interface between the crust and the upper mantle
the Mohorovicic discontinuity is 500-600 degrees C
the mohorovicic discontinuity was named after ANDRIJA MOHOROVICIC.
Mohorovicic discontinuity
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
Andrija Mohorovicic, 1909
It is called the Mohorovicic Discontinuity, or the Moho for short.
the mohorovicic discontinuity was named after ANDRIJA MOHOROVICIC.
Mohorovicic discontinuity
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
Crust and Mantle.
Mohorovicic discontinuity is located between the upper mantle and the crust, while the Gutenberg discontinuityis located between the lower mantle and the outer core.
Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle
mantle
mantle
Crust
the Mohorovicic Discontinuity
The Mohorovicic Discontinuity.
The Mohorovicic Discontinuity.