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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

Vesuvius Erupts, 1767

Torre, Giovanni Maria della (1713-1782). Incendio del Vesuvio accaduto li 19 d’ottobre del 1767. Naples: Nella Stamperia, e a spese di Donato Campo, 1767.

The eruption of Vesuvius of 1767 had two great witnesses, Sir William Hamilton (see exhibit item 11), and Giovanni Maria della Torre. Della Torre is of interest because he subscribed to a recent theory of volcanic action which claimed that eruptions were caused by the effervescence of pyrites, or sulphur compounds. In 1700 the chemist Nicholas Lemery had performed a famous experiment, in which he added water to a model mountain that contained pyrites, and the result was a flaming mini-volcano. Della Torre and a number of other eighteenth-century vulcanologists found this to be an attractive explanation of volcanic action.

Nazzaro 1995, “Vesuvius and the Volcanologists, 1734-1860,” pp. 130-131; Franceschini, Pietro, “Della Torre, Giovanni Maria,” in DSB 4:25-26.

Eruption of Vesuvius in 1767. Image source: Torre, Giovanni Maria della. Incendio del Vesuvio accaduto li 19 d’ottobre del 1767. Naples: Nella Stamperia, e a spese di Donato Campo, 1767, pl. 1.

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