Palaeoclimatic reconstruction from Loch Lomond Readvance glaciers in the West Drumochter Hills, Scotland

Geomorphological mapping in the West Drumochter Hills provides evidence of a readvance of locally nourished glaciers during the Loch Lomond (Younger Dryas) Stade, in the form of an icefield 67.7 km(2) in area drained by outlet glaciers. The icefield limits accord broadly with those proposed by Sisso...

Full description

Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Benn, DI, Ballantyne, Colin Kerr
Format: Article in Journal/Newspaper
Language:English
Published: 2005
Subjects:
Loch Lomond Stade
equilibrium line altitudes
icefield
Scotland
palaeoclimate
EQUILIBRIUM-LINE ALTITUDES
CENTRAL GRAMPIAN HIGHLANDS
HUMMOCKY MORAINE
AIR TEMPERATURES
VALLEY GLACIERS
YOUNGER DRYAS
AGE
DEGLACIATION
MOUNTAINS
CLIMATE
Ela
Loch Lomond
Mull
Ice Sheet
Online Access:https://risweb.st-andrews.ac.uk/portal/en/researchoutput/palaeoclimatic-reconstruction-from-loch-lomond-readvance-glaciers-in-the-west-drumochter-hills-scotland(1ca729b7-47e0-4982-800d-4f8b44a68c2b).html
https://doi.org/10.1002/jqs.925
http://www.scopus.com/inward/record.url?scp=25444445022&partnerID=8YFLogxK

Similar Items