The boundary between the Earth's crust and mantle is called the MohoroviÄiÄ discontinuity, or Moho. It is typically located between 5 to 70 kilometers beneath the Earth's surface and marks the transition from the less dense rocks of the crust to the denser rocks of the mantle. The Moho is defined by a sudden increase in seismic wave velocities as they pass from the crust into the mantle.
The mantle is located directly beneath the Earth's crust and is approximately 1,800 miles (2,900 kilometers) thick. The boundary between the crust and the mantle is known as the MohoroviÄiÄ discontinuity or Moho.
Moho stands for MohoroviÄiÄ discontinuity, which is the boundary between the Earth's crust and mantle.
The Moho, short for MohoroviÄiÄ discontinuity, is a boundary between the Earth's crust and the mantle. It marks a significant change in seismic wave velocities, indicating the transition from the less dense, rigid crust to the more dense, flowing mantle beneath.
The boundary between the crust and upper mantle is known as the MohoroviÄiÄ discontinuity or Moho. It represents the change in seismic wave velocity and composition between the rigid outer layer (crust) and the more ductile layer beneath (mantle).
It is between the Crust and the upper mantle
The mantle is located directly beneath the Earth's crust and is approximately 1,800 miles (2,900 kilometers) thick. The boundary between the crust and the mantle is known as the MohoroviÄiÄ discontinuity or Moho.
Moho stands for MohoroviÄiÄ discontinuity, which is the boundary between the Earth's crust and mantle.
The Moho, short for MohoroviÄiÄ discontinuity, is a boundary between the Earth's crust and the mantle. It marks a significant change in seismic wave velocities, indicating the transition from the less dense, rigid crust to the more dense, flowing mantle beneath.
The boundary between the crust and upper mantle is known as the MohoroviÄiÄ discontinuity or Moho. It represents the change in seismic wave velocity and composition between the rigid outer layer (crust) and the more ductile layer beneath (mantle).
The boundaries between Earth's layers are the crust-mantle boundary (Moho), the mantle-core boundary (Gutenberg discontinuity), and the outer core-inner core boundary.
It is between the Crust and the upper mantle
The boundary between the crust and the mantle was discovered by Croatian seismologist Andrija MohoroviÄiÄ in 1909. This boundary is known as the MohoroviÄiÄ discontinuity or "Moho" and marks the change in seismic wave velocities between the Earth's crust and mantle.
its called the mantle
It is the mantle.
Yes, the boundary between the liquid outer core and the solid mantle is known as the Gutenberg discontinuity. The MohoroviÄiÄ discontinuity, or Moho, is the boundary between the Earth's crust and the mantle.
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).
The Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.