Andrija Mohorovicic, 1909
It is called the Mohorovicic Discontinuity, or the Moho for short.
The Mohorovicic Discontinuity, generally referred to as the Moho, where seismic waves increase in velocity.
Mohorovicic discontinuity
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.
The D" layer (pronounced D double prime layer) forms the base of the Earth's lower mantle. Below this lies the outer core. This boundary zone is marked by a seismic discontinuity known as the Gutenberg discontinuity.
The Mohorovičić discontinuity (the Moho) separates the mantle and the crust.moho
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.
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.
It is called the Mohorovicic Discontinuity, or the Moho for short.
The Mohorovicic Discontinuity, generally referred to as the Moho, where seismic waves increase in velocity.
The Mohorovicic Discontinuity is the boundary between the crust and the mantle, where seismic waves change velocity.
This is known as the Mohorovičić discontinuity. This is often shortened to Moho. It was one of the first 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.
Mohorovicic discontinuity
Yes. It is called the Mohorovicic Discontinuity, where seismic waves increase in velocity.
It is between the Crust and the upper mantle
The sometimes magnesium rich Mohorovičić discontinuity, which often is called simply 'Moho', forms the boundary between the basalt rich crust and the planet's underlying, iron rich mantle.
The boundary between the crust and mantle is called the Mohorovicic discontinuity (or Moho); it is named in honor of the man who discovered it, the Croatian scientist Andrija Mohorovicic