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What separate the crust from the mantle?
The Mohorovicic Discontinuity, generally referred to as the Moho, where seismic waves increase in velocity.
Which seismic discontinuity marks the boundary between the crust and 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.
How thick is the moho discontinuity?
The Moho discontinuity is 31 miles/50KM thick.
What is the temperature of the Moho discontinuity?
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.
What is the difference between the Mohorovicic discontinuity and the Gutenberg discontinuity?
They mark the boundaries of differing layers of the Earth. The Moho marks the boundary between the crust and the mantle, whereas the Gutenberg discontinuity marks the boundary between the mantle and outer core.
What two regions of the earth did the Moho discontinuity separate?
The Moho separates the crust and the mantle.
What boundaries separate the earth's crust with the upper mantle?
mohorocivic discontinuity or moho
Does the Moho barrier separate the earth's crust and mantle?
Yes. It is called the Mohorovicic Discontinuity, where seismic waves increase in velocity.
What does moho stand for?
"moho" is the plate boundary between earth's crust and the mantle.
It separates the mantle and the crust?
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.
Is the boundary between the liquid core and mantle known as the Moho?
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.
Is the Outer Core known as the Moho?
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.
Which feature of earth was discovered by studying the velocities of the seismic waves?
the Mohorovicic (Moho) discontinuity
What separate the crust from the mantle?
The Mohorovicic Discontinuity, generally referred to as the Moho, where seismic waves increase in velocity.
Which seismic discontinuity marks the boundary between the crust and 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.
Who was the Moho Discontinuity named after?
The Mohorovičić Discontinuity, also called the Moho Discontinuity, was named for Andrija Mohorovičić, the Croatian seismologist who first identified it in 1909.
What layer is MOHO directly above?
The Mohorovičić discontinuity (MOHO) is located between the Earth's crust and mantle, making it directly above the Earth's crust.
