The Gutenberg Discontinuity, is the boundary, as detected by changes in seismic waves, between the Earth's lower mantle and the outer core about 1800 miles below the surface.
It is also called the core-mantle boundary.
The zone of discontinuity in the density between mantle and core is known as gutenburg discontinuity.
between the mantle and the core..
Wiechert-Gutenburg Discontinuity
We know the discontinuity exists because of different types of seismic waves; certain waves can penertrate to different depths. Seismic waves are refracted at the Gutenburg discontinuity, which marks the upper boundary of the earth's core
Beno Gutenberg discovered the Gutenberg Discontinuity.
The zone of discontinuity in the density between mantle and core is known as gutenburg discontinuity.
between the mantle and the core..
between the mantle and the core..
Gutenburg Discontinuity
between the mantle and the core..
Wiechert-Gutenburg Discontinuity
Wiechert-Gutenburg Discontinuity
Wiechert-Gutenburg Discontinuity
We know the discontinuity exists because of different types of seismic waves; certain waves can penertrate to different depths. Seismic waves are refracted at the Gutenburg discontinuity, which marks the upper boundary of the earth's core
The sometimes magnesium rich Mohorovičić discontinuity, which often is called simply 'Moho', forms the boundary between the basalt rich crust and the planet's underlying, iron rich mantle.
Gutenburg Discontinuity
Johannes Gutenburg is a person who lived in the 1400's