Landform-sediment distributions within the northern part of the younger dryas highland ice-field, Scotland

被引：5

作者：

Bennett, MR

机构：

[1] School of Earth Sciences, University of Greenwich, Medway Towns Campus, Chatham Maritime

来源：

SCOTTISH JOURNAL OF GEOLOGY | 1996年 / 32卷

关键词：

WITHIN-VALLEY ASYMMETRY; LOCH-LOMOND READVANCE; ISLE-OF-SKYE; HUMMOCKY MORAINE; DEGLACIATION; GLACIERS; REINTERPRETATION; LAURENTIDE; SHEETS;

D O I：

10.1144/sjg32020097

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

The aim of this paper is to describe the landform-sediment distribution within the northern part of the Highland ice-field, which existed in the Scottish Highlands during the Loch Lomond Stadial or Younger Dryas. Strong spatial variations in the distribution of both subglacial and ice-marginal landforms are described. The role of geology and variations in the dynamics of this former ice-field are discussed as possible explanations for the observed patterns.

引用

收藏

页码：97 / 105

页数：9

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