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The Mohorovicic discontinuity occurs between the crust and the?

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.


Where did mohorovicic discontinuity get its name?

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.


mohorovicic discontinuity?

interface between the crust and the upper mantle


Who is the discoverer of 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


Which layer of earth contains the mohorovicic discontinuity?

The Mohorovicic discontinuity is located at the boundary between the Earth's crust and mantle. It marks a change in seismic wave speeds, indicating a transition from the solid crust to the denser, semi-solid mantle below.


Who was Mohorovicic?

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).


Who was Andrija Mohorovicic?

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).


Who discovered mohorovicic distensity?

Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle


Where does the Mohorovicic discontinuity occur?

Crust and Mantle.


It separates the mantle and the crust?

The Mohorovicic Discontinuity (also known as the Moho) separates the Earth's crust from the underlying mantle. It is the boundary where seismic waves change speed, indicating a change in composition and density between the two layers.


How can seismic wave be used to infer the presence of the Mohorovicic Discontinuity?

Seismic waves change speed and direction when they encounter changes in the density and composition of rocks. The Mohorovicic Discontinuity marks the boundary between the Earth's crust and mantle, causing seismic waves to abruptly change behavior when passing through it. By analyzing the way seismic waves interact with this boundary, scientists can infer the presence and properties of the Mohorovicic Discontinuity.


The mohorovicic discontinuity occur between the crust and the?

mantle