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.

Bibliographic Details
Published in:Geological Magazine
Main Authors: Fisher, P., Rolls, J. D.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1982
Subjects:
Geology
Thermokarst
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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spelling 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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