The glacial landforms of Glen Geusachan, cairngorms: A reinterpretation
- 1 September 1991
- journal article
- research article
- Published by Taylor & Francis in Scottish Geographical Magazine
- Vol. 107 (2) , 116-123
- https://doi.org/10.1080/00369229118736819
Abstract
A former glacier is described in Glen Geusachan similar to that identified by Sissons (1979), which probably dates from the Loch Lomond Stadial. However, the “hummocky moraine” within these glacial limits is reinterpreted here as an assemblage of individual ice‐marginal landforms. It implies that the Loch Lomond Stadial deglaciation in Glen Geusachan was characterized by active retreat, the stages and pattern of which are described.Keywords
This publication has 20 references indexed in Scilit:
- The deglaciation of Glen Croulin, KnoydartScottish Journal of Geology, 1990
- The abrupt termination of the Younger Dryas climate eventNature, 1989
- Controls on sedimentation in a late Devensian ice‐dammed lake, Achnasheen, ScotlandBoreas, 1989
- A radiocarbon date on plant detritus beneath till from the type area of the Loch Lomond ReadvanceScottish Journal of Geology, 1988
- Push‐moraines and glacier‐contact fans in marine and terrestrial environmentsSedimentology, 1986
- A study of fluted moraines in the Torridon area, NW ScotlandJournal of Quaternary Science, 1986
- "Crevasse-Fill" Ridges: A Landform Type Characteristic of Surging Glaciers?Geografiska Annaler: Series A, Physical Geography, 1985
- The last glaciers in part of the South East GrampiansScottish Geographical Magazine, 1972
- The Development and Destruction of a Sandur, Breidamerkurjokull, IcelandArctic and Alpine Research, 1971
- West Highland morainic features aligned in the direction of ice flowScottish Journal of Geology, 1967