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What is the asthenosphere and what is it made of?

What is the asthenosphere and what is it made of?

The asthenosphere is solid upper mantle material that is so hot that it behaves plastically and can flow.

What is the asthenosphere and what does it do?

The asthenosphere is a part of the upper mantle just below the lithosphere that is involved in plate tectonic movement and isostatic adjustments.

What is the asthenosphere your answer?

The asthenosphere is the denser, weaker layer beneath the lithospheric mantle. It lies between about 100 kilometers (62 miles) and 410 kilometers (255 miles) beneath Earth’s surface. The temperature and pressure of the asthenosphere are so high that rocks soften and partly melt, becoming semi-molten.

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What is a asthenosphere easy definition?

Definition of asthenosphere : a zone of a celestial body (such as the earth) which lies beneath the lithosphere and within which the material is believed to yield readily to persistent stresses.

What is the asthenosphere made of kids?

The asthenosphere is the layer of the Earth that lies below the lithosphere. It is a layer of solid rock where the extreme pressure and heat cause the rocks to flow like a liquid. The rocks in the asthenosphere are not as dense as the rocks in the lithosphere.

What kind of material is the asthenosphere is made of and how does it behave?

What is the density of the asthenosphere?

about 3.3 g/cc
-Asthenosphere – mean density about 3.3 g/cc. Denser and hotter than lithosphere above. under tremendous pressure and heat so that it is “soft”, near melting point, and flows plastically.

What is the function of asthenosphere in plate tectonics?

Heat from deep within Earth is thought to keep the asthenosphere malleable, lubricating the undersides of Earth’s tectonic plates and allowing them to move. Convection currents generated within the asthenosphere push magma upward through volcanic vents and spreading centres to create new crust.

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What is the densest layer of Earth?

The inner core
The inner core is at the center of the Earth because it is the densest, made of solid iron and nickel.

What is the asthenosphere quizlet?

asthenosphere. the upper layer of the earth’s mantle, below the lithosphere, in which there is relatively low resistance to plastic flow and convection is thought to occur. plate tectonics theory.

What are 3 facts about the asthenosphere?

  • The asthenosphere lubricates plate tectonics. The asthenosphere is the unsung hero of our planet.
  • The asthenosphere is unique to Earth. The asthenosphere is unique to our planet.
  • Convection cells occur in the asthenosphere.
  • Asthenosphere composition and structure.
  • Glaciers compress the asthenosphere.

How do scientists describe the asthenosphere?

The asthenosphere is solid upper mantle material that is so hot that it behaves plastically and can flow. The lithosphere rides on the asthenosphere.

How dense is the asthenosphere?

The mantle extends from the base of the crust to a depth of about 2900 km (1800 mi). Except for the zone known as the asthenosphere, it is solid, and its density, increasing with depth, ranges from 3.3 to 6 g/cm3.

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Is the asthenosphere is hotter than the lithosphere?

Asthenosphere. It is hotter than the lithosphere because it is closer to the inner core. Inside the asthenosphere and lithosphere are currents, they are called convection currents. So because the asthenosphere is less dense or lighter than the lithosphere is forces its way up to the top and foces the lithosphere down.

How hot is the asthenosphere?

The asthenosphere is solid even though it is at very hot temperatures of about 1600 C due to the high pressures from above. However, at this temperature, minerals are almost ready to melt and they become ductile and can be pushed and deformed like silly putty in response to the warmth of the Earth.

Is the asthenosphere below the lithosphere?

The asthenosphere (from Greek ἀσθενής asthenḗs ‘weak’ + “sphere”) is the highly viscous, mechanically weak and ductilely deforming region of the upper mantle of the Earth. It lies below the lithosphere, at depths between approximately 80 and 200 km (50 and 120 miles) below the surface.