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

Granite

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

AI-generated identification · may be incorrect

The specimen is pale pink, cream, and brown with coarse visible crystals and a granular texture. Typical granite hardness is about 6–7 Mohs; it has a massive structure and no distinct cleavage as a rock.

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Physical properties

The specimen is pale pink, cream, and brown with coarse visible crystals and a granular texture. Typical granite hardness is about 6–7 Mohs; it has a massive structure and no distinct cleavage as a rock.

Formation & geological history

Granite forms when silica-rich magma cools slowly deep in continental crust, allowing large crystals to grow. Its exact age cannot be determined from the photograph.

Uses & applications

Granite is widely used for building stone, countertops, paving, monuments, and landscaping; this rough specimen is mainly suitable for collecting or display.

Geological facts

Quartz and feldspar make up most granite, while darker flecks commonly consist of biotite or other accessory minerals.

Field identification & locations

Look for interlocking, centimeter-scale crystals and a mix of light quartz/feldspar with darker minerals; granite is common in continental mountain belts worldwide. The image supports a granite-like identification, though composition cannot be confirmed visually alone.