Abstract
Evidence is presented to show that two fundamental rock types, (a) diabase and (b) granite, are present on Pigeon Point and that so-called intermediate rocks associated with them are not true transitional products of magmatic differentiation but are diabases metamorphosed by thermal solutions after complete solidification. Other rocks of unusual appearance are sediments of the Rove formation contact metamorphosed by the granite and later hydro thermally metamorphosed.
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