please help this is one of my assignments in science...what does JEFFREY'S DICONTINUITY?
Jeffrey Toobin's birth name is Jeffrey Ross Toobin.
Jeffrey Donovan is 6'.
Jeffrey Vinik was born in 1959.
Jeffrey Lagarias was born in 1949.
Jeffrey Spieler was born in 1946.
It is however discovered by the person that is named to it. That is the law, for example you are the one that discovered it. It is named to you.
The Discontinuity Guide was created in 1995.
The Discontinuity Guide has 357 pages.
The Mohorovičić Discontinuity, also called the Moho Discontinuity, was named for Andrija Mohorovičić, the Croatian seismologist who first identified it in 1909.
The unscrambled word is discontinuity.
The ISBN of The Discontinuity Guide is 0-426-20442-5.
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.
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 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.
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.
interface between the crust and the upper mantle
The Gutenberg Discontinuity is a boundary within the Earth's interior that separates the outer core from the lower mantle. It is characterized by a rapid increase in seismic wave velocities, indicating a change in composition and physical properties. The Gutenberg Discontinuity is located at a depth of about 2,900 kilometers (1,800 miles) beneath the Earth's surface.