Geomorphological consequences of a glacier advance across a paraglacial rock avalanche deposit

Glacial reworking of paraglacial rock slope sediment has been inferred from long-deglaciated terrains to contribute significantly to glacial sediment transfer. At Feegletscher, Switzerland, we provide the first description of the geomorphological consequences of glacier advance across paraglacial ro...

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Veröffentlicht in:	Geomorphology (Amsterdam, Netherlands) Netherlands), 2013-05, Vol.189, p.109-120
Hauptverfasser:	Cook, Simon J., Porter, Philip R., Bendall, Charles A.
Format:	Artikel
Sprache:	eng
Schlagworte:	Avalanches Debris Deposits Earth sciences Earth, ocean, space Exact sciences and technology Geomorphology Geomorphology, landform evolution Glacial geomorphology Glacial reworking Glacial sedimentology Glaciers Marine and continental quaternary Moraine Paraglacial Rock Rock avalanche Sediments shear strength snowmelt Surficial geology Terrain
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