Rock Identifier
Polished multicolored granite (Granite, a coarse-grained felsic intrusive igneous rock composed mainly of quartz, feldspar, and mica) — igneous
igneous

Polished multicolored granite

Granite, a coarse-grained felsic intrusive igneous rock composed mainly of quartz, feldspar, and mica

AI-generated identification · may be incorrect

Mottled gray, cream, pink-orange, and black grains with a granular texture and vitreous-to-dull mineral luster. Typical Mohs hardness is about 6–7; interlocking crystals have no consistent cleavage as a rock.

Identified More igneous
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Physical properties

Mottled gray, cream, pink-orange, and black grains with a granular texture and vitreous-to-dull mineral luster. Typical Mohs hardness is about 6–7; interlocking crystals have no consistent cleavage as a rock.

Formation & geological history

Forms when silica-rich magma cools slowly underground, allowing visible crystals to grow; granite occurs in continental crust and ranges widely in age, from ancient Precambrian bodies to younger intrusions.

Uses & applications

Commonly used for countertops, tiles, paving, monuments, and decorative stone; polished slabs are also collected.

Geological facts

The pale grains are likely quartz and feldspar, while dark patches commonly contain biotite or amphibole; the image alone cannot confirm exact mineral proportions.

Field identification & locations

Identify granite by its visible, interlocking light and dark crystals and lack of layering. It is found worldwide in continental mountain belts and shield regions.