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Igneous rocks
are broken into a number of categories based on grain size and composition
- these also match color and cooling history features. |
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Grain Size -
this depends on the time the rocks had to cool and can be divided into
two groups:
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Fine grained
rapidly cooled surface formed rocks - Aphanitic |
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Course grained
slow cooled deep formed rocks - Phaneritic |
|
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Composition
- determined by the relative abundance of Iron and magnesium on one hand
and Aluminum and Silica on the other:
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Felsic - rich
in Aluminum and Silica and low in in mafics - light colored. |
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Mafic - rich
in Iron and magnesium and relatively low in Aluminum and Silica - dark
colored. |
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