The lithosphere
moho
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.
The Moho, or Mohorovičić discontinuity, is located between the Earth's crust and the underlying mantle. It varies in depth, typically ranging from about 5 to 70 kilometers (3 to 43 miles) beneath the Earth's surface, depending on whether it is beneath oceanic or continental crust. The Moho marks a significant change in geological properties, as it separates the less dense materials of the crust from the denser materials of the mantle.
The Mohorovičić discontinuity, commonly referred to as the Moho, is the boundary between the Earth's crust and the underlying mantle. It separates the solid, less dense rocks of the crust from the denser, more viscous rocks of the mantle beneath. This transition marks a significant change in both composition and physical properties of the Earth's materials.
The structure of Earth's interior, including the different layers such as the crust, mantle, and core, was discovered by studying the velocities of seismic waves. The speed at which seismic waves travel through the Earth's layers varies, providing valuable information about the composition and properties of these layers.
Crust, Moho (lithosphere-asthenosphere boundary), mantle, core.
moho barrier?
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.
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.
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 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).
1st-moho barrier2nd-mantle layer with more convection3rd-mantle layer with less convection4th-core
The Moho separates the crust and the mantle.
Yes. It is called the Mohorovicic Discontinuity, where seismic waves increase in velocity.
The Mohorovičić discontinuity (MOHO) is located between the Earth's crust and mantle, making it directly above the Earth's crust.
Moho barrier: Top of mantleOceanic crust: Thinnest layerUpper mantle: Moves the crustLower mantle: Borders liquid 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!