77/78</b>, Jean
|
||||
Pierre Braun<br>
|
||||
Pierre Braun<br />
|
||||
|
||||
<a href="../../others/gsab/en/791855.htm">English Translation</a><br>
|
||||
<a href="../../others/gsab/fr/791855.htm" lang="fr">En Français</a>
|
||||
<a href="../../others/gsab/en/791855.htm">English Translation</a><br />
|
||||
<a href="../../others/gsab/fr/791855.htm" lang="fr">En Français</a></dd>
|
||||
</dl>
|
||||
|
||||
<p>The above description was translated from the references by Andy
|
||||
Waddington and Jill Gates.
|
||||
Waddington and Jill Gates.</p>
|
||||
|
||||
<hr />
|
||||
<!-- LINKS -->
|
||||
|
@ -1,6 +1,7 @@
|
||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
||||
<html lang="en">
|
||||
<html>
|
||||
<head>
|
||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
||||
<title>1626:55</title>
|
||||
<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
|
||||
</head>
|
||||
@ -61,7 +62,7 @@ Geo² Long and Deep caves committee gives 70km and 725m, quoting BCRA
|
||||
Caves & Caving number 44, p 47 as its source (Summer 89).
|
||||
|
||||
<p>The labyrinthine system contains several levels of development, mostly
|
||||
southwards towards <a href="5.htm"><span lang="de">Nagelsteghöhle</a>
|
||||
southwards towards <a href="5.htm"><span lang="de">Nagelsteghöhle</span></a>
|
||||
(the probable resurgence at 850m). The current deepest point (a sump) has
|
||||
been reached by systematically traversing over pitches of 40 to 90m.
|
||||
|
||||
|
File diff suppressed because one or more lines are too long
Binary file not shown.
@ -1,6 +1,7 @@
|
||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
||||
<html lang="en">
|
||||
<html>
|
||||
<head>
|
||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
||||
<title>1623:40</title>
|
||||
<link rel="stylesheet" type="text/css" href="../../css/main2.css" />
|
||||
</head>
|
||||
@ -11,7 +12,7 @@
|
||||
<th align=right><font size=+2>3/S/T/E x</font></th></tr>
|
||||
</table></center>
|
||||
|
||||
<p>Altitudes : (from old kataster)<menu>
|
||||
<p>Altitudes : (from old kataster)<ul>
|
||||
<li>40a Oberer Eingang 1690m
|
||||
<li>40b Schneeschacht 1683m
|
||||
<li>40c Reichenvaterschacht 1635m
|
||||
@ -35,7 +36,7 @@ Other SMKHS entrances:
|
||||
<li>40q Schwaben-Schachthöhle-Eingang c
|
||||
<li>40r Schwaben-Schachthöhle-Eingang d
|
||||
|
||||
</menu>
|
||||
</ul>
|
||||
|
||||
<p>Laser rangefinding puts an entrance (which we believe is 40a - the
|
||||
highest) at E 36458.2 N (52)81700.4 H 1689.5
|
||||
|
@ -1,6 +1,7 @@
|
||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
||||
<html lang=en>
|
||||
<html>
|
||||
<head>
|
||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
||||
<title>
|
||||
1623/116 Elevation
|
||||
</title>
|
||||
@ -9,7 +10,7 @@
|
||||
<body>
|
||||
<center>
|
||||
<h1>1623/116 - Kleine Eishöhle ELEVATION</h1>
|
||||
<img src="../i/116elv.png" width=650 height=440></center>
|
||||
<img src="../i/116elv.png" width="650" height="440" alt="" /></center>
|
||||
<hr />
|
||||
<!-- LINKS -->
|
||||
<ul>
|
||||
|
@ -1,6 +1,7 @@
|
||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
||||
<html lang=en>
|
||||
<html>
|
||||
<head>
|
||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
||||
<title>
|
||||
1623/116 Plan
|
||||
</title>
|
||||
@ -9,7 +10,7 @@
|
||||
<body>
|
||||
<center>
|
||||
<h1>1623/116 - Kleine Eishöhle PLAN</h1>
|
||||
<img src="../i/116pln.png" width=564 height=586></center>
|
||||
<img src="../i/116pln.png" width="564" height="586" alt="" /></center>
|
||||
<hr />
|
||||
<!-- LINKS -->
|
||||
<ul>
|
||||
|
@ -1,6 +1,7 @@
|
||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
||||
<html lang=en>
|
||||
<html>
|
||||
<head>
|
||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
||||
<title>
|
||||
Climbing on ice formations in Schwarzmooskogeleishöhle
|
||||
</title>
|
||||
|
@ -1,6 +1,7 @@
|
||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
||||
<html lang=en>
|
||||
<html>
|
||||
<head>
|
||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
||||
<title>
|
||||
1623: Schwarzmooskogeleishöhle approach
|
||||
</title>
|
||||
|
@ -1,6 +1,7 @@
|
||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
||||
<html lang="en">
|
||||
<html>
|
||||
<head>
|
||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
||||
<title>1977: Mike Perryman's report in Descent 38</title>
|
||||
<link rel="stylesheet" type="text/css" href="../../../css/main2.css" />
|
||||
</head>
|
||||
|
@ -1,6 +1,7 @@
|
||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
||||
<html lang="en">
|
||||
<html>
|
||||
<head>
|
||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
||||
<title>1978: Nick Thorne's report for Descent 40</title>
|
||||
<link rel="stylesheet" type="text/css" href="../../../css/main2.css" />
|
||||
</head>
|
||||
|
@ -1,6 +1,7 @@
|
||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
||||
<html lang="en">
|
||||
<html>
|
||||
<head>
|
||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
||||
<title>1979: Nick Thorne's report for Descent 44</title>
|
||||
<link rel="stylesheet" type="text/css" href="../../../css/main2.css" />
|
||||
</head>
|
||||
|
@ -1,6 +1,7 @@
|
||||
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
|
||||
<html lang="en">
|
||||
<html>
|
||||
<head>
|
||||
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
|
||||
<title>1980: Nick Thorne's report for Descent 49</title>
|
||||
<link rel="stylesheet" type="text/css" href="../../../css/main2.css" />
|
||||
</head>
|
||||
|
Loading…
Reference in New Issue
Block a user