Gutenberg discontinuity. The Gutenberg discontinuity occurs within Earth's
interior at a depth of about 2,900 km (1,800 mi) below the surface, where there is
The mantle–core boundary is the Gutenberg discontinuity at a depth of about
2,800 kilometres. The outer core is thought to be liquid because shear waves do
Gutenberg discontinuity click to hear : Gutenberg discontinuity. Zone separating
the lower mantle from the core; it is located at a depth of about 2,900 km.
Gutenberg discontinuity. ... -discontinuity (Thybo and Perchuc, 1997) marks the
transition from the lid, which is defined as the uppermost mantle beneath the ...
Definition of the Mohorovicic Discontinuity - also known as the Moho - by
Geology.com. ... The red line in the drawing at right shows its location. In geology
Sep 7, 2016 ... Olivine anisotropy suggests Gutenberg discontinuity is not the base of the .... with
estimates for the location of the Gutenberg discontinuity (13).
Seismic stations located at increasing distances from the earthquake epicenter
will record seismic ... Gutenberg Seismic Discontinuity / Core-Mantle Boundary
(seismic wave guide), the stratum in which seismic waves move at decreased
velocities in the upper mantle of the earth. It is named after B. Gutenberg, who ...
Related to Mohorovicic discontinuity: crust, Gutenberg Discontinuity, Convection
... The Mohorovičić discontinuity is located at an average depth of 5 miles (8 ...
Gutenberg Discontinuity - separates mantle from core - change from silicates and
.... At some depth below the surface at this location is a body that has a lower ...