0
What is the three difference between Mohorovicic discontinuity and Gutenberg discontinuity?
Want this question answered?
Be notified when an answer is posted
Add your answer:
Earn +20 pts
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.
mohorovicic discontinuity?
interface between the crust and the upper mantle
Where did mohorovicic discontinuity get its name?
The Mohorovicic discontinuity is named after Croatian seismologist Andrija Mohorovicic, who first discovered it in 1909. It marks the boundary between the Earth's crust and the mantle and is characterized by a sudden increase in seismic wave velocity.
Who is the discoverer of mohorovicic discontinuity?
Andriza Mohorovicic discovered the Mohorovicic discontinuity popularly known as Moho It is the boundary between the crust and the mantle it is about 2,880 kilometers thick. it is the thickest part of the earth's layer
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.
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.
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.
mohorovicic discontinuity?
interface between the crust and the upper mantle
Where did mohorovicic discontinuity get its name?
The Mohorovicic discontinuity is named after Croatian seismologist Andrija Mohorovicic, who first discovered it in 1909. It marks the boundary between the Earth's crust and the mantle and is characterized by a sudden increase in seismic wave velocity.
Who discovered mohorovicic distensity?
Andrija Mohorovicic, a Croatian seismologist, discovered the Mohorovicic discontinuity in 1909. This boundary between the Earth's crust and mantle was named in his honor.
The mohorovicic discontinuity occur between the crust and the?
mantle
What is the boundary between the mantle and outercore?
the Mohorovicic Discontinuity
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.
Where is the Moho locate?
The Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.
Who is the discoverer of mohorovicic discontinuity?
Andriza Mohorovicic discovered the Mohorovicic discontinuity popularly known as Moho It is the boundary between the crust and the mantle it is about 2,880 kilometers thick. it is the thickest part of the earth's layer
What do you call the plastic zone between the mantle and the crust?
Mohorovicic discontinuity (or simply Moho)
Who discovered Gutenberg Discontinuity?
The Gutenberg Discontinuity was discovered by Beno Gutenberg and Charles Francis Richter in the early 20th century. It is a boundary within the Earth's interior where seismic waves change velocity, indicating a change in composition between the outer core and the lower mantle.
