A REINTERPRETATION OF SCOTTISH HUMMOCKY MORAINE AND ITS SIGNIFICANCE FOR THE DEGLACIATION OF THE SCOTTISH HIGHLANDS DURING THE YOUNGER DRYAS OR LOCH-LOMOND STADIAL

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

Authors: Bennett, M.R., Boulton, G.S.

Journal: Geological Magazine

Publication Date: 01/01/1993

Volume: 130

Issue: 3

Pages: 301-318

eISSN: 1469-5081

ISSN: 0016-7568

DOI: 10.1017/S0016756800019993

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. © 1993, Cambridge University Press. All rights reserved.

Source: Scopus

Authors: BENNETT, M.R., BOULTON, G.S.

Journal: GEOLOGICAL MAGAZINE

Publication Date: 05/1993