A thermokarst phenomenon on a terrace of the River Wey near Farnham, Surrey, England
Summary Palaeochannels developed in a terrace of the River Wey are described. Their morphology, relationship with the underlying Folkestone Sands, and the character of associated superficial deposits all suggest that the channels are examples of thermokarst phenomena, probably of Devensian age.
Published in: | Geological Magazine |
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Language: | English |
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Cambridge University Press (CUP)
1982
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Online Access: | http://dx.doi.org/10.1017/s0016756800026133 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800026133 |
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crcambridgeupr:10.1017/s0016756800026133 2024-03-03T08:49:08+00:00 A thermokarst phenomenon on a terrace of the River Wey near Farnham, Surrey, England Fisher, P. Rolls, J. D. 1982 http://dx.doi.org/10.1017/s0016756800026133 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800026133 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 119, issue 3, page 315-318 ISSN 0016-7568 1469-5081 Geology journal-article 1982 crcambridgeupr https://doi.org/10.1017/s0016756800026133 2024-02-08T08:42:11Z Summary Palaeochannels developed in a terrace of the River Wey are described. Their morphology, relationship with the underlying Folkestone Sands, and the character of associated superficial deposits all suggest that the channels are examples of thermokarst phenomena, probably of Devensian age. Article in Journal/Newspaper Thermokarst Cambridge University Press Geological Magazine 119 3 315 318 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology |
spellingShingle |
Geology Fisher, P. Rolls, J. D. A thermokarst phenomenon on a terrace of the River Wey near Farnham, Surrey, England |
topic_facet |
Geology |
description |
Summary Palaeochannels developed in a terrace of the River Wey are described. Their morphology, relationship with the underlying Folkestone Sands, and the character of associated superficial deposits all suggest that the channels are examples of thermokarst phenomena, probably of Devensian age. |
format |
Article in Journal/Newspaper |
author |
Fisher, P. Rolls, J. D. |
author_facet |
Fisher, P. Rolls, J. D. |
author_sort |
Fisher, P. |
title |
A thermokarst phenomenon on a terrace of the River Wey near Farnham, Surrey, England |
title_short |
A thermokarst phenomenon on a terrace of the River Wey near Farnham, Surrey, England |
title_full |
A thermokarst phenomenon on a terrace of the River Wey near Farnham, Surrey, England |
title_fullStr |
A thermokarst phenomenon on a terrace of the River Wey near Farnham, Surrey, England |
title_full_unstemmed |
A thermokarst phenomenon on a terrace of the River Wey near Farnham, Surrey, England |
title_sort |
thermokarst phenomenon on a terrace of the river wey near farnham, surrey, england |
publisher |
Cambridge University Press (CUP) |
publishDate |
1982 |
url |
http://dx.doi.org/10.1017/s0016756800026133 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800026133 |
genre |
Thermokarst |
genre_facet |
Thermokarst |
op_source |
Geological Magazine volume 119, issue 3, page 315-318 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800026133 |
container_title |
Geological Magazine |
container_volume |
119 |
container_issue |
3 |
container_start_page |
315 |
op_container_end_page |
318 |
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1792506290757435392 |