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The Mohorovičić discontinuity, also known as the Moho, marks the boundary between the Earth's crust and mantle. It is identified by a sudden increase in seismic wave velocities, indicating a change in rock density and composition at this boundary.
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What is the difference between the Mohorovicic discontinuity and the Gutenberg discontinuity?
The Mohorovicic discontinuity (Moho) is the boundary between the Earth's crust and mantle, where seismic waves change velocity. The Gutenberg discontinuity is the boundary between the Earth's mantle and outer core, characterized by a sharp increase in seismic wave velocities.
Who discovered the crust mantle seismic discontinuity?
The crust-mantle seismic discontinuity was discovered by Yugoslav seismologist, Andrija Mohorovičić, in 1909 through his observation of seismic waves. This discontinuity marks the boundary between Earth's crust and mantle, characterized by a sudden increase in seismic wave velocity.
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.
Where is the Weichert discontinuity?
The Weichert discontinuity is located at a depth of around 220-240 kilometers in the Earth's mantle, marking the boundary between the upper and lower mantle. It is a seismic discontinuity that causes a change in the velocity of seismic waves travelling through the Earth.
Who discovered the boundary between the crust and the mantle?
The boundary between the crust and the mantle was discovered by Croatian seismologist Andrija Mohorovičić in 1909. This boundary is known as the Mohorovičić discontinuity or "Moho" and marks the change in seismic wave velocities between the Earth's crust and mantle.
Is the boundary between the liquid core and mantle known as the Moho?
Yes, the boundary between the liquid outer core and the solid mantle is known as the Gutenberg discontinuity. The Mohorovičić discontinuity, or Moho, is the boundary between the Earth's crust and the mantle.
What is the difference between the Mohorovicic discontinuity and the Gutenberg discontinuity?
The Mohorovicic discontinuity (Moho) is the boundary between the Earth's crust and mantle, where seismic waves change velocity. The Gutenberg discontinuity is the boundary between the Earth's mantle and outer core, characterized by a sharp increase in seismic wave velocities.
What is the difference between Mohorovicic discontinuity and Gutenberg discontinuity?
The Mohorovicic discontinuity, or Moho, is the boundary between the Earth's crust and mantle, marking a change in seismic wave velocity. The Gutenberg discontinuity is the boundary between the Earth's mantle and outer core, where seismic waves change velocity and nature. Essentially, the Moho separates the crust and mantle, while the Gutenberg discontinuity separates the mantle and outer core.
Who discovered the crust mantle seismic discontinuity?
The crust-mantle seismic discontinuity was discovered by Yugoslav seismologist, Andrija Mohorovičić, in 1909 through his observation of seismic waves. This discontinuity marks the boundary between Earth's crust and mantle, characterized by a sudden increase in seismic wave velocity.
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.
It separates the mantle and the crust?
The Mohorovicic Discontinuity (also known as the Moho) separates the Earth's crust from the underlying mantle. It is the boundary where seismic waves change speed, indicating a change in composition and density between the two layers.
Is the boundary between the crust and upper mantle?
The boundary between the crust and upper mantle is known as the Mohorovičić discontinuity or Moho. It represents the change in seismic wave velocity and composition between the rigid outer layer (crust) and the more ductile layer beneath (mantle).
The Mohorovicic discontinuity occurs between the crust and the?
The Mohorovicic discontinuity occurs between the Earth's crust and the mantle. It marks the boundary where seismic waves change speed, indicating a change in the composition of the Earth's layers.
Boundary between earth's crust and mantle?
It is called the Mohorovičić discontinuity or the Moho for short.It was one of the fist features of the Earth's interior that was discovered using seismic waves. In 1909, Andrija Mohorovicic discovered this boundary and it was named in his honor.
What is the moho in the earths layers?
The Moho, short for Mohorovičić discontinuity, is a boundary between the Earth's crust and the mantle. It marks a significant change in seismic wave velocities, indicating the transition from the less dense, rigid crust to the more dense, flowing mantle beneath.
Where is the Weichert discontinuity?
The Weichert discontinuity is located at a depth of around 220-240 kilometers in the Earth's mantle, marking the boundary between the upper and lower mantle. It is a seismic discontinuity that causes a change in the velocity of seismic waves travelling through the Earth.
What the boundary between the core and mantle?
The boundary of mantle and core are called Gutenberg Discontinuity
