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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.
What is the three difference between Mohorovicic discontinuity and Gutenberg discontinuity?
The Mohorovicic discontinuity, or Moho, is the boundary between the Earth's crust and the underlying mantle, characterized by a significant increase in seismic wave velocity due to the transition from less dense rocks to denser mantle materials. In contrast, the Gutenberg discontinuity marks the boundary between the Earth's mantle and the outer core, where there is a dramatic change in composition and state, transitioning from solid mantle rock to the liquid iron-nickel alloy of the outer core. Additionally, the depth of the Moho varies between about 5 to 70 kilometers, while the Gutenberg discontinuity is found at a depth of approximately 2,900 kilometers. Thus, these discontinuities represent different layers within the Earth's structure, each with distinct physical and chemical properties.
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?
Mohorovicic discontinuity is located between the upper mantle and the crust, while the Gutenberg discontinuityis located between the lower mantle and the outer core.
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.
What is the three difference between Mohorovicic discontinuity and Gutenberg discontinuity?
The Mohorovicic discontinuity, or Moho, is the boundary between the Earth's crust and the underlying mantle, characterized by a significant increase in seismic wave velocity due to the transition from less dense rocks to denser mantle materials. In contrast, the Gutenberg discontinuity marks the boundary between the Earth's mantle and the outer core, where there is a dramatic change in composition and state, transitioning from solid mantle rock to the liquid iron-nickel alloy of the outer core. Additionally, the depth of the Moho varies between about 5 to 70 kilometers, while the Gutenberg discontinuity is found at a depth of approximately 2,900 kilometers. Thus, these discontinuities represent different layers within the Earth's structure, each with distinct physical and chemical properties.
Who discovered mohorovicic distensity?
Andriza Mohorovicic, discover the mohorovicic discontinuity or we called moho Moho is the boundery between the crust and the mantle
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.
