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- W2153775657 abstract "The Strait of Canseau is a narrow passage fourteen miles in length, separating Nova Scotia proper from Cape Breton Island. On the Nova Scotia side it affords an imperfect section of carboniferous strata, interrupted near the middle of the Strait by a mass of reddish syenite and disturbed slates, forming the promontory of Cape Porcupine, which is the abrupt termination of a hilly range extending far into Nova Scotia. On the Cape Breton side, the section exhibits carboniferous rocks; and nearly opposite Cape Porcupine is the small indentation, whose name of Plaister Cove is derived from the mass of gypsum to which the following remarks refer.The gypsum of Plaister Cove, like other large masses of that rock occurring in this province, belongs to the lower part of the carboniferous system, and is associated with limestone and marls. The structure and accompaniments of the bed are, however, more perfectly exposed than in most of the larger masses of gypsum which I have examined. For this reason I shall endeavour, with the aid of the accompanying section fig. 1, and specimens, to give a somewhat detailed view of the appearances presented at this place, with the object of recording facts which may be useful in explaining the origin of the great beds of gypsum.(1). At McMillan's Point, about three-quarters of a mile north of the Cove, are thick beds of grey conglomerate, in a vertical position. These beds form the base of the carboniferous system in this district; and, at" @default.
- W2153775657 created "2016-06-24" @default.
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- W2153775657 date "1849-02-01" @default.
- W2153775657 modified "2023-09-27" @default.
- W2153775657 title "Notice of the Gypsum of Plaister Cove in the Strait of Canseau" @default.
- W2153775657 doi "https://doi.org/10.1144/gsl.jgs.1849.005.01-02.34" @default.
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