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The discovery of moho was through seismic waves...There are two 2 waves namely, Primary and Secondary waves...Secondary waves cannot pass through liquid and gasses. Thus, There is an abrupt increase in the velocity of earthquake waves (specifically P- waves) at this point.
the Mohorovicic (Moho) discontinuity
It is called the Mohorovicic Discontinuity, or the Moho for short.
The Mohorovicic Discontinuity, generally referred to as the Moho, where seismic waves increase in velocity.
The Moho is the name of the boundary between the crust and the mantle. It's a boundary where seismic waves increase in velocity. It is not an actual structure, but the beginning of the uppermost part of the mantle, which is composed of rigid, strong rock.
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The discovery of moho was through seismic waves...There are two 2 waves namely, Primary and Secondary waves...Secondary waves cannot pass through liquid and gasses. Thus, There is an abrupt increase in the velocity of earthquake waves (specifically P- waves) at this point.
They speed up
The Mohorovičić discontinuity (the Moho) separates the mantle and the crust.moho
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Moho
The Moho
it is the mohorovic or the moho
it is the mohorovic or the moho
the Mohorovicic (Moho) discontinuity
the Mohorovicic (Moho) discontinuity
It is called the Mohorovicic Discontinuity, or the Moho for short.