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

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書目名稱Landforms of High Mountains
編輯Alexander Stahr,Ewald Langenscheidt
視頻videohttp://file.papertrans.cn/581/580636/580636.mp4
概述Introduction to geomorphology understandable to a broad audience.Many photographs/illustrations ease the understanding of the text.Examples from many different countries and continents
圖書封面Titlebook: Landforms of High Mountains;  Alexander Stahr,Ewald Langenscheidt Book 2015 Springer-Verlag Berlin Heidelberg 2015 Erosion forms.Geomorphol
描述.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 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 across the world, including the Himalayas, the Alps, the Andes, and the Southern Alps of New Zealand. This work is useful for laymen who are interested in geosciences, especially high-mountain landforms, as well as for students and teachers of earth sciences..
出版日期Book 2015
關(guān)鍵詞Erosion forms; Geomorphology; Glacial erosion; Gravel terrace; High mountains; Landslide landscapes; Morai
版次1
doihttps://doi.org/10.1007/978-3-642-53715-8
isbn_softcover978-3-662-51478-8
isbn_ebook978-3-642-53715-8
copyrightSpringer-Verlag Berlin Heidelberg 2015
The information of publication is updating

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Shaping of High Mountains by Snow,ressure 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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Landscapes Caused by Geological Structure and Rock Features,Geological structures and different geomorphological features of rocks imply a clear differentiation of predominately climate-controlled weathering and erosion processes. This applies not only to high mountains, but also to all other terrestrial landscapes.
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Alexander Stahr,Ewald Langenscheidt1450 bis ca. 1850), lediglich am Rande. Seit der frühen Neuzeit fehlt ein koh?rent sich entwickelnder, aufeinander aufbauender Problemdiskurs, so dass es weder m?glich ist, eine Art ?Ideengeschichte des Alters in der Neuzeit? noch eine koh?rente Diskursgeschichte zu rekonstruieren. Vereinzelte und v
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