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- W2019928287 endingPage "1038" @default.
- W2019928287 startingPage "1017" @default.
- W2019928287 abstract "Simple insights from the physics of ice, water and sediment place constraints on the possible sediment-transport behavior of glaciers and ice sheets. Because glaciers concentrate runoff, streams generated by glaciers transport much sediment and may erode bedrock rapidly. Deforming glacier beds also can transport much sediment, particularly in marginal regions. Rapid sediment entrainment producing thick debris-rich basal zones may occur by regelation into subglacial materials, and by freeze-on from rising supercooled waters. Numerous other mechanisms may be important but primarily near ice margins, especially those of advancing or fluctuating glaciers. Several sediment-entrainment mechanisms may be active beneath a single glacier, but one process is likely to be dominant at any place and time." @default.
- W2019928287 created "2016-06-24" @default.
- W2019928287 creator A5007889831 @default.
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- W2019928287 creator A5080247995 @default.
- W2019928287 creator A5080342215 @default.
- W2019928287 date "1997-01-01" @default.
- W2019928287 modified "2023-10-08" @default.
- W2019928287 title "How glaciers entrain and transport basal sediment: Physical constraints" @default.
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