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The asthenosphere is ductile and can be pushed and deformed like silly putty in response to the warmth of the Earth. These rocks actually flow, moving in response to the stresses placed upon them by the churning motions of the deep interior of the Earth. The flowing asthenosphere carries the lithosphere of the Earth, including the continents, on its back.
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Which is more viscous the asthenosphere or the mantle?
The asthenosphere is less viscous than the mantle. The asthenosphere is partially molten, allowing it to flow more easily under tectonic plates, while the mantle is solid but capable of flowing over long periods of time due to its high temperature and pressure.
What are the layers of the mantle?
The mantle is divided into two main layers: the upper mantle and the lower mantle. The upper mantle is further divided into the lithosphere and the asthenosphere. The lithosphere is rigid and made up of the crust and the upper part of the mantle, while the asthenosphere is semi-molten and capable of flowing.
Is the asthenosphere relatively cool and rigid shell that overlies the lithosphere?
Yes, the cool and rigid shell is the asthenosphere.
Because of the high temperatures and extreme pressure rocks in the asthenosphere are?
soft and flowingsoft and flowing
A layer of slowly flowing rock in the mantle?
This layer is known as the asthenosphere and it lies just below the lithosphere. It is semi-solid and ductile, allowing tectonic plates to move on its surface. The asthenosphere plays a crucial role in the movement of Earth's tectonic plates.
What is unique about the rock in the asthenosphere?
The rock in the asthenosphere is partially molten, allowing it to flow and deform slowly under pressure. This unique property makes the asthenosphere capable of supporting the movement of tectonic plates on Earth's surface.
Can living things be found in the asthenosphere?
No, living things cannot be found in the asthenosphere. The asthenosphere is a region of the Earth's mantle that consists of hot, solid rock that is capable of flowing over long periods of time. Conditions in the asthenosphere are too extreme to support life.
What layer in earth has flowing rocks?
The Asthenosphere.
Which is more viscous the asthenosphere or the mantle?
The asthenosphere is less viscous than the mantle. The asthenosphere is partially molten, allowing it to flow more easily under tectonic plates, while the mantle is solid but capable of flowing over long periods of time due to its high temperature and pressure.
What are the layers of the mantle?
The mantle is divided into two main layers: the upper mantle and the lower mantle. The upper mantle is further divided into the lithosphere and the asthenosphere. The lithosphere is rigid and made up of the crust and the upper part of the mantle, while the asthenosphere is semi-molten and capable of flowing.
Which of the Earths layers is made of hot slowly flowing rock?
Hot, slowly flowing rock comprises the asthenosphere, which is part of the mantle.
Is the asthenosphere relatively cool and rigid shell that overlies the lithosphere?
Yes, the cool and rigid shell is the asthenosphere.
Because of the high temperatures and extreme pressure rocks in the asthenosphere are?
soft and flowingsoft and flowing
Partially molten, plastic-like, flowing layer located below the solid part of Earths mantle?
Partially molten, plastic like, flowing layer located below the solid part of Earth's mantle is the Asthenosphere. The asthenosphere is mechanically weak and ductiley deforming region of the upper mantle.
Why is the asthenosphere not capable of storing elastic energy?
astic energy can only be stored in cold, brittle rocks.
A layer of slowly flowing rock in the mantle?
This layer is known as the asthenosphere and it lies just below the lithosphere. It is semi-solid and ductile, allowing tectonic plates to move on its surface. The asthenosphere plays a crucial role in the movement of Earth's tectonic plates.
Which layer has a flowing solid part?
The layer of the Earth that has a flowing solid part is the asthenosphere. Situated beneath the lithosphere, the asthenosphere consists of partially molten rock that can flow slowly over geological time. This characteristic allows tectonic plates to move on top of it, contributing to geological activities such as earthquakes and volcanic eruptions.
