Titlebook: Glaciology and Glacial Geomorphology; Wilfried Hagg Textbook 2022 The Editor(s) (if applicable) and The Author(s), under exclusive license

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Michael Ertel,Eberhard Pech,Peter Ullspergerrole here. Glacial ice, a material with special physical properties, is formed from snow via various transformation processes. The temperature of the ice is of central importance for the movement of the glaciers and the shaping of the bedrock.

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Heavy Metals in the Infant Diet,a. Over the last 75 years, a binding catalogue of terms and methods has emerged, all of which have advantages and disadvantages. In addition to the three classical methods of mass balance determination, a new approach has been added in recent years in the form of the gravimetric method, which has ye

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https://doi.org/10.1057/9781137282613 typification according to the mode of feeding, which is hardly in use today. The most commonly used classification is morphological glacier types, where, strictly speaking, glaciers are categorized according to their size, their position in the relief and its influence on ice movement. The subdivis

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https://doi.org/10.1007/978-981-16-0578-9ous phase. Hydrological systems exist on, in and under glaciers that regulate the budget of this water reservoir. In the case of supraglacial ice melt, in addition to the energy exchange with the atmosphere, the debris layers are of particular importance because, depending on their thickness, they c

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T.K. Sundari Ravindran,Rakhal Gaitonded human traces also allow conclusions to be drawn about past extents. In the ice ages, warm periods (interglacials) alternated with cold periods (glacials) during which the glaciers were particularly large. The triggering and regulating mechanisms of these large climate fluctuations are subject to b

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