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
Gutenberg discontinuity click to hear. Zone separating the lower mantle from the
core; it is located at a depth of about 1,800 mi.
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 ...
Seismic stations located at increasing distances from the earthquake epicenter
will record seismic ... Gutenberg Seismic Discontinuity / Core-Mantle Boundary
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, ...
(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 ...
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.