Vad Är Mohorovicic Discontinuity? 2021
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Also called, Mo•ho (ˈmoʊ hoʊ) [1935–40; after Andrija Mohorovičić (1857–1936), Croatian geophysicist, who discovered it] The Mohorovičić discontinuity is located at an average depth of 5 miles (8 kilometers) under the oceans and 20 miles (32 kilometers) under the continents. Scientists discovered this boundary because they noticed that the velocity of seismic waves increases sharply as the waves pass from the Earth's crust into the mantle. Andrya Mohorovicic determined the boundary between the crust and the mantle, which is now named the Mohorovicic discontinuity. Velocities of seismic waves were used to identify this boundary. He had seismographs installed before the 1909 earthquake had occurred.
The article Mohorovičić discontinuity on Wikipedia projects: (en) Mohorovičić discontinuity (af) Mohorovičić-diskontinuïteit (bg) Граница на Мохоровичич (bs) Mohorovičićev diskontinuitet (ca) Discontinuïtat de Mohorovičić (cs) Mohorovičićova diskontinuita (de) Mohorovičić-Diskontinuität (eo) Malkontinuo de The Mohorovicic discontinuity (Moho) defines the boundary between the Earth's crust and mantle. Basic facts about the nature of the boundary, and changes across it, are described. The background to The boundary surface between the earth's crust and the mantle, lying at a depth of about 6–7 miles (10–12 km) under the ocean bed and about 24–30 miles (40–50 km) under the continents. ‘The sharp boundary between the crust and mantle is called the Mohorovicic discontinuity or Moho.’ the discontinuity between the crust and the mantle of the earth, occurring at depths that average about 22 mi.
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Andrija. Mohorovicic.
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Video shows what Mohorovičić discontinuity means. The boundary between the Earth's crust and mantle.. Mohorovičić discontinuity Meaning. How to pronounce, d 2018-11-10 · This page was last edited on 10 November 2018, at 15:04.
Department of Geodesy and Geophysics, University of Cambridge, Cambridge, England. Search for more papers by this author. mohorovicic discontinuity Interpretation Translation. 1 Mohorovicic-discontinuity < geo> Moho-Diskontinuität f
Mohorovicic Discontinuity: Transition zone between the Crust and Mantle. Repiti Discontinuity: Transition zone between Outer mantle and Inner mantle. In respect to this, what is meant by Gutenberg discontinuity? The Gutenberg Discontinuity is a relatively low density (lower density) lower mantle with a relatively liquid (low density) outer core.
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e. up to the Mohorovicic discontinuity. 2.
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Definition av Mohorovicic Discontinuity - även känd som Moho - av Moho: Bild av Earth interna truktur av UG - Mohorovicic Dicontinuity (röd linje) tillagd av. Yugoslav geophysicist for whom the Mohorovicic discontinuity was named (1857-1936). Exempel på användning. sweden.
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Definition from Wiktionary, the free dictionary. Jump to navigation Jump to search. See also: Mohorovičić discontinuity.
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This boundary is located at approximately 2891 km depth beneath the 19 Oct 2017 The Mohorovicic Discontinuity is the boundary between the earth's crust and mantle.
(35 km) beneath the continents and about 6 mi. (10 km) beneath the ocean floor. Also called, Mo•ho (ˈmoʊ hoʊ) [1935–40; after Andrija Mohorovičić (1857–1936), Croatian geophysicist, who discovered it] The Mohorovicic Discontinuity is the boundary between the earth 's crust and mantle. It was discovered by the refraction of seismic waves passing from one layer to the other. The Nature of the Mohorovicic Discontinuity.