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
The Mohorovicic discontinuity is named after Croatian seismologist Andrija Mohorovicic, who first discovered it in 1909. It marks the boundary between the Earth's crust and the mantle and is characterized by a sudden increase in seismic wave velocity.
interface between the crust and the upper mantle
There's no specific answer because it discontinued
The Mohorovicic Discontinuity, generally referred to as the Moho, where seismic waves increase in velocity.
The seismic discontinuity at the base of the crust is known as the Mohorovičić discontinuity, or Moho for short. It marks the boundary between the Earth's crust and the underlying mantle, where seismic waves experience a sudden change in velocity.
The Mohorovicic discontinuity is named after Croatian seismologist Andrija Mohorovicic, who first discovered it in 1909. It marks the boundary between the Earth's crust and the mantle and is characterized by a sudden increase in seismic wave velocity.
interface between the crust and the upper mantle
Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle
Crust and Mantle.
mantle
the Mohorovicic Discontinuity
The Mohorovicic Discontinuity.
The Mohorovicic Discontinuity.
mohorovicic discontinuity
mohorovicic discontinuity
The Mohorovicic discontinuity occurs between the Earth's crust and the mantle. It marks the boundary where seismic waves change speed, indicating a change in the composition of the Earth's layers.
The Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.