Foremost of these are magma viscosity, gas loss and external properties such as conduit geometry. Ultimately, these parameters control the speed at which magmas ascend, decompress and outgas en route to the surface, and thus determine eruptive style and evolution.
It's made up of silicate minerals. aluminum and granite, the types of silicate minerals are quarts, micas, and feldspars.
Answer:
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Explanation:
The Atlantic Ocean is the correct answer for this equation
