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Eishohle entrances docum. improvements

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Philip Sargent
2025-12-21 19:19:09 +00:00
parent a765790f95
commit dbd5f3b11b
21 changed files with 166 additions and 103 deletions
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cave_data/1623-216.html
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@@ -1,64 +1,47 @@
<!DOCTYPE html>
<!-- This file is generated by troggle on Nov. 2, 2023, 8:14 p.m. UTC using the form documented at /handbook/survey/caveentry.html -->
<!-- This file is generated by troggle using the form documented at /handbook/survey/caveentry.html -->
<!-- ALTERNATIVELY you can download an example template from expoweb/templates/cave_data.html -->
<!-- Only put one cave in this file -->
<!-- If you edit this 1623-nnn.html file by hand, and manually upload it to the server using git,
<!-- If you edit this 162x-nnn.html file by hand, and manually upload it to the server using git,
make sure you update the database by doing a full data import. If you edit it using the online form
though, you do not need to do a data import as it happens automatically -->
<!-- ALTERNATIVELY you can download an example template from expoweb/templates/cave_data.html -->
<html lang="en">
<head>
<meta http-equiv="Content-Type" content="text/html; charset=UTF-8"/>
</head>
<body>
<b>This file is generated by troggle</b> on Nov. 2, 2023, 8:14 p.m. UTC using the form documented at
<b>This file is generated by troggle</b> using the form documented at
the form documented at
<a href="/handbook/survey/caveentry.html">handbook/survey/caveentry.html</a>
<br>
<cave>
<non_public>False</non_public><!-- 'False' or 'True'. True if the cave should only be visible to logged-in users. Caves are normally public, so enter 'False' unless you know otherwise. -->
<caveslug>1623-216</caveslug><!--(Ignored). Internal I.D. formerlly used. Using filename'' -->
<official_name>Nichts 50</official_name><!-- Name of the cave (normally in German) Use &uuml; for u+Umlaut and &ouml; for o+umlaut eg H&ouml;hle for Hohle and Gl&uuml;ck for Gluck-->
<area>1623</area><!-- e.g. "1623" -->
<kataster_code></kataster_code><!-- 'length-or-depth/type exploration'
code used in the Austrian kataster e.g '1/S +' - https://expo/.survex.com/katast.htm
<non_public>False</non_public>
<unexplored>False</unexplored>
T Trockenh&ouml;hlen (Dry caves)
W Wasserh&ouml;hlen (Caves with water)
(W) Zeitweilig aktiv Wasserh&ouml;hlen (Caves with seasonal water)
E Eishohlen (Caves with ice formations)
S Schachth&ouml;hlen (Caves with pitches)
H Halbh&ouml;hlen (Rock shelters ?)
- unerforscht (unexplored)
= befahren (visited)
× teilweise vermessen (partly surveyed)
+ erforscht (exploration considered complete)
-->
<kataster_number>216</kataster_number> <!-- (Either this or unofficial_number is required). Official number in Austrian kataster if one has been allocated -->
<unofficial_number>2000-06</unofficial_number><!-- (Either this or kataster_number is required). Initial temporary cave ID used until kataster number is allocated e.g. '2012-DD-01'-->
<official_name>Nichts 50</official_name>
<area>1623</area>
<kataster_code></kataster_code>
<kataster_number>216</kataster_number>
<unofficial_number>2000-06</unofficial_number>
<entrance>
<entranceslug>1623-216</entranceslug><!-- Internal ID to refer to each entrance instance in the entrance files (typically the same as that filename (e.g. 1623-161c). Matches the 'slug' field in the entrance file -->
<!-- DEBUG 1623-216+1623-216 'Z' == -->
<letter></letter><!--Leave blank for single-entrance cave. If there is more than one entrace then the letter needs to be given. Generally matches the entranceslug ID. -->
<entranceslug>1623-216</entranceslug>
<letter></letter>
</entrance>
<explorers>not-CUCC-Expo</explorers><!-- 'CUCC Expo' and year(s) of exploration. To distinguish from caves explored by foreign groups. Individual names can be given too if it was a small cave. -->
<survex_file>caves-1623/216/216.svx</survex_file><!-- Name of top-level survey file for this cave. Relative to the 'loser' survex repository. So for most caves that's "caves-162x/cavenum/cavnum.svx". (e.g. caves-1623/204/204.svx -->
<underground_description></underground_description><!-- Underground description. (description of approach and entrance goes in entrance file). For a small cave this will be the entire description. For larger caves it will be the front page of the description, or a short intro, containing links to other pages with the cave description in, or even nothing but a link. -->
