Large Scale Patterned Ground in the Valley of the Worcestershire Avon
Abstract Crop markings reveal a polygonal network resembling that of “patterned ground” in arctic Alaska. From this the former presence of perennially frozen ground is inferred, with the implication that the mean annual isotherm of this part of Worcestershire was at least 13½ ° C. lower than it is a...
Published in: | Geological Magazine |
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Language: | English |
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Cambridge University Press (CUP)
1960
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Online Access: | http://dx.doi.org/10.1017/s0016756800061756 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800061756 |
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crcambridgeupr:10.1017/s0016756800061756 2024-09-09T19:22:46+00:00 Large Scale Patterned Ground in the Valley of the Worcestershire Avon Shotton, F. W. 1960 http://dx.doi.org/10.1017/s0016756800061756 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800061756 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 97, issue 5, page 404-408 ISSN 0016-7568 1469-5081 journal-article 1960 crcambridgeupr https://doi.org/10.1017/s0016756800061756 2024-07-24T04:03:22Z Abstract Crop markings reveal a polygonal network resembling that of “patterned ground” in arctic Alaska. From this the former presence of perennially frozen ground is inferred, with the implication that the mean annual isotherm of this part of Worcestershire was at least 13½ ° C. lower than it is at present. It is argued that this condition obtained at the period of the Irish Sea Glaciation maximum. Article in Journal/Newspaper Arctic Alaska Cambridge University Press Arctic Geological Magazine 97 5 404 408 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Abstract Crop markings reveal a polygonal network resembling that of “patterned ground” in arctic Alaska. From this the former presence of perennially frozen ground is inferred, with the implication that the mean annual isotherm of this part of Worcestershire was at least 13½ ° C. lower than it is at present. It is argued that this condition obtained at the period of the Irish Sea Glaciation maximum. |
format |
Article in Journal/Newspaper |
author |
Shotton, F. W. |
spellingShingle |
Shotton, F. W. Large Scale Patterned Ground in the Valley of the Worcestershire Avon |
author_facet |
Shotton, F. W. |
author_sort |
Shotton, F. W. |
title |
Large Scale Patterned Ground in the Valley of the Worcestershire Avon |
title_short |
Large Scale Patterned Ground in the Valley of the Worcestershire Avon |
title_full |
Large Scale Patterned Ground in the Valley of the Worcestershire Avon |
title_fullStr |
Large Scale Patterned Ground in the Valley of the Worcestershire Avon |
title_full_unstemmed |
Large Scale Patterned Ground in the Valley of the Worcestershire Avon |
title_sort |
large scale patterned ground in the valley of the worcestershire avon |
publisher |
Cambridge University Press (CUP) |
publishDate |
1960 |
url |
http://dx.doi.org/10.1017/s0016756800061756 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800061756 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Alaska |
genre_facet |
Arctic Alaska |
op_source |
Geological Magazine volume 97, issue 5, page 404-408 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800061756 |
container_title |
Geological Magazine |
container_volume |
97 |
container_issue |
5 |
container_start_page |
404 |
op_container_end_page |
408 |
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1809763103394496512 |