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Granites usually are classified as Igneous rocks obtained from molten masses or magmas. There is evidence that the origin of some granites may be attributed to regional metamorphism or pre-existing rocks. Rearrangement and re-crystallization taking place without a liquid or molten stage.
Granite may occur in dikes or sills (tabular bodies injected in fissures and inserted between other rocks), but more characteristically it forms irregular masses of extremely variable size, ranging from less than eight kilometres (five miles) in maximum dimension to larger masses (batholiths) that are often hundreds or thousands of square kilometres in area.
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Adoni Brown |
Amarello Real |
Aqua Marina |
Arco Baleno |
Atibaia |
Autumn Brown |
Azul Aran |
Azul Bahia |
Baltic Brown |
Baltic Green |
Barre Grey |
Bethel White |
Bianco Cardinalle. |
Bianco Castilla |
BiancoC
opacabana |
Bianco Cristalle |
Bianco Montorfano |
Bianco Regina |
Bianco Sardo |
Blue Eyes |
Blue King |
Blue PearlT |
Brasil Violet |
Caesar White |
Caledonia |
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