Relict sorted patterned ground in Lesotho

Abstract Relict sorted patterned ground is described from an upland interfluve on the Lesotho‐South Africa border at an elevation of 3280 m a.s.l. The site comprises 2–4° slope angles. Frost penetration through the regolith is inferred to have been to 1 m depth during pattern formation. Sorting is t...

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Published in:Permafrost and Periglacial Processes
Main Author: Sumner, Paul
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2004
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.459
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spelling crwiley:10.1002/ppp.459 2024-06-02T08:13:03+00:00 Relict sorted patterned ground in Lesotho Sumner, Paul 2004 http://dx.doi.org/10.1002/ppp.459 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.459 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.459 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 15, issue 1, page 89-93 ISSN 1045-6740 1099-1530 journal-article 2004 crwiley https://doi.org/10.1002/ppp.459 2024-05-03T10:49:35Z Abstract Relict sorted patterned ground is described from an upland interfluve on the Lesotho‐South Africa border at an elevation of 3280 m a.s.l. The site comprises 2–4° slope angles. Frost penetration through the regolith is inferred to have been to 1 m depth during pattern formation. Sorting is thought to have resulted from deep seasonal freezing during the depressed temperatures of the Late‐Pleistocene Last Glacial Maximum (∼18 000 years B.P.). No direct evidence for permafrost is documented. Copyright © 2004 John Wiley & Sons, Ltd. Article in Journal/Newspaper permafrost Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 15 1 89 93
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Relict sorted patterned ground is described from an upland interfluve on the Lesotho‐South Africa border at an elevation of 3280 m a.s.l. The site comprises 2–4° slope angles. Frost penetration through the regolith is inferred to have been to 1 m depth during pattern formation. Sorting is thought to have resulted from deep seasonal freezing during the depressed temperatures of the Late‐Pleistocene Last Glacial Maximum (∼18 000 years B.P.). No direct evidence for permafrost is documented. Copyright © 2004 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Sumner, Paul
spellingShingle Sumner, Paul
Relict sorted patterned ground in Lesotho
author_facet Sumner, Paul
author_sort Sumner, Paul
title Relict sorted patterned ground in Lesotho
title_short Relict sorted patterned ground in Lesotho
title_full Relict sorted patterned ground in Lesotho
title_fullStr Relict sorted patterned ground in Lesotho
title_full_unstemmed Relict sorted patterned ground in Lesotho
title_sort relict sorted patterned ground in lesotho
publisher Wiley
publishDate 2004
url http://dx.doi.org/10.1002/ppp.459
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.459
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.459
genre permafrost
Permafrost and Periglacial Processes
genre_facet permafrost
Permafrost and Periglacial Processes
op_source Permafrost and Periglacial Processes
volume 15, issue 1, page 89-93
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.459
container_title Permafrost and Periglacial Processes
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