The asthenosphere is in a semi-molten state because of high temperatures and pressure. The combination of these factors causes the rocks in the asthenosphere to deform and flow slowly, giving it its semi-molten properties. This allows the tectonic plates to move and interact with each other.
Temperature is relatively uniform throughout the asthenosphere due to its semi-molten state. This consistent temperature allows for the flow of material within the asthenosphere, contributing to the movement of tectonic plates.
It is called the asthenosphere.
asthenosphere
Matter in the Asthenosphere is in the molten or semi-molten state. This is because its temperatures can peak at 3,000 degrees Celsius. Its composition consists of magnesium and iron silicates. The Asthenosphere plays a key role in the movement of tectonic plates.
It's called the asthenosphere.
the two mantles are pie and pencil
The asthenosphere is in a semi-molten state because of high temperatures and pressure. The combination of these factors causes the rocks in the asthenosphere to deform and flow slowly, giving it its semi-molten properties. This allows the tectonic plates to move and interact with each other.
Temperature is relatively uniform throughout the asthenosphere due to its semi-molten state. This consistent temperature allows for the flow of material within the asthenosphere, contributing to the movement of tectonic plates.
Asthenosphere
The asthenosphere is a partially molten layer of the Earth's upper mantle. It is in a plastic state, meaning that it can flow slowly under stress but is not completely liquid. This characteristic allows for the movement of tectonic plates.
Solid
The partially molten layer of Earth's mantle is called the asthenosphere. It is located below the lithosphere and is responsible for the movement of tectonic plates due to its semi-fluid state. The asthenosphere facilitates the process of mantle convection, which drives the motion of Earth's lithospheric plates.
It is called the asthenosphere.
The asthenosphere, located in the upper mantle, is easily deformed due to its semi-molten state. This layer allows tectonic plates to move on the ductile rock beneath them.
asthenosphere
they sit on the asthenosphere