The general pattern of magma circulation in the mantle is ; upwards and downwards towards the earth crust
The mantle is situated between the solid crust making up the earth surface and Earth's outer core and it is made of molten rocks which are heated up due to high pressures.
The mantle ( semisolid molten magma ) experiences an upward pattern of magma circulation and this is caused by mantle convection currents.
Hence we can conclude that the general pattern of magma circulation in the mantle is Upwards and downwards towards the crust.
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