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A reinterpretation of Scottish ‘hummocky moraine’ and its significance for the deglaciation of the Scottish Highlands during the Younger Dryas or Loch Lomond Stadial

Published online by Cambridge University Press:  01 May 2009

Matthew R. Bennett  and
Geoffrey S. Boulton
Matthew R. Bennett
Affiliation:
Department of Geology and Geophysics, The Grant Institute, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, U.K.
Geoffrey S. Boulton
Affiliation:
Department of Geology and Geophysics, The Grant Institute, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, U.K.
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Abstract

The aim of this paper is to demonstrate that much of the ‘hummocky moraine’ present within the northern part of the LochLomond Readvance ice cap formerly situated in the North West Scottish Highlands may be interpreted as suites of ice-front moraines deposited during active decay. These landforms can be used to reconstruct ice cap decay, whichleads to important insights into the shrinking form of the ice cap and associated environmental conditions. Evidence has been collected from 10803 airphotographs and from detailed field survey. It is presented at three spatial scales.

Type
Articles
Information
Geological Magazine , Volume 130 , Issue 3 , May 1993 , pp. 301 - 318
Copyright
Copyright © Cambridge University Press 1993

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