19 Oct 2017 The Mohorovicic Discontinuity is the boundary between the earth's crust and mantle. It was discovered by the refraction of seismic waves

Gränsytan mellan jordskorpan och manteln kallas Moho (Mohorovicic to discontinuity mapping with ground-penetrating radar in crystalline rock of the Gotthard

2000. Mohorovicic discontinuity translation in English-French dictionary. Showing page 1. Found 7 sentences matching phrase "Mohorovicic discontinuity".Found in 3 ms. ‘These values suggest that the Mohorovicic discontinuity remains relatively deep, 40 to 45 km, beneath western half of the transect.’ ‘The Mohorovicic discontinuity, or Moho, the first major boundary of the earth's interior, separates the crust from the underlying mantle.’ ‘This seismic boundary is known as the Mohorovicic 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 Moho definition is - the boundary layer between the earth's crust and mantle whose depth varies from about 3 miles (5 kilometers) beneath the ocean floor to about 25 miles (40 kilometers) beneath the continents. The Gutenberg discontinuity occurs within Earth's interior at a depth of about 2,900 km (1,800 mi) below the surface, where there is an abrupt change in the seismic waves (generated by earthquakes or explosions) that travel through Earth.

Mohorovicic discontinuity

Seismic- and satellite-derived (GOCE) crustal thickness. Detection of Moho (Mohorovicic) discontinuity. 10 · Visa alla. Mohorovicic discontinuity), kunde vara just en sådan plats i Jordens lager där man kunde få svar på sina frågor. Man visste att moho-lagret Den diskontinuiteten som heter Mohorovicic discontinuity eller "Moho" är den accepterade gränsen mellan skorpan och manteln.

Language · Watch · Edit. See also: Mohorovicic discontinuity 15 Feb 2017 Learn the proper pronunciation of "mohorovicic discontinuity" Visit us at: http:// howtopronounce.org to learn more! 12 Mar 2012 Scientists map the boundary between the Earth's crust and its mantle - the so- called Mohorovicic discontinuity - in unprecedented detail.

Mohorovičić-diskontinuiteten (moxoroʋitʃitɕ), vanligtvis känd som Moho, betecknar gränsen mellan jordskorpan och manteln.Namngiven efter den kroatiske seismologen Andrija Mohorovičić.

As stated above, it occurs at an average depth of about 8 kilometers beneath the ocean basins and 32 kilometers beneath continental surfaces. Mohorovicic was able to use his discovery to study thickness variations of the crust. Se hela listan på worldatlas.com Mohorovičić-diskontinuiteten (moxoroʋitʃitɕ), vanligtvis känd som Moho, betecknar gränsen mellan jordskorpan och manteln.Namngiven efter den kroatiske seismologen Andrija Mohorovičić. Mohorovičić discontinuity definition, the discontinuity between the crust and the mantle of the earth, occurring at depths that average about 22 miles (35 km) beneath the continents and about 6 miles (10 km) beneath the ocean floor.

‘These values suggest that the Mohorovicic discontinuity remains relatively deep, 40 to 45 km, beneath western half of the transect.’ ‘The Mohorovicic discontinuity, or Moho, the first major boundary of the earth's interior, separates the crust from the underlying mantle.’ ‘This seismic boundary is known as the Mohorovicic

Översättning till svenska. ”the Mohorovicic discontinuity averages 5 miles down under oceans and 20 miles down under continents”. sweden. Svenska. Översättning till svenska.

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Gutenberg's (1951 c) temperature curve (fìg. 2). 3. Constant chemical composition. 4.

Översättning till svenska. Moho Upptäckten av denna partikulära diskontinuitet (nu kallad Mohorovicic Discontinuity eller Moho), 1909 av den kroatiska forskaren Andrija Mohorovicic, är en It was located at earth's mohorovicic discontinuity.
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8 Dec 2013 The seismic signature of the Moho from which geologic and tectonic evolution hypotheses are derived is to a large degree a result of the

(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.

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Andrya Mohorovicic determined the boundary between the crust and the mantle, which is now named the Mohorovicic discontinuity. Velocities of seismic waves

Andrija. Mohorovicic. Beno. Gutenberg. Inge. Lehman. Click on the blue buttons to The Mohorovicic Discontinuity marks the boundary between the earth's crust and mantle.