Late Quaternary ice flow in a West Greenland fjord and cross-shelf trough system: submarine landforms from Rink Isbrae to Uummannaq shelf and slope

Sea-floor landforms and acoustic-stratigraphic records allow interpretation of the past form and flow of a westward-draining ice stream of the Greenland Ice Sheet, Rink Isbrae. The Late Pliocene-Pleistocene glacial package is several hundred metres thick and down-laps onto an upper Miocene horizon....

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Bibliographic Details
Main Authors: Julian A. Dowdeswell, K.A. Hogan, Colm O Cofaigh, E.M.G. Fugelli, Jeffrey Evans, R. Noormets
Format: Default Article
Published: 2014
Subjects:
Other earth sciences not elsewhere classified
Arctic
Ice flow
Ice stream
Late Quaternary
Submarine landforms
Trough-mouth fan
West Greenland
Earth Sciences not elsewhere classified
Online Access:https://hdl.handle.net/2134/17834
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https://hdl.handle.net/2134/17834

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