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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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 |
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Wiley Online Library |
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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 |
container_volume |
15 |
container_issue |
1 |
container_start_page |
89 |
op_container_end_page |
93 |
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1800759693102022656 |