The glacial landforms of Glen Geusachan, cairngorms: A reinterpretation

Matthew R. Bennett; Neil F. Glasser

doi:10.1080/00369229118736819

The glacial landforms of Glen Geusachan, cairngorms: A reinterpretation

Matthew R. Bennett, Neil F. Glasser

University of Edinburgh

Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid

40 Dyfyniadau (Scopus)

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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.

Iaith wreiddiol	Saesneg
Tudalennau (o-i)	116-123
Nifer y tudalennau	8
Cyfnodolyn	Scottish Geographical Magazine
Cyfrol	107
Rhif cyhoeddi	2
Dynodwyr Gwrthrych Digidol (DOIs)	https://doi.org/10.1080/00369229118736819
Statws	Cyhoeddwyd - Medi 1991

Mynediad at Ddogfen

10.1080/00369229118736819

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title = "The glacial landforms of Glen Geusachan, cairngorms: A reinterpretation",

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.",

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author = "Bennett, {Matthew R.} and Glasser, {Neil F.}",

year = "1991",

month = sep,

doi = "10.1080/00369229118736819",

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AU - Bennett, Matthew R.

AU - Glasser, Neil F.

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N2 - 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.

AB - 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.

KW - Deglaciation

KW - Glen Geusachan

KW - Hummocky moraine

KW - Loch Lomond Stadial

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SN - 1470-2541

VL - 107

SP - 116

EP - 123

JO - Scottish Geographical Magazine

JF - Scottish Geographical Magazine

IS - 2

ER -

The glacial landforms of Glen Geusachan, cairngorms: A reinterpretation

Crynodeb

Mynediad at Ddogfen

Cysylltiad parhaol

Ffeiliau eraill a chysylltiadau

Ôl bys

Dyfynnu hyn