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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, 1738

Reale Accademia delle Scienze Fisiche e Matematiche di Napoli. Istoria dell’ incendio del Vesuvio accaduto nel mese di maggio dell’anno MDCCXXXVI. Naples: Nella stamperia di Novello de Bonis, 1738.

Francesco Serao (1702-1785), who wrote this description of the eruption of Vesuvius of 1737, was a professor of medicine at the University in Naples. He believed that volcanoes did not spew forth "fire and brimstone," but rather that the lava they produced consisted of sand and earth that had been melted by the volcanic fire and converted to a glass-like material. He also argued that Vesuvius had looked different in the past. In his time Vesuvius consisted of a volcanically active peak, surrounded by a half-ring called Mount Somma. Serao pointed out that if Vesuvius had always had this structure, it was difficult to explain the locations of some lava flows on the other side of Mount Somma.

Nazzaro 1995, “Vesuvius and the volcanologists, 1734-1860,” pp. 132-133.

Engraving of Vesuvius. Image source: Reale Accademia delle Scienze Fisiche e Matematiche di Napoli. Istoria dell’ incendio del Vesuvio accaduto nel mese di maggio dell’anno MDCCXXXVI. Naples: Nella stamperia di Novello de Bonis, 1738, pl. 1.

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