Andriza Mohorivicic
the Mohorovicic (Moho) discontinuity
Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle
The Mohorovičić Discontinuity, also called the Moho Discontinuity, was named for Andrija Mohorovičić, the Croatian seismologist who first identified it in 1909.
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 project was suggested in March 1957 by Walter Munk, a NAS member (1956) and member of the National Science Foundation (NSF) Earth Science Panel. Andrija Mohorovicic a Croatian geologist discovered that there was an area, known as the "moho". The Moho was named for Andrija Mohorovicic, who first proposed the existence of such a discontinuity.
FeaR is MoHo
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 Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.
"moho" is the plate boundary between earth's crust and the mantle.
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.
No. The Moho is simply the boundary between the mantle and the crust.
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.