the mohorovicic discontinuity was named after ANDRIJA MOHOROVICIC.
Andriza Mohorovicic discovered the Mohorovicic discontinuity popularly known as Moho It is the boundary between the crust and the mantle it is about 2,880 kilometers thick. it is the thickest part of the earth's layer
interface between the crust and the upper mantle
Croatia.
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 mohorovicic discontinuity was named after ANDRIJA MOHOROVICIC.
Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle
Andriza Mohorovicic discovered the Mohorovicic discontinuity popularly known as Moho It is the boundary between the crust and the mantle it is about 2,880 kilometers thick. it is the thickest part of the earth's layer
interface between the crust and the upper mantle
Andriza Mohorovicic
Croatia.
He was old and sick.
Crust and Mantle.
mantle
mantle
Crust
the Mohorovicic Discontinuity