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The Gutenberg Discontinuity is found directly above this layer of the earth.?
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∙ 7y ago
The Gutenberg discontinuity is found directly above the outer core.
Darien Renner
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The Gutenberg Discontinuity is found beneath this layer?
The Gutenberg Discontinuity is found above the earth layer called the outer core. This boundary line, which separates the outer core from the lower mantle, is approximately 1798 miles below the Earth's surface.
What is Gutenberg weichert discontinuity?
The Gutenberg Discontinuity is the mantle/core boundary within Earth's interior where there is an abrupt change in the seismic waves (generated by earthquakes or explosions) that travel through Earth. It is at a depth of about 1,800 mi (2,900 km) below the surface.
Is the boundary between the liquid core and mantle known as the Moho?
No. The Moho (more correctly the Mohorovičić discontinuity) is the name given to a seismic discontinuity between the Earth's crust and mantle. The seismic discontinuity between the Earth's mantle and liquid core is known as the Gutenberg discontinuity or the CMB - Core Mantle Boundary.
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
What is the gutenburg discontinuity?
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 Gutenberg Discontinuity is found beneath this layer?
The Gutenberg Discontinuity is found above the earth layer called the outer core. This boundary line, which separates the outer core from the lower mantle, is approximately 1798 miles below the Earth's surface.
What is the difference between the Mohorovicic discontinuity and the Gutenberg discontinuity?
They mark the boundaries of differing layers of the Earth. The Moho marks the boundary between the crust and the mantle, whereas the Gutenberg discontinuity marks the boundary between the mantle and outer core.
What two regions of the earth does the Gutenberg discontinuity separate?
lower mantle from upper core
What is Gutenberg weichert discontinuity?
The Gutenberg Discontinuity is the mantle/core boundary within Earth's interior where there is an abrupt change in the seismic waves (generated by earthquakes or explosions) that travel through Earth. It is at a depth of about 1,800 mi (2,900 km) below the surface.
What happens to the Gutenberg Discontinuity as the earth cools down?
It will disintegrate as the temperature becomes too extreme
What is named after the German geologist that discovered the thing that separates the earth's mantle from the outer core?
the Gutenberg discontinuity
Is the boundary between the liquid core and mantle known as the Moho?
No. The Moho (more correctly the Mohorovičić discontinuity) is the name given to a seismic discontinuity between the Earth's crust and mantle. The seismic discontinuity between the Earth's mantle and liquid core is known as the Gutenberg discontinuity or the CMB - Core Mantle Boundary.
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
Where are you if you are at the Gutenberg Discontinuity?
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.
Where is the Weichert discontinuity?
The Gutenberg Discontinuity is the mantle/core boundary within Earth's interior where there is an abrupt change in the seismic waves (generated by earthquakes or explosions) that travel through Earth. It is at a depth of about 1,800 mi (2,900 km) below the surface.
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.
What is the gutenburg discontinuity?
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.
