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geologist : ウィキペディア英語版
geologist

A geologist is a scientist who studies the solid and liquid matter that constitutes the Earth as well as the processes and history that have shaped it. Geologists usually engage in studying geology. Geologists, studying more of an applied science than a theoretical one, must approach Geology using physics, chemistry and biology as well as other sciences. Geologists, compared to scientists engaged in other fields, are generally more exposed to the outdoors than staying in laboratories; although some geologists prefer to perform most of their studies in the lab. A geologists tool used for exploring are pickaxes, gloves, glasses, mining tools and a magnifying glass.
Geologists are engaged in exploration for mining companies in search of metals, oils, and other Earth resources. They are also in the forefront of natural hazards and disasters warning and mitigation, studying earthquakes, volcanic activity, tsunamis, weather storms, and the like; their studies are used to warn the general public of the occurrence of these events. Currently, geologists are also engaged in the discussion of climate change, as they study the history and evidence for this Earth process.
==History==

James Hutton is often viewed as the first modern geologist.〔(James Hutton: The Founder of Modern Geology ), American Museum of Natural History〕 In 1785 he presented a paper entitled ''Theory of the Earth'' to the Royal Society of Edinburgh. In his paper, he explained his theory that the Earth must be much older than had previously been supposed in order to allow enough time for mountains to be eroded and for sediments to form new rocks at the bottom of the sea, which in turn were raised up to become dry land. Hutton published a two-volume version of his ideas in 1795 ((Vol. 1 ), (Vol. 2 )).
Followers of Hutton were known as ''Plutonists'' because they believed that some rocks were formed by ''vulcanism'', which is the deposition of lava from volcanoes, as opposed to the ''Neptunists'', led by Abraham Werner, who believed that all rocks had settled out of a large ocean whose level gradually dropped over time.
The first geological map of the U.S. was produced in 1809 by William Maclure.〔(【引用サイトリンク】title=Title Page: Observations on the geology of the United States of America. )〕 In 1807, Maclure commenced the self-imposed task of making a geological survey of the United States. Almost every state in the Union was traversed and mapped by him; the Allegheny Mountains being crossed and recrossed some 50 times.〔Page 39 in Greene, J.C. and Burke, J.G. (1978) The Science of Minerals in the Age of Jefferson. Transactions of the American Philosophical Society, New Series, Vol. 68, No. 4,pp. 1-113〕 The results of his unaided labours were submitted to the American Philosophical Society in a memoir entitled ''Observations on the Geology of the United States explanatory of a Geological Map'', and published in the ''Society's Transactions'', together with the nation's first geological map.〔(【引用サイトリンク】title=Map of the United States of America. )〕 This antedates William Smith's geological map of England by six years, although it was constructed using a different classification of rocks.
Sir Charles Lyell first published his famous book, ''Principles of Geology'', in 1830. This book, which influenced the thought of Charles Darwin, successfully promoted the doctrine of uniformitarianism. This theory states that slow geological processes have occurred throughout the Earth's history and are still occurring today. In contrast, catastrophism is the theory that Earth's features formed in single, catastrophic events and remained unchanged thereafter. Though Hutton believed in uniformitarianism, the idea was not widely accepted at the time.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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