Glaciohydraulic supercooling in former ice sheets?

Glaciohydraulic supercooling has been observed at many modern glaciers and has been shown to generate thick zones of debris-laden basal ice which, when exposed to melting, can produce debris-flow and melt-out till deposits, as well as hummocky terrain. Glaciohydraulic supercooling probably occurred...

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Bibliographische Detailangaben

Veröffentlicht in:	Geomorphology (Amsterdam) 2006-04, Vol.75 (1), p.20-32
Hauptverfasser:	Larson, Grahame J., Lawson, Daniel E., Evenson, Edward B., Alley, Richard B., Knudsen, Óskar, Lachniet, Mathew S., Goetz, Staci L.
Format:	Artikel
Sprache:	eng
Schlagworte:	Basal ice Debris-flow deposits Earth sciences Earth, ocean, space Exact sciences and technology External geophysics Geomorphology, landform evolution Glaciers Glaciohydraulic supercooling Ice sheets Marine and continental quaternary Melt-out till Snow. Ice. Glaciers Surficial geology
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