The Moho discontinuity is 31 miles/50KM thick.
There's no specific answer because it discontinued
The Mohorovičić discontinuity, also known as the Moho, marks the boundary between the Earth's crust and mantle. It is identified by a sudden increase in seismic wave velocities, indicating a change in rock density and composition at this boundary.
The Mohorovičić discontinuity (Moho) separates the Earth's crust from the underlying mantle. It is found beneath continents and beneath ocean basins.
To the best of my knowledge, he was a Croatian geologist the developed the theory of discontinuity, which means that the crust of the Earth is about 6 miles thick under the oceans and about 22 miles thick under the continents. Now called 'Moho's Discontinuity' or simply 'Moho'
The temperature of the Moho discontinuity is estimated to be around 500 to 900 degrees Celsius. This high temperature is due to the increased heat coming from the Earth's interior, causing the rocks to be partially melted along this boundary.
The Mohorovičić Discontinuity, also called the Moho Discontinuity, was named for Andrija Mohorovičić, the Croatian seismologist who first identified it in 1909.
There's no specific answer because it discontinued
The Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.
The Mohorovicic Discontinuity (also known as the Moho) separates the Earth's crust from the underlying mantle. It is the boundary where seismic waves change speed, indicating a change in composition and density between the two layers.
The Moho is an abbreviation of the Mohorovicic Discontinuity, the boundary between the crust and the upper mantle.
The Moho separates the crust and the mantle.
The Mohorovičić discontinuity, also known as the Moho, marks the boundary between the Earth's crust and mantle. It is identified by a sudden increase in seismic wave velocities, indicating a change in rock density and composition at this boundary.
No. The Moho (more correctly the Mohorovičić discontinuity) is the name given to a seismic discontinuity between the Earth's crust and mantle. The seismic discontinuity between the Earth's mantle and liquid core is known as the Gutenberg discontinuity or the CMB - Core Mantle Boundary.
The Mohorovičić discontinuity (Moho) separates the Earth's crust from the underlying mantle. It is found beneath continents and beneath ocean basins.
To the best of my knowledge, he was a Croatian geologist the developed the theory of discontinuity, which means that the crust of the Earth is about 6 miles thick under the oceans and about 22 miles thick under the continents. Now called 'Moho's Discontinuity' or simply 'Moho'
"moho" is the plate boundary between earth's crust and the mantle.
No, the Outer Core is not known as the Moho. The Moho, short for Mohorovicic Discontinuity, is the boundary between the Earth's crust and mantle, while the Outer Core is a layer of molten iron and nickel that surrounds the Earth's solid inner core.