- Felix Andries Vening Meinesz
Infobox Scientist
name = Felix Andries Vening Meinesz
box_width =
image_width =150px
caption =Vening Meinesz with his gravimeter
birth_date =July 30 1887
birth_place =the Hague
death_date =August 10 1966
death_place =Amersfoort
residence =
citizenship =
nationality = Dutch
ethnicity =
field = geophysicist geodesist
work_institutions =
alma_mater =
doctoral_advisor =
doctoral_students =
known_for =gravimeter
author_abbrev_bot =
author_abbrev_zoo =
influences =
influenced =
prizes =
religion =
footnotes =Felix Andries Vening Meinesz (
the Hague July 30 1887 -Amersfoort August 10 1966 ) was a Dutch geophysicist and geodesist. He is known for his invention of a precise method for measuringgravity . Thanks to his invention, it became possible to measure gravity at sea, which led him to the discovery of gravity anomalies above the ocean floor. He later attributed these anomalies tocontinental drift .Named after him are:
*a
gravimeter , an apparatus to measure gravity
*a mathematical function used in geodesy
*a medal of the European Geophysical Society/European Geosciences Union
*a research school atUtrecht University
*Vening Meinesz crater on theMoon .Biography
Vening Meinesz' father, Sjoerd Anne Meinesz, was mayor, first of
Rotterdam , then ofAmsterdam . He grew up in a protected environment. In 1910 he graduated in civil engineering inDelft . The same year he started working for the Dutch gravitational survey. In 1915 he wrote hisdissertation on the defects of the gravimeters used at that time.Vening Meinesz then designed a new gravimeter, which the KNMI (Royal Dutch Meteorological Institute) built. The apparatus has two pendula of the same size hanging in a frame but moving in opposite phases. With mirrors and lightbeams the difference in amplitude of the two pendula is captured on a film. Vening Meinesz had discovered that horizontal accelerations (as by waves on a boat) had no influence on the difference in amplitude between the two pendula. The recorded difference then is the amplitude of a theoretical, undisturbed pendulum. Now it became possible to measure gravity more accurately. Vening Meinesz started with measuring gravity all over the Netherlands, for which a network of 51 monitoring stations was created. This became a success, which encouraged him to do measurements at sea. A perfected gravimeter, hanging in a 'swing', was designed. The experiment was successful.
Now measuring gravity at sea had become possible. Between 1923 and 1929 the tall (over 2 metres) Vening Meinesz embarked in small submarines for some uncomfortable expeditions. His goal was to establish the exact shape of the
geoid and the Earth. When one of his expeditions was made into a movie in 1935, Vening Meinesz became a hero of the Dutch cinema public. Besides, his research was in the international scientific spotlight. In 1927 he become a parttime professor in geodesy,cartography and geophysics atUtrecht University , and in 1937 he became professor at theDelft University of Technology as well.In
World War II , Vening Meinesz was involved in the Dutch resistance. After the war he could take up his tasks as a professor again. From 1945 to 1951 he was the director of the KNMI. He retired in 1957.Research and Discoveries
The vast amounts of data that his expeditions yielded were analyzed and discussed together with other leading Dutch Earth scientists of the time J.H.F. Umbgrove, B.G. Escher and Ph.H. Kuenen, the results were published in 1948. An important result was the discovery of elongated belts of negative gravity anomalies along the
oceanic trench es. The mean gravity force appeared to be the same on land and at sea, which was in agreement with the principle ofisostasy . Vening Meinesz was especially intrigued by the oceanic trenches. The coexisitence of activevolcanism , large negative gravity anomalies and the sudden difference in terrain elevation could only be explained by assuming the Earth's crust was somehow pushed together at these places. As a geophysicist, he was prejudiced that the crust was too rigid to deform at that scale in such a way. His discoveries could be explained only with the development of the theory ofplate tectonics in the '50s.External links
* [http://vmsg.geo.uu.nl/ Vening Meinesz Research School of Geodynamics at Utrecht University]
* [http://www.ncg.knaw.nl/eng/publications/greenseries.html Some downloadable (pdf scanned) publications by FA Vening Meinesz]
Wikimedia Foundation. 2010.