It is between the Crust and the upper mantle
Moho barrier: Top of mantleOceanic crust: Thinnest layerUpper mantle: Moves the crustLower mantle: Borders liquid core
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.
Crust, Moho (lithosphere-asthenosphere boundary), mantle, core.
The Moho Barrier is characterized by a seismic velocity discontinuity that separates the Earth's crust from the underlying mantle. It is located at an average depth of about 25-35 kilometers beneath continental crust and 5-10 kilometers beneath oceanic crust.
The Moho barrier, or Mohorovičić discontinuity, is postulated based on the observed change in seismic wave velocities at a certain depth beneath the Earth's surface. This change in velocity indicates a boundary between the Earth's crust and mantle, suggesting differences in composition and physical properties. Scientists use this boundary to study the Earth's internal structure and tectonic processes.
moho barrier?
It is between the Crust and the upper mantle
Moho barrier: Top of mantleOceanic crust: Thinnest layerUpper mantle: Moves the crustLower mantle: Borders liquid core
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.
Crust, Moho (lithosphere-asthenosphere boundary), mantle, core.
The Moho Barrier is characterized by a seismic velocity discontinuity that separates the Earth's crust from the underlying mantle. It is located at an average depth of about 25-35 kilometers beneath continental crust and 5-10 kilometers beneath oceanic crust.
Yes. It is called the Mohorovicic Discontinuity, where seismic waves increase in velocity.
Moho barrier=where crust meets the mantle Oceanic crust=Thinnest layer
The Moho barrier, or Mohorovičić discontinuity, is postulated based on the observed change in seismic wave velocities at a certain depth beneath the Earth's surface. This change in velocity indicates a boundary between the Earth's crust and mantle, suggesting differences in composition and physical properties. Scientists use this boundary to study the Earth's internal structure and tectonic processes.
FeaR is MoHo
No, the Moho (Mohorovičić discontinuity) is not the thinnest layer of the Earth. It is located between the Earth's crust and mantle and typically ranges from 5 to 10 kilometers in thickness. The Earth's crust is generally thinner, especially in oceanic areas where it can be as thin as 5 kilometers.
moho