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Journal article

Lithospheric flexure, uplift, and landscape evolution in south-central England

Abstract:

The high level river gravels in Oxfordshire (the Northern Drift Group), which range in age from Early Pleistocene to around 450 ka, contain pebbles that were derived from a source area to the north near Birmingham. The pebbles could not have been transported across the Upper Triassic and Lower Jurassic clay outcrops of the Midlands unless the region was at or close to sea level. The present day Cotswold escarpment ranges from 70 to 215 m: this uplift must therefore have occurred after deposit...

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Publication status:
Published

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Publisher copy:
10.1144/jgs.157.6.1169

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
Journal:
JOURNAL OF THE GEOLOGICAL SOCIETY
Volume:
157
Issue:
6
Pages:
1169-1177
Publication date:
2000-11-01
DOI:
EISSN:
2041-479X
ISSN:
0016-7649
Language:
English
Keywords:
Pubs id:
pubs:82246
UUID:
uuid:c821822f-bdd3-41c8-860e-6ce25bba0020
Local pid:
pubs:82246
Source identifiers:
82246
Deposit date:
2012-12-19

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