Philip Henry Kuenen
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
- ↑ Dennis King: Bouma's Sequence Was Just a Start. American Association of Petroleum Geologists
Web links
- Hendrik M. Van Aken: Dutch Oceanographic Research in Indonesia in Colonial Times . In: Oceanography . Volume 18, No. 4, 2005, pp. 30-41. The Snellius Expedition (pdf; 1.27 MB)
personal data | |
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SURNAME | Kuenen, Philip Henry |
BRIEF DESCRIPTION | Dutch geologist |
DATE OF BIRTH | July 22, 1902 |
PLACE OF BIRTH | Dundee |
DATE OF DEATH | 17th December 1976 |
Place of death | Suffer |