The layer immediately beneath the Moho is called the mantle. It is a region of hot, solid rock that extends from the base of the Earth's crust to the top of the outer core.
The Moho discontinuity is typically about 5-10 kilometers thick beneath the oceanic crust and about 20-90 kilometers thick beneath the continental crust.
The Moho, short for Mohorovičić discontinuity, is a boundary in the Earth's crust that separates the solid crust from the underlying mantle. So, the Moho is where the solid crust transitions into the solid mantle, but it is not a solid or liquid layer itself.
The pressure of the Moho is estimated to be around 27 to 30 kilobars, which is equivalent to about 27,000 to 30,000 times the atmospheric pressure at sea level. This high pressure is due to the immense weight of the overlying rocks and crust above the Moho boundary.
Andrija_Mohorovičić (1857-1936) was a Croatian seismologist and meteorologist who theorized the boundary layer between the Earth's crust and its mantle, now known as the Mohorovicic Discontinuity (aka Moho).
The layer immediately beneath the Moho is called the mantle. It is a region of hot, solid rock that extends from the base of the Earth's crust to the top of the outer core.
The core is actually located beneath the Earth's mantle. The layer immediately beneath the Moho is the Earth's mantle, which is a region of hot, flowing rock that lies between the crust and the outer core.
FeaR is MoHo
The Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.
Moho stands for Mohorovičić discontinuity, which is the boundary between the Earth's crust and mantle.
No. The Moho is simply the boundary between the mantle and the crust.
The boundary between the Earth's crust and mantle is called the Mohorovičić discontinuity or Moho. It is typically located between 5-70 kilometers (3-43 miles) beneath the Earth's surface. Below the Moho, lies the Earth's mantle, which extends to a depth of about 2,900 kilometers (1,800 miles).
The Moho is an abbreviation of the Mohorovicic Discontinuity, the boundary between the crust and the upper 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.
Moho
Andriza Mohorivicic
Moho