noun the boundary between the Earth s crust and the underlying mantle the Mohorovicic discontinuity averages 5 miles down under oceans and 20 miles down under continents • Syn: ↑Moho • Topics: ↑geology • Instance Hypernyms: ↑boundary, ↑bound

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 Mohorovicic discontinuity (the Moho) is the boundary lying between the crust and the mantle of the earth across which seismic waves change velocities. This boundary is located approximately 24 miles below the earth’s surface and 6 miles below the oceanic floor, a distance which varies from place to place. Mohorovičić discontinuity [ mō′hə-rō ′və-chĭch ] The boundary between the Earth's crust and mantle, located at an average depth of 8 km (5 mi) under the oceans and 32 km (20 mi) under the continents. The Mohorovicic Seismic Discontinuity- boundary between crust and mantle (or Moho) Mohorovičić discontinuity exists everywhere on the Earth.

Mohorovicic discontinuity

This boundary marks a You have learned that the Mohorovičić Discontinuity is a real seismic boundary within the Earth. It is located at different depths within the Earth's lithosphere. In Mohorovicic discontinuity Add to list Share. Definitions of Mohorovicic discontinuity. noun. the boundary between the Earth's crust and the underlying mantle.

Inge. Lehman.

15 Feb 2017 Learn the proper pronunciation of "mohorovicic discontinuity" Visit us at: http:// howtopronounce.org to learn more!

Andrija. Mohorovicic. Beno.

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.

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This problem will be postponed to a succeeding paper. 1 Jan 2009 The seismic discontinuity discovered by Mohorovičić is a primary definition of the boundary between crust and upper mantle, given in terms of the 13 May 2015 The Moho discontinuity is the boundary between the Earth's crust and the mantle. It has been named so because it was discovered by a 5 Apr 2005 the elusive "Moho"--the boundary, which geologists refer to as the Mohorovicic discontinuity, between Earth's brittle outer crust and its hotter, The Mohorovicic Discontinuity, or "Moho", is the boundary between the crust and the mantle.
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Repiti Discontinuity: Transition zone between Outer mantle and Inner mantle. In respect to this, what is meant by Gutenberg discontinuity?

Pronunciation IPA : /məʊhəʊˈɹə(ʊ)vɪtʃɪtʃ ˌdɪskɒntɪˈnjuːɪti/ Proper noun . Mohorovičić discontinuity The boundary between the Earth’s crust and mantle.
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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.

Mohorovicic discontinuity Zone that separates the Earth’s crust from the asthenosphere. Gutenberg discontinuity Zone separating the lower mantle from the core; it Mohorovicic discontinuity. Definition from Wiktionary, the free dictionary. Jump to navigation Jump to search. See also: Mohorovičić discontinuity.

A: crust-mantle boundary (Mohorovičić discontinuity, “Moho”): B: core-mantle boundary (Gutenberg discontinuity): C: boundary between inner and outer core

Inmediatamente por encima del Moho, las velocidades de las ondas sísmicas primarias (ondas P) son consistentes con las del basalto (6.7–7.2 km/s), y debajo son similares a los de peridotita o dunita (7.6–8.6 km/s). [5] Mohorovicic discontinuity. Mohorovicic discontinuity: translation after Mohorovicic, the junction between the crust and the mantle. Mohorovicic discontinuity Zone that separates the Earth’s crust from the asthenosphere. Gutenberg discontinuity Zone separating the lower mantle from the core; it Mohorovicic discontinuity.

Gutenberg. Inge. Lehman. Click on the blue buttons to The Mohorovicic Discontinuity marks the boundary between the earth's crust and mantle. (The Moho was named for Andrija Mohorovicic, a Croatian geologist who Layer of the upper mantle with a thickness of 125 mi; it is composed of molten rock, on top of which the lithospheric plates slide. Mohorovicic discontinuity click to Andrya Mohorovicic determined the boundary between the crust and the mantle, which is now named the Mohorovicic discontinuity.