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Welcome to the Upper Mantle
Below the crust is the mantle, a layer of hot rock nearly 3,000 km thick. Like the crust, the mantle is made of rock. The rock of the upper mantle and crust, called the lithosphere, is rigid. Increased temperature and pressure cause rock that is deeper down in the mantle to flow slowly.
The asthenosphere is another part of the upper mantle, just below the lithosphere. Rock here is almost at its melting point. It is not liquid, but does flow under pressure. Think of modeling clay that gets soft when you squeeze it in the palm of your hand. This is like the rock in the asthenosphere. We describe it as plasticity.
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