Scientific American Supplement, No. 829, November 21, 1891 by Various
page 21 of 146 (14%)
page 21 of 146 (14%)
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contains. A range of limestone rock 100 miles in length by 10 miles in
width, and 1,000 yards in depth, would contain 743,000 million tons of carbon, or sufficient to provide carbon for 875,000 million tons of petroleum. Deposits of oil-bearing shale have also limestone close at hand; e.g., coral rag underlies Kimmeridge clay, as it also underlies the famous black shale in Kentucky, which is extraordinarily rich in oil. II. As evidence of volcanic action in close proximity to petroleum strata, the mud volcanoes at Baku and in Burma are described, and a sulphur mine in Spain is mentioned (with which the writer is well acquainted), situated near an extinct volcano, where a perpetual gas flame in a neighboring chapel and other symptoms indicate that petroleum is not far off. While engaged in studying the geological conditions of this mine, the author observed that Dr. Christoff Bischoff records in his writings that he had produced sulphur in his own laboratory by passing hot volcanic gases through chalk, which, when expressed in a chemical formula, leads at once to the postulate that, in addition to sulphur, _ethylene_, and all its homologues (C_{n}H_{2n}), which are the oils predominating at Baku, would be produced by treating: 2, 3, 4, 5 equivs. of carbonate of lime (limestone) with 2, 3, 4, 5 " sulphurous acid (SO_{2}) and 4, 6, 8, 10 " sulphureted hydrogen (H_{2}S); and that marsh gas and its homologues, which are the oils predominating in Pennsylvania, would be produced by treating: 1, 2, 3, 4, 5 equivs. of carbonate of lime with |
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