Stampflkees
| Stampflkees | ||
|---|---|---|
 The Stampflkees with the Schrammacher |
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| location | Tyrol , Austria | |
| Mountains | Zillertal Alps | |
| surface | 1.59 km² (1999) | |
| Exposure | south | |
| Altitude range | 3276 m above sea level A. - 2800 m above sea level A. | |
| Tilt | ⌀ 16.8 ° (30%) | |
| Coordinates | 47 ° 1 '6 " N , 11 ° 38' 16" E | |
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| drainage | Zamser Bach → Zemmbach → Ziller → Inn | |
The Stampflkees is a glacier in the Zillertal Alps in Tyrol . With an area of around 1.5 km², it is the second largest glacier in the Tux main ridge after the Tuxer Ferner .
The Stampflkees flows south on the southeast flank of the Tuxer Kamm. The nutrient area is framed by the Hoher Wand ( 3289 m above sea level ), Sagwandspitze ( 3227 m above sea level ) and Schrammacher ( 3410 m above sea level ). In the east, the narrow Schrammach ridge separates the glacier from the much smaller Oberschrammachkees. It drains over the Zamser Bach and Zemmbach to the Ziller .
Since the end of the Little Ice Age around 1850, the Stampflkees, like many other Alpine glaciers, has retreated a long way . The ice-free foreland of the glacier has very high lateral moraines , the western one is up to 65 m high. The terminal moraine at around 2250 m marks the last high point of the glacier around 1850. The area between 2530 m and 2700 m is occupied by the moraine of the advance around 1920.
Individual evidence
- ↑ a b Michael Kuhn, Astrid Lambrecht, Jakob But man (2013): Austrian glacier inventory 1998 (GI II). PANGEA, doi : 10.1594 / PANGEA.809196
- ↑ a b Jerzy Zasadni: Report 2008 on geological recordings of Quaternary sediments in the Zemmtal and Zamsergrund on sheet 149 Lanersbach. In: Yearbook of the Federal Geological Institute, Volume 149 (2009), pp. 541–545 ( PDF; 468 kB )