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wet magma is nothing but magma which is cooling down.

if wet magma touches water, it will cool down the magma.

2. Much volcanic material, magma included contains water - hence forming clouds above an active volcano. But seldom is material ejected from the throat steaming when it lands, therefore most of the moisture is rapidly dissipated.

Volcanic glasses can occasionally contain water, under large pressure and temperature, and upon the explosive ejection, may form pumice or ignimbrite.

Presumably the water in the magma was entrained during the subduction phase of the cycle.

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