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Arthur Holmes

 
Scientist: Arthur Holmes

British geologist (1890–1965)

Holmes came from a farming background in Hebburn-on-Tyne in the northeast of England. He graduated from Imperial College, London, in 1910, and went on to work with Lord Rayleigh on radioactivity. After an expedition to Mozambique in 1911 he taught at Imperial College until 1920 when he went to Burma as an oil geologist. In 1925 he returned to England to become professor of geology at Durham University, where he remained until 1943 when he moved to Edinburgh University.

Holmes conducted major work on the use of radioactive techniques to determine the age of rocks, leading to his proposal of the first quantitative geological time scale in 1913 and to his estimate of the age of the Earth being about 1600 million years. He continued to revise this estimate throughout his life, producing a figure in 1959 some three times larger.

Holmes also made a major contribution to the theory of continental drift proposed by Alfred Wegener in 1915. One of the early difficulties the theory faced was that geologists could not envisage a force capable of moving the continents in the way described by Wegener. In 1929 Holmes proposed the existence of convection currents in the Earth's mantle. Rocks in the Earth's interior are, according to Holmes, heated by radioactivity, causing them to rise and spread out and, when cold and dense, to sink back to the interior. It was only after World War II that hard evidence for such a view could be produced.

In 1944 Holmes published his Principles of Physical Geology, a major work on the subject. A substantially revised edition of this book was published in 1965, shortly before Holmes's death.

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Biography: Arthur Holmes
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The English geologist Arthur Holmes (1890-1965) was a pioneer in geochronology, a gifted petrologist, and a lucid expositor of the physics and history of the earth's outer layers.

Arthur Holmes was born on Jan. 14, 1890, at Heb-burn-on-Tyne. At school he became interested in the age of the earth through reading Lord Kelvin's Addresses. Winning a scholarship to London's Imperial College, he graduated in geology and physics in 1911 and immediately began research on the radioactivity of rocks, guided by R. J. Strutt (later 4th Baron Rayleigh). Strutt's studies had revealed a source of heat within the earth, unsuspected when Kelvin made his estimate that not more than 40 million years had elapsed since the earth's crust had solidified from the molten state. Holmes shared with Strutt in overthrowing this conclusion, and he made successive advances toward establishing a new and much longer geological time scale, eventually showing the earth to be at least 4.5 billion years old.

Holmes's researches were twice interrupted by participation as geologist in commercial explorations, first in Mozambique (1911-1912), where he contracted tropical diseases which precluded military service in World War I, and in Burma (1921-1924); the latter expedition failed, and he had to sue for his pay on return to England.

Holmes was demonstrator in geology at the Imperial College from 1912 to 1921, where he wrote three books and published many scientific memoirs. From 1924 to 1943 he headed the geology department of Durham University, which gained international fame as a center of petrological research. He was regius professor of geology and mineralogy at the University of Edinburgh from 1943 until his retirement, in poor health, in 1956. While at Durham his wife died in 1938; in 1939 he married the distinguished petrologist Doris L. Reynolds, with whom he made important researches on the evolution of igneous rock.

Holmes's work touched nearly all aspects of geology except paleontology. His geological researches were widespread, concerning India, Mozambique, and elsewhere in Africa, besides his native Britain. His textbook Principles of Physical Geology (1944; 2d ed. 1965) is considered a classic. Though a man of quiet demeanor, whose main outside interest was music, he did not shrink from the controversies that have figured so notably in the history of his science. He was one of the earliest and most forceful supporters of the theory of continental drift and held that it must be produced by convection currents in the substratum of the crust. In his textbook Holmes gives some diagrams describing the formation of new ocean floor by rising materials - diagrams which are almost prophetic in their anticipation of later results. He died, after a prolonged illness, in London on Sept. 20, 1965.

Further Reading

Information on Arthur Holmes can be found in W. B. Harland, A. Gilbert Smith, and B. Wilcock, eds., The Phanerozoic Time-Scale (1964).

WordNet: Arthur Holmes
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Note: click on a word meaning below to see its connections and related words.

The noun has one meaning:

Meaning #1: English geologist and supporter of the theory of continental drift (1890-1965)
  Synonym: Holmes


Wikipedia: Arthur Holmes
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Arthur Holmes (14 January 1890 – 20 September 1965) was a British geologist. As a child he lived in Low Fell, Gateshead and attended the Gateshead Higher Grade School (later Gateshead Grammar School).[1]

Holmes was a pioneer of geochronology, and performed the first uranium-lead radiometric dating (specifically designed to measure the age of a rock) while an undergraduate at the Royal College of Science (now Imperial College) in London, assigning an age of 370 Ma to a Devonian rock from Norway. This result was published in 1911,[2] after his graduation in 1910. By 1911 he had already spent six months in Mozambique prospecting for minerals. While abroad he had contracted blackwater fever and malaria so severe that a note of his death was sent home by telegraph. However, he returned home and recovered – though suffering life-long recurrences of the illness.

1912 saw Holmes on the staff of Imperial College, publishing his famous booklet The Age of the Earth in 1913 ( he estimated the Earth's age to be 1600 Ma). He obtained his doctorate (of Science) in 1917 and in 1920 joined an oil company in Burma as chief geologist. The company failed, and he returned to England penniless in 1924. He had been accompanied in Burma by his three-year-old son, who contracted dysentery and died shortly before Holmes’s departure.

In 1924 he was appointed to the newly-created post of reader in geology at Durham University. Eighteen years later his achievements were recognised, when he became a Fellow of the Royal Society in 1942. In the following year he was appointed to the chair of geology at Edinburgh University, which he held until retirement in 1956.

Holmes championed the theory of continental drift at a time when it was deeply unfashionable. He proposed that Earth's mantle contained convection cells that dissipated radioactive heat and moved the crust at the surface. His second famous book Principles of Physical Geology, ending with a chapter on continental drift, was published in 1944. His later measurements of the age of the Earth (4,500 +/- 100 Ma) were based on measurements of the relative abundance of uranium isotopes by Alfred O. C. Nier.

He was awarded both the Wollaston Medal and the Penrose Medal in 1956. The Arthur Holmes Medal of the European Geosciences Union is named after him.

A crater on Mars has been named in his honour.

The Durham University Department of Earth Sciences' Arthur Holmes Isotope Geology Laboratory is named after him, as is the students' Geology Society.

Notes

  1. ^ "Commemorative Plaques in Gateshead Borough". http://www.bpears.org.uk/Misc/Gateshead_Plaques/#HolmesA. 
  2. ^ Holmes, Arthur "The association of lead with uranium in rock-minerals and its application to the measurement of geological time", Proceedings of the Royal Society, Series A, vol. 85, pages 248-256 (9 June 1911)

References

  • Lewis, Cherry (2000) The Dating Game: One Man's Search for the Age of the Earth, Cambridge University Press, ISBN 0-521-89312-7

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