Late Quaternary evolution of the Tees–Swale interfluve east of the Pennines: the role of glaciation in the development of river systems in northern England-Reference-Cited by-同舟云学术

Late Quaternary evolution of the Tees–Swale interfluve east of the Pennines: the role of glaciation in the development of river systems in northern England

Published:2010-01 Issue:4 Volume:121 Page:410-422
ISSN:0016-7878
Container-title:Proceedings of the Geologists' Association
language:en
Short-container-title:Proceedings of the Geologists' Association

Author:

Mitchell W.A.,Bridgland D.R.,Innes J.B.

Publisher

Elsevier BV

Subject

Paleontology,Geology

Reference55 articles.

1. Glacial and post-glacial geology of Middlesbrough and the Tees estuary;Agar;Proceedings of the Yorkshire Geological Society,1954

2. British Regional Geology: The Pennines and Adjacent Areas;Aitkenhead,2002

3. The Tees laminated clays;Bell,1991

4. Westward pro-glacial drainage in Cleveland;Best;Proceedings of the Yorkshire Geological Society,1956

5. Late Quaternary Landscape Evolution of the Swale–Ure Washlands;Bridgland,2010

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