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- W2783176796 abstract "About 7% of Austria's currently known 16,300 caves host accumulations of perennial snow, firn, and/or ice. This high percentage is mainly due to the presence of large uplifted and heavily karstified plateaus in particular in the central and eastern part of the Northern Calcareous Alps. The highest abundance of ice-bearing caves can be found between about 1800 and 2100 m a.s.l. Most of the about 1200 ice caves in this country are small pits which act as cold traps. Almost all large ice caves, however, show more than one entrance and are characterized by strong seasonal air flow, giving rise to strong winter cooling and ice deposition close to the lower-elevation entrance. Four examples of ice caves are reviewed in this article. Eisriesenwelt opens at the western escarpment of Tennengebirge and hosts 28,000 m2 of ice behind the main (lower) entrance of a 42 km-long system. Located in the western part of Totes Gebirge, Schönberg-Höhlensystem ranks as the longest cave in the European Union. Its currently known 34 entrances give rise to a complex ventilation pattern and the presence of ice bodies in three parts of this vast system. Dachstein-Mammuthöhle is a giant cave system at the northern escarpment of the Dachstein massif. Its two ice-bearing parts show an uninterrupted decline of ice height and volume since at least the last three decades and the ice will likely disappear within the next decade. Located in the lower Inn Valley of Tyrol, Hundsalm Eis- und Tropfsteinhöhle is an example of a small sag-type cave hosting a shrinking firn and ice body. This cave will likely transform into a seasonal ice cave within the not-too-distant future." @default.
- W2783176796 created "2018-01-26" @default.
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- W2783176796 date "2018-01-01" @default.
- W2783176796 modified "2023-10-18" @default.
- W2783176796 title "Ice Caves in Austria" @default.
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- W2783176796 doi "https://doi.org/10.1016/b978-0-12-811739-2.00013-9" @default.
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