Philip Henry Kuenen

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Philip Henry Kuenen (born July 22, 1902 in Dundee , † December 17, 1976 in Leiden ) was a Dutch geologist .

Live and act

Kuenen was the son of physics professor Johannes Petrus Kuenen and spent his earliest childhood in Scotland . He studied geology at the University of Leiden and was a student of Karl Martin and Berend George Escher . In 1925 he finished his studies, became Escher's assistant and worked in the fields of paleontology and experimental geology.

From 1929 to 1930 Kuenen took part in the Snellius expedition , which traveled the waters around the Sunda Islands in what was then the Dutch East Indies . In 1934 he became a lecturer at the University of Groningen . Since the Dutch government had decided that geology was not a major at the University of Groningen, Kuenen was able to devote a major part of his time to research. It was not until 1946 that he was appointed full professor , because the Nazis had prevented this during the German occupation of the Netherlands in World War II because he had British ancestors .

Kuenen is best known for his work in the field of marine geology , on which he published a book. His other contributions to geology include geochemical calculations on sediments and the water cycle, as well as research on absolute and relative sea ​​level fluctuations , the rounding of sediment grains, faults in the area of continental slopes and especially turbidites . He studied these both by means of experiments and in geological outcrops . One of his students was Arnold Bouma , another pioneer in the field of turbidite research, after whom the typical layer sequence of a turbidite was named, the Bouma sequence .

In 1970 the Doeglas Commission recommended that the Dutch government abandon all geological research in Groningen and concentrate it on other universities instead. Kuenen was a staunch opponent of this plan, but could not prevent its implementation. After a nervous breakdown in 1970, he retired in 1972.

In the course of his career, Kuenen received the Penrose Medal in 1961 , the Gustav Steinmann Medal in 1966 and the Wollaston Medal in 1970 . In 1961 he was elected to the American Academy of Arts and Sciences . Since 1966 he was a member of the Leopoldina .

Works (selection)

  • 1937–1942: Scientific results of the Snellius Expedition in the eastern part of the Netherlands East Indies, 1929–1930. EJ Brill
  • 1950: Marine geology. Wiley, New York
  • 1952: Turbidity currents, graded and non-graded deposits. In: Journal of Sedimentary Research . Volume 22, pp. 83-96 (with Henry William Menard)
  • 1953: Graded bedding, with observations on lower Paleozoic rocks of Britain. (= Negotiating of the Koninklijke Nederlandse Akademie van Wetenschappen, Afdeeling Natuurkunde, 1. reeks, deel 20, no. 3)
  • 1959: Sand - its origin, transportation, abrasion, and accumulation. (= Alexander L. du Toit memorial lectures, No. 6)

literature

  • LMJU van Straaten: In memoriam Ph. H. Kuenen. In: Geologie en Mijnbouw . Vol. 56, No. 1, 1977, pp. 1-3
  • AJ Pannekoek: Geological research at the universities of The Netherlands, 1877–1962. In: Geologie en Mijnbouw . Tape. 41, No. 4, 1962, pp. 161-174

Individual evidence

  1. Dennis King: Bouma's Sequence Was Just a Start. American Association of Petroleum Geologists

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