Secondary sorting of sorted patterned ground

Abstract The arrangement of small sorted patterns within the central fine domain of a larger sorted circle (herein called 'secondary sorting') was observed at two patterned ground sites: Arikaree Cirque, Colorado Front Range, USA, and Kapp Linné, Western Spitzbergen. Large polygons do not...

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Published in:Permafrost and Periglacial Processes
Main Author: Warburton, Jeff
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1990
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.3430010312
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spelling crwiley:10.1002/ppp.3430010312 2024-06-02T08:13:11+00:00 Secondary sorting of sorted patterned ground Warburton, Jeff 1990 http://dx.doi.org/10.1002/ppp.3430010312 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430010312 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430010312 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 1, issue 3-4, page 313-318 ISSN 1045-6740 1099-1530 journal-article 1990 crwiley https://doi.org/10.1002/ppp.3430010312 2024-05-03T11:32:00Z Abstract The arrangement of small sorted patterns within the central fine domain of a larger sorted circle (herein called 'secondary sorting') was observed at two patterned ground sites: Arikaree Cirque, Colorado Front Range, USA, and Kapp Linné, Western Spitzbergen. Large polygons do not appear to be randomly filled by smaller ones of all sizes. The size of the inset polygons seems to be related to the dimensions of the larger form. Preliminary field survey suggests that large forms are filled by smaller polygon sizes in a width ratio of approximately 1:2.5‐3. Subdivision of the fine centres occurs in 77% of the sorted polygons at the Colorado site ( n = 100) but only 42% of patterns at Kapp Linné (n = 31). Possible explanations of the scaling of the secondary polygons include pore water and/or soil convection and desiccation cracking. Desiccation crack systems simulated in a laboratory experiment are similar to those observed in the field. Article in Journal/Newspaper Permafrost and Periglacial Processes Spitzbergen Wiley Online Library Kapp Linné ENVELOPE(13.621,13.621,78.063,78.063) Permafrost and Periglacial Processes 1 3-4 313 318
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The arrangement of small sorted patterns within the central fine domain of a larger sorted circle (herein called 'secondary sorting') was observed at two patterned ground sites: Arikaree Cirque, Colorado Front Range, USA, and Kapp Linné, Western Spitzbergen. Large polygons do not appear to be randomly filled by smaller ones of all sizes. The size of the inset polygons seems to be related to the dimensions of the larger form. Preliminary field survey suggests that large forms are filled by smaller polygon sizes in a width ratio of approximately 1:2.5‐3. Subdivision of the fine centres occurs in 77% of the sorted polygons at the Colorado site ( n = 100) but only 42% of patterns at Kapp Linné (n = 31). Possible explanations of the scaling of the secondary polygons include pore water and/or soil convection and desiccation cracking. Desiccation crack systems simulated in a laboratory experiment are similar to those observed in the field.
format Article in Journal/Newspaper
author Warburton, Jeff
spellingShingle Warburton, Jeff
Secondary sorting of sorted patterned ground
author_facet Warburton, Jeff
author_sort Warburton, Jeff
title Secondary sorting of sorted patterned ground
title_short Secondary sorting of sorted patterned ground
title_full Secondary sorting of sorted patterned ground
title_fullStr Secondary sorting of sorted patterned ground
title_full_unstemmed Secondary sorting of sorted patterned ground
title_sort secondary sorting of sorted patterned ground
publisher Wiley
publishDate 1990
url http://dx.doi.org/10.1002/ppp.3430010312
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430010312
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430010312
long_lat ENVELOPE(13.621,13.621,78.063,78.063)
geographic Kapp Linné
geographic_facet Kapp Linné
genre Permafrost and Periglacial Processes
Spitzbergen
genre_facet Permafrost and Periglacial Processes
Spitzbergen
op_source Permafrost and Periglacial Processes
volume 1, issue 3-4, page 313-318
ISSN 1045-6740 1099-1530
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op_doi https://doi.org/10.1002/ppp.3430010312
container_title Permafrost and Periglacial Processes
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