To the best of my knowledge, he was a Croatian geologist the developed the theory of discontinuity, which means that the crust of the Earth is about 6 miles thick under the oceans and about 22 miles thick under the continents.
Now called 'Moho's Discontinuity' or simply 'Moho'
There is no widely known public figure or historical figure named Andrea Mohorovicic. It is possible that this person is a private individual or a lesser-known figure.
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.
Crust and Mantle.
He was old and sick.
mantle
mantle
Crust
the Mohorovicic Discontinuity