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- W2014133367 abstract "In several late papers on the carboniferous rocks of Nova Scotia, reference has been made to a deposit of red sandstone skirting the shores of Cobequid Bay, and resting unconformably on strata of the carboniferous system. I propose in the present paper, to describe this formation as it occurs in the above-named locality, and in other parts of the country bordering the southern arm of the Bay of Fundy, retaining provisionally the name of New Red Sandstone, which is at least locally appropriate. The new red sandstone of Nova Scotia has already been described by Messrs. Jackson and Alger, and by Dr. Gesner. The attention of these geologists was however directed rather to the structure of the trap, and to the numerous crystallized minerals which it contains, than to the geological relations of the deposit; and they did not distinguish it from a group of sandstones, with beds of limestone and gypsum, occurring in its vicinity, which has since been shown by Mr. Lyell to belong to the carboniferous system." @default.
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- W2014133367 date "1848-02-01" @default.
- W2014133367 modified "2023-10-14" @default.
- W2014133367 title "On the New Red Sandstone of Nova Scotia" @default.
- W2014133367 doi "https://doi.org/10.1144/gsl.jgs.1848.004.01-02.15" @default.
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