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The Discontinuity Guide was created in 1995.

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How many pages does The Discontinuity Guide have?

The Discontinuity Guide has 357 pages.


What is the ISBN of The Discontinuity Guide?

The ISBN of The Discontinuity Guide is 0-426-20442-5.


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 word will you get when you unscramble this word dustointinyic?

The unscrambled word is discontinuity.


When was The Guide created?

The Guide was created in 1958.


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.


Is the lehmann discontinuity 220 km beneath the Gutenberg discontinuity?

No, the Lehmann discontinuity is believed to be located between 220 km and 260 km beneath the Earth's surface. The Gutenberg discontinuity, on the other hand, sits at a depth of around 2,900 km.


The seismic discontinuity at the base of the crust is known as?

The seismic discontinuity at the base of the crust is known as the Mohorovičić discontinuity, or Moho for short. It marks the boundary between the Earth's crust and the underlying mantle, where seismic waves experience a sudden change in velocity.


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