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Where is the Wiechert-Gutenburg discontinuity located?
The Wiechert-Gutenberg discontinuity is located at a depth of around 2,900 kilometers (1,800 miles) below the Earth's surface, between the outer core and the lower mantle. This boundary marks the transition between the liquid outer core and the solid mantle in the Earth's interior.
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.
Who was the Moho Discontinuity named after?
The Mohorovičić Discontinuity, also called the Moho Discontinuity, was named for Andrija Mohorovičić, the Croatian seismologist who first identified it in 1909.
What are the two layers of discontinuity that are part of the interior structure of earth?
The two layers of discontinuity in Earth's interior are the Mohorovičić discontinuity (Moho) that separates the Earth's crust from the underlying mantle, and the Gutenberg discontinuity that marks the boundary between the mantle and the outer core. These discontinuities are characterized by changes in seismic wave velocity and composition.
Where is wiechert-gutenburg discontinuity located?
between the mantle and the core..
Where is the wiechert gutenburg discontinuity located?
between the mantle and the core..
What is boundary between the mantle and outer core?
Gutenburg Discontinuity
Which area indicates a dramatic decrease in material inside the earth?
Wiechert-Gutenburg Discontinuity
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.
Where is the Wiechert-Gutenburg discontinuity located?
The Wiechert-Gutenberg discontinuity is located at a depth of around 2,900 kilometers (1,800 miles) below the Earth's surface, between the outer core and the lower mantle. This boundary marks the transition between the liquid outer core and the solid mantle in the Earth's interior.
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.
What was Johannes Gutenburg?
Johannes Gutenburg is a person who lived in the 1400's
What did gutenburg do?
Johannes Gutenburg created the printing press, making more copies of the Bible.
When was The Discontinuity Guide created?
The Discontinuity Guide was created in 1995.
Where is the wiechert -gutenburg discontinuited located?
The Wiechert-Gutenberg Discontinuity is located within the Earth's mantle, specifically at a depth of approximately 400 to 700 kilometers (about 250 to 430 miles) beneath the Earth's surface. It marks the boundary between the upper mantle and the lower mantle, characterized by a change in seismic wave speeds and material properties. This discontinuity is named after the seismologists Emil Wiechert and Beno Gutenberg, who contributed to our understanding of the Earth's internal structure.
