The Mohorovicic discontinuity, usually referred to as the Moho, is the boundary between the Earth's crust and the mantle. The Moho serves to separate both oceanic crust and continental crust from underlying mantle. The Moho mostly lies entirely within the lithosphere; only beneath mid-ocean ridges does the Moho also define the lithosphere-asthenosphere boundary. The Mohorovicic discontinuity was first identified in 1909 by Andrija Mohorovicic, a Croatian seismologist, when he observed the abrupt increase in the velocity of earthquake waves (specifically P-waves) at this point.
The Mohorovicic discontinuity is about 5 km below the ocean floor and 30 to 50 km beneath typical continents. The Moho is deepest beneath the Tibetan Plateau, where it is approximately 75 km below the surface.[
The Mohorovicic discontinuity is the separation between the crust and the upper mantle.
Averages 7-8km under ocean basins, ~32km under the continents, and up to ~88km under some large mountain ranges.
About 500 to 600 °C
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Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle
The Mohorovičić discontinuity (the Moho) separates the mantle and the crust.moho
No. The Moho, or Mohorovicic Discontinuity is the boundary between the crust and the mantle.
The Mohorovicic Discontinuity is the boundary between the crust and the mantle, where seismic waves change velocity.
This is known as the Mohorovičić discontinuity. This is often shortened to Moho. It was one of the first features of the Earth's interior that was discovered using seismic waves. In 1909, Andrija Mohorovicic discovered this boundary and it was named in his honor.
Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle
The Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.
The Mohorovičić discontinuity (the Moho) separates the mantle and the crust.moho
It is called the Mohorovicic Discontinuity, or the Moho for short.
No. The Moho, or Mohorovicic Discontinuity is the boundary between the crust and the mantle.
moho
The Moho is an abbreviation of the Mohorovicic Discontinuity, the boundary between the crust and the upper mantle.
Andriza Mohorovicic discovered the Mohorovicic discontinuity popularly known as Moho It is the boundary between the crust and the mantle it is about 2,880 kilometers thick. it is the thickest part of the earth's layer
Mohorovicic discontinuity (or simply Moho)
the Mohorovicic (Moho) discontinuity
the Mohorovicic (Moho) discontinuity
The Moho , short for Mohorovicic discontinuity , is about 7 kilometers below the floor of the ocean and the MANTLE is the layer immediately beneath the Moho !