On the Early Pebble Gravels of the Thames Basin from the Hertfordshire-Essex Border to Clacton-on-Sea

Abstract The erratic rocks of the early pebble gravels are similar to those of the Oxford plateau drift, and reasons are given for concluding that they belong to the drifts of the proto-Thames, and are earlier than the southward diversion of that river by an advancing ice-sheet. Comparisons with the...

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Bibliographic Details
Published in:Geological Magazine
Main Author: Warren, S. Hazzledine
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1957
Subjects:
Geology
Ice Sheet
Online Access:http://dx.doi.org/10.1017/s001675680006828x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S001675680006828X
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spelling crcambridgeupr:10.1017/s001675680006828x 2024-03-03T08:45:25+00:00 On the Early Pebble Gravels of the Thames Basin from the Hertfordshire-Essex Border to Clacton-on-Sea Warren, S. Hazzledine 1957 http://dx.doi.org/10.1017/s001675680006828x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S001675680006828X en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 94, issue 1, page 40-46 ISSN 0016-7568 1469-5081 Geology journal-article 1957 crcambridgeupr https://doi.org/10.1017/s001675680006828x 2024-02-08T08:46:23Z Abstract The erratic rocks of the early pebble gravels are similar to those of the Oxford plateau drift, and reasons are given for concluding that they belong to the drifts of the proto-Thames, and are earlier than the southward diversion of that river by an advancing ice-sheet. Comparisons with the constituents of the later deposits of the Clacton channel are also discussed. Article in Journal/Newspaper Ice Sheet Cambridge University Press Geological Magazine 94 1 40 46
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
spellingShingle Geology
Warren, S. Hazzledine
On the Early Pebble Gravels of the Thames Basin from the Hertfordshire-Essex Border to Clacton-on-Sea
topic_facet Geology
description Abstract The erratic rocks of the early pebble gravels are similar to those of the Oxford plateau drift, and reasons are given for concluding that they belong to the drifts of the proto-Thames, and are earlier than the southward diversion of that river by an advancing ice-sheet. Comparisons with the constituents of the later deposits of the Clacton channel are also discussed.
format Article in Journal/Newspaper
author Warren, S. Hazzledine
author_facet Warren, S. Hazzledine
author_sort Warren, S. Hazzledine
title On the Early Pebble Gravels of the Thames Basin from the Hertfordshire-Essex Border to Clacton-on-Sea
title_short On the Early Pebble Gravels of the Thames Basin from the Hertfordshire-Essex Border to Clacton-on-Sea
title_full On the Early Pebble Gravels of the Thames Basin from the Hertfordshire-Essex Border to Clacton-on-Sea
title_fullStr On the Early Pebble Gravels of the Thames Basin from the Hertfordshire-Essex Border to Clacton-on-Sea
title_full_unstemmed On the Early Pebble Gravels of the Thames Basin from the Hertfordshire-Essex Border to Clacton-on-Sea
title_sort on the early pebble gravels of the thames basin from the hertfordshire-essex border to clacton-on-sea
publisher Cambridge University Press (CUP)
publishDate 1957
url http://dx.doi.org/10.1017/s001675680006828x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S001675680006828X
genre Ice Sheet
genre_facet Ice Sheet
op_source Geological Magazine
volume 94, issue 1, page 40-46
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s001675680006828x
container_title Geological Magazine
container_volume 94
container_issue 1
container_start_page 40
op_container_end_page 46
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