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ABRAHAM GOTTLOB WERNER (1750-1817)

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Originally appearing in Volume V28, Page 523 of the 1911 Encyclopedia Britannica.
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ABRAHAM GOTTLOB WERNER (1750-1817)  ,
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father of German geology, was born in Upper Lusatia, Saxony, on the 25th of September 1750 . The
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family to which he belonged had been engaged for several
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hundred years in
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mining pursuits . His father was inspector of Count Solm's iron-
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works at Wehrau and Lorzendorf, and from young Werner's
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infancy cultivated in him a taste for minerals and rocks . The boy showed early promise of distinction . He began to collect specimens of stones, and one cf his favourite employments was to
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pore over the pages of a
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dictionary of mining . At the age of nine he was sent to school at
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Bunzlau in
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Silesia, where he remained until 1764, when he joined his father at Wehrau with the idea of ultimately succeeding him in the
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post of inspector . When nineteen years of age (1769) he journeyed to Freiberg, where he attracted the
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notice of the officials, who invited him to attend the mining school established two years previously . This was the turning point in Werner's career . He soon distinguished himself by his industry and by the large amount of
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practical knowledge of
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mineralogy which he acquired . In 1771 he repaired to theuniversity of
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Leipzig and went through the usual curriculum of study, paying attention at first chiefly to the subject of law, but continuing to devote himself with
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great ardour to mineralogical pursuits . While still a student he wrote his first
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work on the
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external characters of minerals, Von den etusserlichen Kennzeichen der Fossilien (1774), which at once gave him a name among the mineralogists of the day . In 1775 he was appointed inspector in the mining school and teacher of mineralogy at Freiberg .

To the development of that school and to the cultivation of mineralogy and geognosy he thence-forth, for about

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forty years, devoted the whole of his active and indefatigable industry . From a mere provincial institution the Freiberg academy under his care rose to be one of the great centres of scientific
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light in
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Europe, to which students from all parts of the
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world flocked to listen to his eloquent teaching . He wrote but little, and though he elaborated a
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complete
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system of geognosy and mineralogy he never could be induced to publish it . From the notes of his pupils, however, the general purport of his teaching was well known, and it widely influenced the science of his time . He died at Freiberg on the 3oth of
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June 1817 . One of the distinguishing features of Werner's teaching was the care with which he taught lithology and the succession of
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geological formation; a subject to which he applied the name geognosy . His views on a definite geological succession were inspired by the works of J . G . Lehmann and G . C . Fuchsel (1722-1773) . He showed that the rocks of the earth are not disposed at random, but follow each other in a certain definite order .

Unfortunately he had never enlarged his experience by travel, and the sequence of

rock-masses which he had recognized in Saxony was believed by him to be of universal application (see his Kurze Klassifikation and Beschreibung der verschiedenen Gebirgsarten, 1787) . He taught that the rocks were the precipitates of a primeval ocean, and followed each other in successive deposits of world-wide extent . Volcanoes were regarded by him as abnormal phenomena, probably due to the combustion of subterranean beds of
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coal .
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Basalt and similar rocks, which even then were recognized by other observers as of igneous origin, were believed by him to be
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water-formed accumulations of the same ancient ocean . Hence arose one of the great
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historical controversies of geology . Werner's followers preached the
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doctrine of the aqueous origin of rocks, and were known as Neptunists; their opponents, who recognized the important
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part taken in the construction of the earth's crust by subterranean heat, were styled Vulcanists . R . Jameson, the most distinguished of his
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British pupils, was for many years an ardent teacher of the Wernerian doctrines . Though much of Werner's theoretical work was erroneous, science is indebted to him for so clearly demonstrating the
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chronological succession of rocks, for the enthusiastic zeal which he infused into his pupils, and for the impulse which he thereby gave to the study of geology . See S . G . Frisch, Lebensbeschreibung A .

G . Werners (Leipzig, 1825) ;

Cuvier, Eloge de Werner; Lyell, Principles of Geology; and
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Sir A . Geikie, Founders of Geology (1897; 2nd ed., 1906) .

End of Article: ABRAHAM GOTTLOB WERNER (1750-1817)
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