<equipment></equipment><!-- For a small cave, summary of gear needed to descend. For longer caves it could be blank, a table, or just refer to the description/topos. Leave blank if this info is in the description. -->
<references></references><!-- References to documentation. Could be Journal articles or Logbook entries. Can be links if the docs are online. -->
<survey></survey><!-- Drawn-up surveys. Scans of paper surveys or images/PDFs of electronic surveys. Should include HTML to display current plan and elevation, with links to larger versions (See section on URLs and files). Could list links to multiple years of survey, or even a separate survey page if it's complicated enough. -->
<kataster_status></kataster_status>
<underground_centre_line>In dataset</underground_centre_line><!-- 'In dataset' if it is in the survex dataset. Blank if not, or notes about status such as 'surveyed, but no entrance fix so not yet in dataset'. -->
<notes></notes><!-- Normally empty, but place for anything else that should be noted, such as info on cave maybe being a duplicate, or lost -->
<length></length><!-- Cave length. Can be left blank and system should fill it in automatically from survey data (it doesn't yet) -->
<depth></depth><!--Cave depth. Can be left blank and system should fill it in automatically from survey data (it doesn't yet) -->
<explorers>not-CUCC-Expo</explorers>
<survex_file>caves-1623/216/216.svx</survex_file>
<underground_description></underground_description>
<equipment></equipment>
<references></references>
<survey></survey>
<notes>Thought to be the bivouak cave used by the German team exploring Eishohle (1623-40).</notes>
<length></length>
<depth></depth>
<extent></extent>
<description_file></description_file><!-- Path of top-level description file for this cave, when a separate file is used. Otherwise blank. -->
<url>1623/216/216.html</url><!-- (Required). Relative URL of this cave. i.e the URL this cave appears at on the website, not including 'https://expo.survex.com/. Normally area/cavenum., e.g ('1623/000')-->
<description_file></description_file>
</cave>
</body>
</html>

12
cave_data/1623-40.html
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@@ -17,6 +17,7 @@ the form documented at
<cave>
<non_public>True</non_public>
<unexplored>False</unexplored>
<official_name>Schwarzmooskogeleish&ouml;hle</official_name>
<area>1623</area>
@@ -75,7 +76,7 @@ the form documented at
though tackle is needed to explore it fully, and crampons are necessary in parts,
because of the substantial quantities of ice in the cave. Was extended by the Germans who worked in the area
in the early eighties, who suggested then that there was potential for extension vertically.
Subsequently linked via a 30m pitch to <a href="/1623/88/88.html">L&auml;rchenschacht</a> (1623/88) which in turn
Subsequently linked via a 30m pitch to <a href="/1623/88/88.html">L&auml;rchenschacht</a> (1623/88, now also entrance 40i) which in turn
was connected to the <a href="/1623/41/41.html">Stellerwegh&ouml;hlensystem</a>, giving no increase in depth
if the laser-rangefound altitude is correct rather than the old kataster one, which seems likely.</p>
<h4>Translated brief guide</h4><p>From 'L&auml;ngsten und Tiefsten Hohlen in &Ouml;sterreich', translated by Wookey
@@ -127,10 +128,17 @@ was connected to the <a href="/1623/41/41.html">Stellerwegh&ouml;hlensystem</a>,
<a href='/1623/40/l/40-olly-in-2000.html'><img src='/1623/40/t/40-olly-in-2000.jpg' /></a>&nbsp;
<p>
The duck was dry in 2001, but back again in 2002.</p><p>50m further round (downslope) the ice drops away steeply under the wall. A line is advisable for the descent. 20m down, the ice slope peters out giving way to sand and rocks. At the end here is a very strongly draughting hole [<a href="/1623/40/qm.htm#C000040-04" name="qC000040-04">C0000-40-04</a> B]. This appears too tight, but survey data shows this is where Kalten Gang and Spinnefriedhof are (VfHM, 1984). To the right at the foot of the slope closes down with rocks and ice - it would probably connect with Plastic Hell. A few metres up from the bottom of the slope on the left hand (N) wall is a gap between the ice and rock leading into a large chamber [<a href="qm.htm#A199840-05" name="qA199840-05">A1998-40-05</a> B] (reported by Robert Winkler).</p><p>Back in Schneevulkanhalle, another 10m clockwise round the chamber is another, steeper iceslope. A rope is definitely needed for this. This is the way to <a href="/1623/40/cucc.htm#phell">Plastic Hell.</a></p><p>Beyond and above are more thin icefalls coming from high in the ceiling - trying to climb these would be bonkers - the debris from the collapse of some of them is all around.