An Account of the Basalts of Saxony: With Observations on the Origin of Basalt in General [Paperback]

This 1803 paper by a student of Abraham Werner provides a fascinating example of the arguments of nineteenth-century Neptunists.This detailed and carefully argued essay attempts to prove the Neptunist theory of basalt formation. Now discredited, and rejected by Daubuisson later in his career, Neptunism was nevertheless influential into the early nineteenth century, and this 1814 translation provides a fascinating example of the arguments of its proponents.This detailed and carefully argued essay attempts to prove the Neptunist theory of basalt formation. Now discredited, and rejected by Daubuisson later in his career, Neptunism was nevertheless influential into the early nineteenth century, and this 1814 translation provides a fascinating example of the arguments of its proponents.Jean-Fran?ois Daubuisson (17691841), geologist and engineer, was an Officer of the L?gion d'Honneur, Knight of St Louis and Chief Engineer at the Royal Mining Corps. He published numerous papers on geology, mining and hydraulics, and is best known for his textbooks, Trait? de G?ognosie and Trait? d'Hydraulique. He studied geology and mineralogy in Freiburg with Abraham Werner, the key proponent of Neptunism, the theory that all rocks had an aqueous origin. Later in his career Daubuisson was to side with the Plutonists, who argued that basalts formed from molten rock. However, in this paper, published in French in 1803, he describes his observations of the basalts of Saxony and argues that they, and all basalts, are sedimentary. This English translation by the Secretary of the Wernerian Natural History Society was published in 1814, and provides a fascinating insight into this discredited but once influential theory of the Earth.Preface by the translator; Introduction; 1. Preliminary definitions; 2. Of the basalts of Saxony; 3. Inferences respecting the formation of the basalts of Saxony; 4. Proofs that the basaltic rocks of Saxony are not of volcanic origin; Observations on the origin of lT