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The inner core of the earth has a temperature of about 5700 degrees C. About the same as the surface of the Sun. Above this is the outer core, which has a similar temperature, but as it is under less pressure, it is molten.

This molten material undergoes convection and this is the primary driving force for the movement of the magma just below the crust. There appear to be some stationary 'hot spots' of which Hawaii and Iceland are conspicuous examples. Even though the plates there are moving, the hot spot seems stationary.

So magma is just a hot liquid form of rock. Not necessarily very viscous.

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14y ago

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