Subglacial drainage by groundwater-channel coupling, and the origin of esker systems: Part 1—glaciological observations

Author:

Boulton G.S.,Lunn R.,Vidstrand P.,Zatsepin S.

Publisher

Elsevier BV

Subject

Geology,Archeology,Archeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference51 articles.

1. Physical Processes of Sedimentation;Allen,1970

2. Hydrology of Ice Caps in Volcanic Regions;Björnsson,1988

3. Scales and rates of glacial sediment removal: a 20km long, 300m deep trench created beneath Breidamerkurjökull during the Little Ice Age;Björnsson;Annals of Glaciology,1996

4. Bogadottir, H., Boulton, G.S., Tomasson, H., Thors, K., 1985. The structure of the sediments beneath Breidamerkursandur and the form of the underlying bedrock. In: Sigbjarnarson, (Ed.), Iceland Coastal and River Symposium. Proceedings National Energy Authority, Reykjavik, Iceland, pp. 295–303.

5. Groundwater flow beneath ice sheets: Part II—its impact on glacier tectonic structures and moraine formation;Boulton;Quaternary Science Reviews,1995

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