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Adam Sedgwick

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English geologist (1785–1873)

Key facts

Born
( 1785-03-22 ) 22 March 1785, Dent , Yorkshire , England
Died
27 January 1873 (1873-01-27) (aged 87), Cambridge , England
Alma mater
Trinity College, Cambridge
Known for
Classification of Cambrian rocks ; opposition to evolution and natural selection
Awards
Wollaston Medal (1833), Copley Medal (1863)
Fields
Geology
Institutions
Trinity College, Cambridge
Academic advisors
Thomas Jones , John Dawson
Notable students
George Peacock , William Hopkins , Charles Darwin , Joseph Jukes

via Wikipedia infobox

Wikidata facts

Instance of
human
Given name
Adam
Gender
male
Place of birth
Dent
Place of death
Cambridge
Languages spoken
English language
Religion
Anglicanism
Doctoral advisor
John Dawson
Student of
John Dawson
Doctoral student
William Hopkins
Field of work
geology
Image
Adam Sedgwick.jpg
Residence
England
Show 9 more facts
name in native language
Adam Sedgwick
described by source
The Nuttall Encyclopædia
date of birth
1785-03-22
date of death
1873-01-27
Commons gallery
Adam Sedgwick
Commons category
Adam Sedgwick
different from
Adam Sedgwick
Sources (4)

via Wikidata · CC0

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Encyclopedic overview

Adam Sedgwick FRS (/ˈsɛdʒwɪk/; 22 March 1785 – 27 January 1873) was a British geologist and Anglican priest, one of the founders of modern geology. He proposed the Cambrian and Devonian period of the geological timescale. Based on work which he did on Welsh rock strata, he proposed the Cambrian period in 1835, in a joint publication in which Roderick Murchison also proposed the Silurian period. Later in 1840, to resolve what later became known as the Great Devonian Controversy about rocks near the boundary between the Silurian and Carboniferous periods, he and Murchison proposed the Devonian period.

Though he had guided the young Charles Darwin in his early study of geology and continued to be on friendly terms, Sedgwick was an opponent of Darwin's theory of evolution by means of natural selection.

Excerpted from Wikipedia’s “Adam Sedgwick” article, available under the CC BY-SA 4.0 licence.