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Scrivenor, J. B. (1938) Notes on the Geology of the Lizard Peninsula. No 3. The Epidote Bands, Lenticles, and Veins. Geological Magazine, 75 (11) 515-526 doi:10.1017/s0016756800091974

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Reference TypeJournal (article/letter/editorial)
TitleNotes on the Geology of the Lizard Peninsula. No 3. The Epidote Bands, Lenticles, and Veins
JournalGeological Magazine
AuthorsScrivenor, J. B.Author
Year1938 (November)Volume75
Page(s)515-526Issue11
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800091974
Mindat Ref. ID246864Long-form Identifiermindat:1:5:246864:2
GUIDbc7e0825-f43f-4523-bcec-41d75a1439a2
Full ReferenceScrivenor, J. B. (1938) Notes on the Geology of the Lizard Peninsula. No 3. The Epidote Bands, Lenticles, and Veins. Geological Magazine, 75 (11) 515-526 doi:10.1017/s0016756800091974
Plain TextScrivenor, J. B. (1938) Notes on the Geology of the Lizard Peninsula. No 3. The Epidote Bands, Lenticles, and Veins. Geological Magazine, 75 (11) 515-526 doi:10.1017/s0016756800091974
In(1938, November) Geological Magazine Vol. 75 (11) Cambridge University Press (CUP)
Abstract/NotesA striking feature of the geology of the Lizard is the occurrence of rocks very rich in, or consisting entirely of epidote; as bands parallel to the foliation of the hornblende-gneiss and the green schists of the Old Lizard Head Series; as lenticles caused by local enlargement of those bands; and sometimes as veins cutting the foliation, for instance on Polurrian Beach. The coast-sections at Mullion do not show great development of these epidotic rocks in the hornblende-gneiss but bands one inch thick occur. At Porthallow and north of Porthoustock there is an even smaller development of these rocks, but along the coast from Pentreath Beach southwards round Lizard Point to Cadgwith epidote bands and lenticles are abundant. Sir John Flett remarks in the 1912 Memoir (p. 50) on the perfection of this banding, “which cannot be paralleled anywhere else in Britain,” but he has told me that in Anglesey epidotic rocks approach them in abundance. These Anglesey rocks were described by Dr. E. Greenly in the Survey Memoir of that area (1919, pp. 108 and 109 inter alia).

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Howard (1888) Quart. Journ. Geol. Soc. The Gneissic Rocks off the Lizard xliv, 309


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