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.
Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle
the inner mantle is different than the outer mantle because the inner mantle is hotter than the outer mantle.
upper mantle and the lower mantle
The upper mantle and the lower mantle.
The mantle was discovered in1936.
Andrija Mohorovicic, 1909
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
The Croatian seismologist Andrija Mohorovicic.
the Gutenberg discontinuity
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.
Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle
mantle and crust
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 inner mantle is different than the outer mantle because the inner mantle is hotter than the outer mantle.
The upper mantle and the lower mantle.
Upper Mantlemantle