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Image source: Scrope, George Poulett (1797-1876). Memoir on the geology of central France; including the volcanic formations of Auvergne, the Velay, and the Vivarais. London: Printed for Longman, Rees, Orme, Brown, and Green, 1827

Vulcan's Forge and Fingal's Cave

Volcanoes, Basalt, and the Discovery of Geological Time

Keir, Basalt, and Cooling Glass, 1776

Keir, James (1735-1820). "On the Crystallizations Observed on Glass." Philosophical Transactions of the Royal Society of London, 1776, 66:530-542.

James Keir was not a geologist but a well-known chemist, who moved in an intellectual circle known as the Lunar Society that included James Watt and Matthew Boulton, of steam-engine fame, and Josiah Wedgwood, the maker of porcelain. In experiments with molten glass, Keir discovered that if glass were cooled very slowly, it did not assume a glassy structure, but instead became crystalline, very much like fine-grained basalt. In this paper of 1776, he suggested that perhaps he had discovered evidence that basalt was an igneous rock, and then made a remarkable intellectual leap, by suggesting that the basalt of the Giant’s Causeway was the product of a volcano.

Smith 1969, “Porcelain and Plutonism;” Stokes 1971, “Volcanic Studies by Members of the Royal Society of London, 1665-1780,” p. 63; Newcomb 1990, “Contributions of British Experimentalists to the Discipline of Geology, 1780-1820;” Scott, E.L., “Keir, James,” in DSB 7:277-278.

Keir’s paper, presenting new basalt evidence. Image source: Keir, James (1735-1820). "On the Crystallizations Observed on Glass." Philosophical Transactions of the Royal Society of London, vol. 66, 1776, p. 539.

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