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by Jenny SMember since:October 28, 2008Total points:6,522 (Level 5)

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Best Answer - Chosen by VotersThe previous answers are correct, but there is an additional feature resulting from cooling rates.

A magma which cools rapidly will comprise small to microscopic crystals and generally be homogeneous.

A magma which chills slowly will not only form larger crystals, but may also have time to differentiate - that is for some of the earliest crystallised materials to settle through the magma chamber if there is an adequate density contrast between minerals. This results in different compositional rock types, layering within the body, and alignment of alongate crystals. Slower cooling magmas also have the possibility of forming late stage products such as aplitic and pegmatitic bodies. They also have time to alter themselves or the adjacent rocks by passing reactive fluids through themselves and the country rock.

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How does the pH of magma affect the formation of igneous rocks?

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How is the texture of an igneous rock related to the rate which it cooled?

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Is granite formed from lava cooling or magma cooling?

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When magma is cooled it becomes what?

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What two processes results in the formation of igneous rocks?

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