Field Notebook: New Brunswick, Nova Scotia, Quebec 1905
Page 118
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Transcription
all of the Grand [illegible] formation. The hills are thus disposed:- Oyster Point S. C. Concava P. foveosulca S. cune dentata There is a very narrow band of beds of this kind. Framing Cape Raine Road The land rises here again into the high sea cliffs as high as the Grand [illegible] hills. These sea cliffs have beds not far which I collected open deep cup Coelospermum Concava and a type of Delmanites. I rather think that this deeper Oolite any limestone lies once down in one probably below the second layer seen on the level at Ship Head. In other words close to the Leptocidella flabellata (very large speci- mens) beds with Michelinia and Ostreacidae.