The Moho boundary separates the Earth's crust from the mantle. It marks the boundary between the Earth's rigid outer layer (crust) and the underlying, more ductile layer (mantle).
"moho" is the plate boundary between earth's crust and the mantle.
Crust, Moho (lithosphere-asthenosphere boundary), mantle, core.
ummm hello! its just the moho layer! the moho layer is the boundary between the mantle and the crust!there is absolutely no boundary between the moho layer and the mantle! you think i am wrong? then drill to the moho layer and find out!
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 mantle is separated from the layer above it, the crust, by a boundary known as the Mohorovičić discontinuity or Moho. This boundary represents a sharp increase in seismic wave velocities, indicating the transition from the less dense crust to the denser mantle.
"moho" is the plate boundary between earth's crust and the mantle.
Moho
Crust, Moho (lithosphere-asthenosphere boundary), mantle, core.
ummm hello! its just the moho layer! the moho layer is the boundary between the mantle and the crust!there is absolutely no boundary between the moho layer and the mantle! you think i am wrong? then drill to the moho layer and find out!
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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 mantle is separated from the layer above it, the crust, by a boundary known as the Mohorovičić discontinuity or Moho. This boundary represents a sharp increase in seismic wave velocities, indicating the transition from the less dense crust to the denser 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.
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.
The Mohorovičić discontinuity, also known as the Moho, is the boundary between the Earth's crust and the underlying mantle. It is characterized by a sudden increase in seismic wave velocities, indicating a change in the composition and density of the Earth's layers. The Moho typically lies at depths ranging from 5 to 70 kilometers beneath the Earth's surface.
One unique characteristic of the Moho (Mohorovičić discontinuity) is that it represents the boundary between Earth's crust and mantle, marking a significant change in seismic wave velocities. This boundary is known for its sharp transition from the less dense crust to the denser mantle layer.
The Moho separates the crust and the mantle.