Abstract
The Charmouth district, situated in the south-west corner of Dorsetshire, consists of valleys in the Lias clays, separated by hills which are capped by Upper Cretaceous rocks, resting unconformably upon the Lias. Black Ven is the name of the cliff face bisecting one of these hills, which, lying between Charmouth and Lyme Regis, divides the valleys of the Char and the Lyme stream. of this cliff, the lower 350 feet consist of Lias clays and limestones.
Publisher
Cambridge University Press (CUP)
Cited by
3 articles.
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1. William Dickson Lang, 1878-1966;Biographical Memoirs of Fellows of the Royal Society;1966-11
2. The geology of the Charmouth cliffs, beach and fore-shore;Proceedings of the Geologists' Association;1914-01
3. Excursion to Lyme Regis, Easter, 1906;Proceedings of the Geologists' Association;1906-01