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The Liassic Succession in a Clay Pit at Kirton in Lindsey, North Lincolnshire

Published online by Cambridge University Press:  01 May 2009

M. K. Howarth  and
P. F. Rawson
M. K. Howarth
Affiliation:
British Museum (Natural History), Cromwell Road, London, S.W. 7.
P. F. Rawson
Affiliation:
Department of Geology, The University, Hull.
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Abstract

A new clay pit at Kirton in Lindsey, Lincolnshire, gives continuous exposures of 21 feet of clays and limestone nodules of the davoei Zone at the top of the Lower Lias, 18 feet of similar beds and 8 feet of Marlstone Rock Bed belonging to the Middle Lias, and 38 feet of shales and limestones of the tenuicostatum and falciferum Zones of the Upper Lias. Liparoceratid, Amaltheid, Dactylioceratid and Hildoceratid ammonites occur and allow the zones to be delimited with some accuracy.

Type
Articles
Information
Geological Magazine , Volume 102 , Issue 3 , June 1965 , pp. 261 - 266
Copyright
Copyright © Cambridge University Press 1965

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References

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