Titlebook: Geomorphology of Proglacial Systems; Landform and Sedimen Tobias Heckmann,David Morche Book 2019 Springer Nature Switzerland AG 2019 Alpine

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Debris-Covered Glacierslacier mass balance as they are regions of significantly enhanced ice melt. The glacier snouts of debris-covered glaciers are often very slow or stagnant, and the terminus positions are stable over long periods. In this case, only small amounts of debris are transported from the glacial into the pro

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Closing the Balances of Ice, Water and Sediment Fluxes Through the Terminus of Gepatschfernerce, water and sediments entering the narrow terminus at an elevation of 2875 m and leaving it at the glacier snout at 2200 m was based on glacier motion, surface and basal melt rates and on the lateral mass transport to the glacier from rock face and moraine bedrock erosion recorded from repeated te

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(Ground) Ice in the Proglacial Zoneglacio-fluvial processes, low-temperature conditions, as well as the occurrence of ground ice, are the most effective drivers for geomorphic dynamics and related landform evolution in these proglacial areas. A deeper knowledge of ongoing processes as well as of the amounts of sediment and ground ice

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Rock Slope Instability in the Proglacial Zone: State of the Art: (i) fracture growth and seismicity arising from the unloading of glacial loads over millennial timescales, and (ii) rock fracture growth and loss of strength as a result of hydrological and thermal effects that fluctuate over daily to seasonal timescales, but are superimposed upon long-term trends

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Glacial Sediment Stores and Their Reworkingtic complexity and geomorphological evidence of sediment reworking, in the form of deep gullies and associated debris cones and fans, would suggest that such units can yield sediments dependant on multiple climatic, geomorphical and biogeomorphical factors. Similarly, the extent to which the general

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Glacier Changes Since the Little Ice AgeIce Age (LIA). During this period, the lateral accumulation of rock and debris created impressive moraine walls. Between these LIA moraines and the actual terminus position is the glacier forefield, which is growing as glaciers retreat. Whereas the forefields are constantly changing (e.g. due to the