By Alexander E. Gates
In a single quantity, this authoritative reference covers awesome Earth scientists from the 19th century to the current, in components together with weather switch, geophysics, oceanography, paleontology, planetary geology, sedimentology and stratigraphy, and tectonics. John Dewey, Ian Carmichael, Stephen Jay Gould, Carl Sagan, Richard Tuttle, and Heinrich Holland are only some of the many scientists incorporated during this interesting assortment.
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Additional resources for A to Z of Earth Scientists (Notable Scientists)
Berry was a Guggenheim Fellow in 1967. Berry has performed significant service to the profession and the public. He has served in numerous roles for the International Stratigraphic Commission, the National Research Council, the Geological Society of America, the American Geological Institute, and the American Association for the Advancement of Science. He was also the director of the Environmental Sciences Curriculum Development Program for the San Francisco, California, Unified School District.
Bowen was born in Kingston, Ontario, on June 21, 1887. He completed his elementary and high school education in Kingston public schools, and entered Queen’s University, Canada. Bowen had his sights set on becoming a teacher but after one year decided to join an Ontario Bureau of Mines geological mapping party to Larder Lake with the allure of money and travel. It was a revelation for him and he enrolled in the School of Mining upon his return, registering in mineralogy and petrology. He graduated with a bachelor of science degree in chemistry and geology in 1909.
During this project he performed research on rocks from the Avalon Terrane in Nova Scotia, Canada, as well as those in Namibia and Madagascar, Africa, and the White Sea in Russia. The other major area of research for Sam Bowring is the development of the continental crust. Ocean crust is created at the mid-ocean ridges and destroyed at the subduction zones within about 200 million years. Continental crust, on the other hand, has been built throughout the history of the Earth. Because there are numerous and complex processes in the assembly of a continent, all of which overprint and modify each other in complex ways, deciphering the geology of continents becomes a monumental task.