No. The Moho (more correctly the Mohorovičić discontinuity) is the name given to a seismic discontinuity between the Earth's crust and mantle. The seismic discontinuity between the Earth's mantle and liquid core is known as the Gutenberg discontinuity or the CMB - Core Mantle Boundary.
The boundary between the crust and the upper mantle is called the Mohorovičić discontinuity, commonly known as the Moho.
The boundary between the mantle and the outer core is a layer known as D". It is a thermal and chemical boundary where a change in speed of seismic waves has been noted.
No. The Moho, or Mohorovicic Discontinuity is the boundary between the crust and the mantle.
The Moho is best known for being the boundary between the Earth's crust and the mantle. A unique characteristic of the Moho are its dry and deep ridges.
It is called the Mohorovičić discontinuity or the Moho for short.It was one of the fist features of the Earth's interior that was discovered using seismic waves. In 1909, Andrija Mohorovicic discovered this boundary and it was named in his honor.
Gutenburg Discontinuity
The boundary between the crust and the upper mantle is called the Mohorovičić discontinuity, commonly known as the Moho.
This region is known as the mesosphere. The base of the mesosphere includes the D'' (D double prime) layer which is sometimes considered to be a transition zone between the mantle and the core-mantle boundary zone.
The boundary between the mantle and the outer core is a layer known as D". It is a thermal and chemical boundary where a change in speed of seismic waves has been noted.
No. The Moho, or Mohorovicic Discontinuity is the boundary between the crust and the mantle.
The boundary between the crust and the mantle is called the Mohorovicic discontinuity. It is also called simply the Moho and it is the abrupt divide between faster and slower speeds where the mantle starts.
This occurs at a convergent plate boundary and is known as subduction.
The Moho is best known for being the boundary between the Earth's crust and the mantle. A unique characteristic of the Moho are its dry and deep ridges.
It is called the Mohorovicic Discontinuity, or the Moho for short.
It is called the Mohorovičić discontinuity or the Moho for short.It was one of the fist features of the Earth's interior that was discovered using seismic waves. In 1909, Andrija Mohorovicic discovered this boundary and it was named in his honor.
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).
Yes