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Well When melted rock cool, they either cool fast or slowly. You have those that extruded to the surface and cool very fast usually have a fine grain igneous rocks. like the basalts and they are called extrusive igneous rocks. Those that cool with the earth as the magma rises are called intrusive igneous rocks and they have course grain. Eg are the Granite

Not quite...

In fact it's nothing to do with cooling rate and location.

Igneous rocks are those formed by crystallising from molten blends of metal-silicates.

Basalt and Granite are two very different rocks chemically and mineralogically. Their cooling and crystallising are not part of that difference.

Granite can be very fine-grained - it's called "aplite" - though it usually found in coarsely-crystalline forms (pegmatite, if I recall correctly, for very coarse versions).

The main difference between the two is the proportion of silica, with granite having the greater proportion. That makes it viscous when molten, leading to explosive eruptions as such volcanoes are also very gassy.

Further, granite is so by being a blend of 3 "essential minerals" - quartz, mica and felspar, with these occurring in a wide range of specific compounds.

Basalt is simpler, iron-rich, with relatively low silicon content which makes its lava fairly free-flowing.

Between these two main rocks is a bewilderingly complicated range controlled by essential and accessory minerals and the silica content. Igneous petrology is a speciality all of its own!

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How do igneous rock become metamorphic rocks?

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