Think about the asthenosphere. The molten rocks in this area are so hot, they flow like a fluid. Heat moves from warm areas to cooler areas. As the cool areas heat up, they become less dense and rise. Then they cool and sink. This circular pattern is called a convection current. The convection currents just beneath the earth's crust flow very slowly, causing movement in the earth's plates above them.
The slow creeping motion of Earth's solid silicate mantle caused by convection currents carrying heat from the interior to the planet's surface. Mantle convection is the very slow creeping motion of Earth's solid silicate mantle caused by convection currents carrying heat from the interior to the planet's surface.
The mantle is solid despite high temperatures because of high lithostatic pressures.
The mantle is solid. It only melts in special cases very near the surface.
solid
The mantle layer of the Earth is said to be "solid-plastic". This means that it is a solid, but it can be moved.
Yes the upper mantle is solid. The lower mantle however is not.
it is solid.
It is the ability of the mantle (solid) to flow like liquid.
it is a solid.
No. The mantle is solid.
solid
the lower mantle of earth is a solid
The mantle layer of the Earth is said to be "solid-plastic". This means that it is a solid, but it can be moved.
Both. The upper mantle is solid and the lower mantle is liquid.
Yes the upper mantle is solid. The lower mantle however is not.
yes it is solid
it is solid.
solid
solid
Igneous rock