The Gutenberg discontinuity was discovered by a German geophysicist named Beno Gutenberg in 1913.Gutenberg find out that it is the boundary that seperates the two layers.The gutenberg layer is 1500 km thick.
Beno Gutenberg discovered the Gutenberg Discontinuity.
Beno Gutenberg
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The Gutenberg discontinuity is actually found at the base of the mantle, not the lithosphere.
The Gutenberg discontinuity is found directly above the outer core.
Mohorovicic discontinuity is located between the upper mantle and the crust, while the Gutenberg discontinuityis located between the lower mantle and the outer core.
The Gutenberg Discontinuity is found above the earth layer called the outer core. This boundary line, which separates the outer core from the lower mantle, is approximately 1798 miles below the Earth's surface.
what is these seven major plates
The Moho discontinuity is 31 miles/50KM thick.
They mark the boundaries of differing layers of the Earth. The Moho marks the boundary between the crust and the mantle, whereas the Gutenberg discontinuity marks the boundary between the mantle and outer core.
2000 km 20 miles long
The boundary of mantle and core are called Gutenberg Discontinuity