Neptunism in the context of "Facies"

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👉 Neptunism in the context of Facies

In geology, a facies (/ˈfʃɪ.z/ FAY-shih-eez, US also /ˈfʃz/ FAY-sheez; same pronunciation and spelling in the plural) is a body of rock with distinctive characteristics. The characteristics can be any observable attribute of rocks (such as their overall appearance, composition, or condition of formation) and the changes that may occur in those attributes over a geographic area. A facies encompasses all the characteristics of a rock including its chemical, physical, and biological features that distinguish it from adjacent rock.

The term "facies" was introduced by the Swiss geologist Amanz Gressly in 1838 and was part of his significant contribution to the foundations of modern stratigraphy, which replaced the earlier notions of Neptunism.

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Neptunism in the context of Abraham Gottlob Werner

Abraham Gottlob Werner (German: [ˈaːbʁaham ˈɡɔtloːp ˈvɛʁnɐ]; 25 September 1749 – 30 June 1817) was a German geologist who set out an early theory about the stratification of the Earth's crust and propounded a history of the Earth that came to be known as Neptunism. While most tenets of Neptunism were eventually set aside, Werner is remembered for his demonstration of chronological succession in rocks; for the zeal with which he infused his pupils; and for the impulse he thereby gave to the study of geology. He has been called the "father of German geology".

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