Titlebook: Landforms of High Mountains; Alexander Stahr,Ewald Langenscheidt Book 2015 Springer-Verlag Berlin Heidelberg 2015 Erosion forms.Geomorphol

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Glaciers,nawed on mountains, abrased the bottom of the valleys, and deposited large amounts of debris. Glaciers are a huge water reservoir for people who live in high mountains; their dammed meltwater supplies energy to millions, and without glaciers, high mountains would lose their charm and fascination for mountaineers, hikers, and nature lovers.

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from many different countries and continents.This image atlas?and reference book is written in simple language that can be understood by a broad audience. The work comprehensively explains the geomorphological forms of high mountains using many examples like glacial erosion forms and deposits such a

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Landforms Determined by Tectonics,e earth’s crust. Therefore, wherever tectonic plates are colliding earth’s largest, more or less folded ranges of high mountains are arising as mountain chains. These are for example: the Alps, the Himalaya, the Andes, the Rocky Mountains, the Caucasus, or the central mountains of Papua New Guinea.

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Meltwater and Landscape, the glaciers. Some speak therefore of “fluvioglacial” erosion and deposition. If these processes are happening outside of the glacier instead, it is called “glacialfluvial.” In scientific literature, there is often the synonymous use of the two terms (Fig. 9.1).

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Book 2015eomorphological forms of high mountains using many examples like glacial erosion forms and deposits such as moraines and gravel terraces, which are illustrated with numerous photographs. Landslide landscapes, volcanoes, weathering, and erosion are other examples discussed. These examples are from ac

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