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60 lines
2.5 KiB
HTML
60 lines
2.5 KiB
HTML
<!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.0//EN">
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<html lang=en>
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<head>
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<title>1623:190</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>190</font></th>
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<th align=center><font size=+2>Glitterstompf</font><br>(formerly CUCC 1976/B9)</th>
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<th align=right><font size=+2>1/S/t/E =</font></th></tr>
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</table></center>
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<p><b>Altitude:</b> c 1640m or a little higher<br>
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<b>Depth:</b> c 25m<br>
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<b>Location: (Tag) E 35561, N 82547</b>
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<b>Access:</b>From <a href="164.htm">164</a>, north to an east-west
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fault line (climbing past the large open and heavily snow-plugged shaft,
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which is <a href="189.htm">189</a>). To the east, this fault line is a
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north-facing scarp, below which is 190 (number in red, and Austrian metal
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tag on this wall above the SW corner of the shaft), somewhat before (ie.
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west of) <a href="197.htm">B8</a> (1623/197).
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<p><b>Marking:</b> On wall above entrance, facing N, number in red, 1993.
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Austrian metal tag, 1995. The 1976 number "B9" was in dull green
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and was already hard to spot in 1977, since when it has not been seen.
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<p><center><a href="others/l/190.htm"><img alt="Entrance photo"
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src="others/t/190.jpg" width=121 height=177></a></center>
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<p>Rectangular shaft 6.7m long (aligned on a joint on 275°) and 4.0m
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wide. Wall on south side is 1.5m higher than rest of surface. Freeclimb
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descent of 6m to scree/boulder floor usually with snow plug. At eastern end
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of the south wall, a horizontal passage leads 7.5m on 185° to the lip of
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a second pitch. This is 10m leading to a big rift. Ahead over boulders and
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ice an 8m pitch descends through (sic) spectacular ice stalactites. Way on is
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effectively blocked by ice but could well connect with a major shaft nearby
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(<a href="189.htm">1623/189</a>), not descended in 1976 on account of the
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condition of the ice. The small alternative hole back in the rift is blocked
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by ice at -6m.
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<p>In 1993 the cave was "extremely cold and some ice formations".
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<p><b>Exploration:</b> CUCC 1976, 1993
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<hr>
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