Abstract
Snow is a major factor of actual landscape shaping in high mountains of the middle and high latitudes. A snow blanket demands the Earth’s surface by pressure and movement, and meltwater also plays an important role. The process of landscape shaping by snow is called nivation (from Latin nix = snow). It can take place very slowly by frost splitting or gliding snow blankets, but also very quickly by snow slab avalanches.
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© 2015 Springer-Verlag Berlin Heidelberg
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Stahr, A., Langenscheidt, E. (2015). Shaping of High Mountains by Snow. In: Landforms of High Mountains. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-53715-8_6
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DOI: https://doi.org/10.1007/978-3-642-53715-8_6
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Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-53714-1
Online ISBN: 978-3-642-53715-8
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