The core–mantle boundary of the Earth lies between the planet's silicate mantle
and its liquid iron-nickel outer core. This boundary is located at approximately
2891 km (1796 mi) depth ben...
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
The Gutenberg Discontinuity, is the boundary, as detected by changes in seismic
waves, ... Mohorovicic discontinuity is located between the upper mantle and the
crust, while the Gutenberg discontinuity is located between the lower mantle ...
Definition of Gutenberg discontinuity – Our online dictionary has Gutenberg
discontinuity information from A Dictionary of Earth Sciences dictionary.
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 ...
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
(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 ...
Jul 7, 2015 ... The Moho is not located at a uniform depth, but about 10 kilometers (6 ... The
mantle is divided from the core by the Gutenberg discontinuity, ...
Aug 11, 2015 ... This point, called the Gutenberg discontinuity, marks the end of the mantle and
the beginning of Earth's liquid outer core. Mantle Convection.
It is located below the lithosphere (the crust and upper mantle), between about
100 and ... The Gutenberg discontinuity separates the outer core and the mantle.