By Timothy Kusky
The hot, two-volume of Earth and area technological know-how is the proper supplement to the fabric mostly taught in highschool and faculty Earth technology and astronomy sessions. in keeping with the NSES content material criteria, this entire new reference emphasizes the actual methods concerned with the formation and evolution of the Earth and universe, describes many examples of other varieties of geological and astrophysical phenomena, presents old views, and provides perception into the method of medical inquiry by means of incorporating biographical profiles of people that have contributed considerably to the advance of the sciences. the massive bang thought is gifted in addition to an overview of its actual ideas and basic legislation. The ensuing constitution of the universe, galaxies, sun approach, planets, and areas on the earth also are mentioned.
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Additional resources for Encyclopedia of Earth and Space Science
R. Hunter, and W. E. L. Minter. 8 Billion Years of Earth History. New York: SpringerVerlag, 1982. Tesfaye, Sansom, David Harding, and Timothy M. Kusky. ” Geological Society of America Bulletin 115 (2003): 1,053–1,067. , Chris Roering, Rojer J. Hart, Richard A. Armstrong, Charles E. J. de Ronde, R. W. E. Green, Marian Tredoux, E. Pederdy, and R. A. Hart. ” Nature 357 (1992): 553–562. Andes Mountains The Andes are a 5,000-mile (8,000-km) long mountain range in western South America, running generally parallel to the coast, between the Caribbean coast of Venezuela in the north and Tierra del Fuego in the south.
Western Antarctica (using the Greenwich meridian that runs nearly along the Transantarctic Mountains) is covered by the West Antarctic Ice Sheet, which some climatologists warn could collapse, raising sea levels by 10 feet (3 m) or more in a short time. The Antarctic Peninsula, Marie Byrd Land, and the area east and north of the Transantarctic Mountains are part of West Antarctica. The eastern part of Antarctica is a large Precambrian craton known as East Antarctica, with ages extending to at least 3 billion years.
The Antarctic Peninsula, Marie Byrd Land, and the area east and north of the Transantarctic Mountains are part of West Antarctica. The eastern part of Antarctica is a large Precambrian craton known as East Antarctica, with ages extending to at least 3 billion years. The rocks of the ancient craton, however, were reworked in younger mountain-building events, including an Early Paleozoic event during which East Antarctica was incorporated into Gondwana. Most of western Antarctica was built up through the accretion of microplates that include the Ellsworth Mountains terrane, the Antarctic Peninsula, Marie Byrd Land, and an unnamed block of igneous and metamorphic rocks.
Encyclopedia of Earth and Space Science by Timothy Kusky