The Late Devensian and Flandrian history of the Teith valley, Scotland

Two episodes of glaciation are identified in the Teith valley, central Scotland. During the earlier episode, the valley was wholly occupied by an ice sheet, but during the later episode, correlated with the Loch Lomond Readvance, ice only occupied the upper part of the valley. The deglaciation which...

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Published in:Boreas
Main Authors: SMITH, DAVID E., THOMPSON, KENNETH S. R., KEMP, DAVID D.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1978
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1502-3885.1978.tb00268.x
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spelling crwiley:10.1111/j.1502-3885.1978.tb00268.x 2024-09-15T18:12:21+00:00 The Late Devensian and Flandrian history of the Teith valley, Scotland SMITH, DAVID E. THOMPSON, KENNETH S. R. KEMP, DAVID D. 1978 http://dx.doi.org/10.1111/j.1502-3885.1978.tb00268.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1978.tb00268.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1978.tb00268.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 7, issue 2, page 97-107 ISSN 0300-9483 1502-3885 journal-article 1978 crwiley https://doi.org/10.1111/j.1502-3885.1978.tb00268.x 2024-07-25T04:21:29Z Two episodes of glaciation are identified in the Teith valley, central Scotland. During the earlier episode, the valley was wholly occupied by an ice sheet, but during the later episode, correlated with the Loch Lomond Readvance, ice only occupied the upper part of the valley. The deglaciation which followed each episode was marked in particular by sequences of kame and outwash terraces. A terrace related to the second episode grades into a large fan buried beneath a sequence of marine deposits in the nearby Forth valley. The latest of these, the carse clays, are related to Flandrian terraces in the Teith valley. Article in Journal/Newspaper Ice Sheet Wiley Online Library Boreas 7 2 97 107
institution Open Polar
collection Wiley Online Library
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language English
description Two episodes of glaciation are identified in the Teith valley, central Scotland. During the earlier episode, the valley was wholly occupied by an ice sheet, but during the later episode, correlated with the Loch Lomond Readvance, ice only occupied the upper part of the valley. The deglaciation which followed each episode was marked in particular by sequences of kame and outwash terraces. A terrace related to the second episode grades into a large fan buried beneath a sequence of marine deposits in the nearby Forth valley. The latest of these, the carse clays, are related to Flandrian terraces in the Teith valley.
format Article in Journal/Newspaper
author SMITH, DAVID E.
THOMPSON, KENNETH S. R.
KEMP, DAVID D.
spellingShingle SMITH, DAVID E.
THOMPSON, KENNETH S. R.
KEMP, DAVID D.
The Late Devensian and Flandrian history of the Teith valley, Scotland
author_facet SMITH, DAVID E.
THOMPSON, KENNETH S. R.
KEMP, DAVID D.
author_sort SMITH, DAVID E.
title The Late Devensian and Flandrian history of the Teith valley, Scotland
title_short The Late Devensian and Flandrian history of the Teith valley, Scotland
title_full The Late Devensian and Flandrian history of the Teith valley, Scotland
title_fullStr The Late Devensian and Flandrian history of the Teith valley, Scotland
title_full_unstemmed The Late Devensian and Flandrian history of the Teith valley, Scotland
title_sort late devensian and flandrian history of the teith valley, scotland
publisher Wiley
publishDate 1978
url http://dx.doi.org/10.1111/j.1502-3885.1978.tb00268.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1978.tb00268.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1978.tb00268.x
genre Ice Sheet
genre_facet Ice Sheet
op_source Boreas
volume 7, issue 2, page 97-107
ISSN 0300-9483 1502-3885
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op_doi https://doi.org/10.1111/j.1502-3885.1978.tb00268.x
container_title Boreas
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