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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.

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Q: What is the gutenburg discontinuity?
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Related questions

What is gutenburg discontinuity?

The zone of discontinuity in the density between mantle and core is known as gutenburg discontinuity.


Where is the wiechert gutenburg discontinuity located?

between the mantle and the core..


Where is wiechert-gutenburg discontinuity located?

between the mantle and the core..


What is boundary between the mantle and outer core?

Gutenburg Discontinuity


Where is the Wiechert-Gutenburg discontinuity located?

between the mantle and the core..


Which area indicates a dramatic decrease in material inside the earth?

Wiechert-Gutenburg Discontinuity


Which area indicates a dramatic decrease in material density inside the Earth?

Wiechert-Gutenburg Discontinuity


Which area indicates a dramatic decrease in material density inside earth?

Wiechert-Gutenburg Discontinuity


How did geologists locate the Gutenberg 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


Which seismic discontinuity forms the boundary between the crust and the mantle?

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.


The liquid layer of earths core between mantle and inner core?

Gutenburg Discontinuity


What was Johannes Gutenburg?

Johannes Gutenburg is a person who lived in the 1400's