Exploration Insights Great Geos ebook | Page 58

58 | Great Geologists Dana’s sketch of an erupting Vesuvius, published in 1834. After completing his studies at Yale in 1833, Dana served as a mathematics instructor on a U.S. Navy ship that sailed to the Mediterranean. There, he saw Mount Vesuvius in eruption and sent a report back to Silliman. This report would form the basis for the first paper published by Dana in 1834. In this same year, Dana returned to Yale to take up teaching and research duties. His first objective was mineralogy. Silliman had an extensive collection of minerals which Dana could supplement with his own specimens, some collected when a child. Using this material, Dana set about developing a new mineral classification based on chemistry and crystallography. His results were published as System of Mineralogy when he was just 24. This remarkable work has formed the basis of modern mineralogical studies ever since. Reminiscent of the opportunity afforded to Charles Darwin to sail on the Beagle, in 1838 Dana was offered the opportunity to serve as the geologist and mineralogist of the U.S. Exploring Expedition (1838–1842). For American science, this expedition was without precedent. A fleet of six ships was charged with charting islands in the Pacific, exploring the South American coast and even venturing towards Antarctica. The expedition was substantially funded by the U.S. Navy; and in addition to Dana, there were specialists in botany, vertebrate and invertebrate zoology and philology on board, plus two artists. For Dana, the voyage was not always comfortable (“naval servitude” as he remarked in a letter). The expedition captain had a volatile temperament, and there were the hazards of any voyage in difficult waters. Dana’s ship was almost lost in the Straits of Magellan, and aggressive natives made work difficult in Fiji. Nonetheless, he explored the Andes, the atolls of the Pacific and the active volcanoes in Hawaii. Thus, the expedition gave Dana the chance to experience geology on a global scale, which impacted his geological thinking for the rest of his life. On his return to Yale, Dana’s observations were summarised