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A Llandovery Conglomeratic Limestone in Gullet Quarry, Malvern Hills, and its Conodont Fauna

Published online by Cambridge University Press:  01 May 2009

M. Brooks  and
E. C. Druce
M. Brooks
Affiliation:
Department of Geology, University College of Swansea, Swansea, Wales.
E. C. Druce
Affiliation:
Department of Geology, University College of Swansea, Swansea, Wales.
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Abstract

A conglomerate band exposed in Gullet Quarry, at the southern end of the Malvern Hills, contains a layer of shelly limestone in which are embedded large, often angular, boulders of Malyernian rock. The character of the limestone and the form and distribution of included boulders suggest that a near-shore environment of carbonate deposition was continually supplied with clastic material from adjacent sea-stacks. The limestone has yielded a conodont fauna indicative of a Llandovery age earlier than that assigned to the conglomerate by Reading and Poole (1961) on the basis of brachiopod evidence.

Type
Articles
Information
Geological Magazine , Volume 102 , Issue 5 , October 1965 , pp. 370 - 382
Copyright
Copyright © Cambridge University Press 1965

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