</p><h4><a name="schotterland">Schotterland</a> (Munich cavers 198? and ARGE 2000)</h4><p>The foot of the piss-wet pitch opens out into very large triangular passage. You can go NE about 35m until it chokes (a good draught comes out of one hoplessly choked corner) or SW 20 to a T-junction. Right (W) is Kleiner keller. Left, ducking under the low wall, is Schotterland.</p><p>Kleiner keller is about 50m on huge passage to where the end is choked with glacial fill and a waterspout comes in the from the roof 3m up. A sling ladder makes it possible to ascend the waterspout - you can even doing it without getting very wet, as the spout is unusually well-concentrated, and thus avoidable. This comes into an E-W rift, with the water coming from the E end. It can be ascended in both directions at various traverse levels for about 30m, but the top appears choked at all points. The top is probably very close to the floor of Elephantengang.</p><p>The old Munich cavers' data suggests that there is a passage off kleiner keller that we missed - which seems hard to believe, but maybe it is worth another visit?</p><p>Schotterland is more enormous passage (10m wide) going SSE, presumably schotterland, due to the flooring of small rocks. A ramp goes up steeply on the L after 30m. It closes down after 40m. Ahead the passage slowly narrows until it chokes at the end - probably very close to the surface.</underground_description>
The duck was dry in 2001, but back again in 2002.</p><p>50m further round (downslope) the ice drops away steeply under the wall. A line is advisable for the descent. 20m down, the ice slope peters out giving way to sand and rocks. At the end here is a very strongly draughting hole [<a href="/1623/40/qm.htm#C000040-04" name="qC000040-04">C0000-40-04</a> B]. This appears too tight, but survey data shows this is where Kalten Gang and Spinnefriedhof are (VfHM, 1984). To the right at the foot of the slope closes down with rocks and ice - it would probably connect with Plastic Hell. A few metres up from the bottom of the slope on the left hand (N) wall is a gap between the ice and rock leading into a large chamber [<a href="qm.htm#A199840-05" name="qA199840-05">A1998-40-05</a> B] (reported by Robert Winkler).</p><p>Back in Schneevulkanhalle, another 10m clockwise round the chamber is another, steeper iceslope. A rope is definitely needed for this. This is the way to <a href="/1623/40/cucc.htm#phell">Plastic Hell.</a></p><p>Beyond and above are more thin icefalls coming from high in the ceiling - trying to climb these would be bonkers - the debris from the collapse of some of them is all around.</p><h4><a name="schotterland">Schotterland</a> (Munich cavers 198? and ARGE 2000)</h4><p>The foot of the piss-wet pitch opens out into very large triangular passage. You can go NE about 35m until it chokes (a good draught comes out of one hoplessly choked corner) or SW 20 to a T-junction. Right (W) is Kleiner keller. Left, ducking under the low wall, is Schotterland.</p><p>Kleiner keller is about 50m on huge passage to where the end is choked with glacial fill and a waterspout comes in the from the roof 3m up. A sling ladder makes it possible to ascend the waterspout - you can even doing it without getting very wet, as the spout is unusually well-concentrated, and thus avoidable. This comes into an E-W rift, with the water coming from the E end. It can be ascended in both directions at various traverse levels for about 30m, but the top appears choked at all points. The top is probably very close to the floor of Elephantengang.</p><p>The old Munich cavers' data suggests that there is a passage off kleiner keller that we missed - which seems hard to believe, but maybe it is worth another visit?</p><p>Schotterland is more enormous passage (10m wide) going SSE, presumably schotterland, due to the flooring of small rocks. A ramp goes up steeply on the L after 30m. It closes down after 40m. Ahead the passage slowly narrows until it chokes at the end - probably very close to the surface.
<center>
<a href='/1623/40/l/eishohle-ents.html'><img src='/1623/40/i/eishohle-ents.jpg' width=27%/></a>&nbsp;
<c/enter></underground_description>
<equipment></equipment>
<references></references>
<survey><center><a href='/1623/40/l/schneevulkanhalle.html'><img src='/1623/40/i/schneevulkanhalle.jpg' width=40% /></a>&nbsp;
<p>
<a href='/others/gscb/index.htm'><img src='/others/gscb/EH-plan-elev-centre.jpg' width=25% /></a><br />
<em>Old survey by GSCB before the significant extensions</em>
</center></survey>
<notes>see also <a href="/1623/40/cucc.htm">CUCC discoveries in Eish&ouml;hle</a></notes>
<length>SMK system total 54000m</length>