Rock Identifier
Weathered granite (likely granitic gneiss) (Granite; predominantly quartz, feldspar, and mica) — igneous
igneous

Weathered granite (likely granitic gneiss)

Granite; predominantly quartz, feldspar, and mica

AI-generated identification · may be incorrect

Coarse-grained, pale gray to whitish, with dark mica/amphibole flecks; crystalline texture, vitreous quartz luster, Mohs hardness about 6–7, poor cleavage overall, and specific gravity roughly 2.63–2.75. Strong surface weathering has produced pits and rounded edges.

Identified More igneous
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Physical properties

Coarse-grained, pale gray to whitish, with dark mica/amphibole flecks; crystalline texture, vitreous quartz luster, Mohs hardness about 6–7, poor cleavage overall, and specific gravity roughly 2.63–2.75. Strong surface weathering has produced pits and rounded edges.

Formation & geological history

Granite crystallizes slowly from silica-rich magma deep in continental crust, commonly during Precambrian to Phanerozoic mountain-building events; exact age cannot be determined from the image. Weathering and erosion exposed and shaped this specimen.

Uses & applications

Widely used as dimension stone, countertops, paving, monuments, aggregate, and landscaping rock; ordinary weathered pieces have little decorative or collector value.

Geological facts

Quartz appears glassy and gray, while feldspar commonly weathers to chalky white. The image does not show diagnostic banding clearly enough to confirm gneiss rather than granite.

Field identification & locations

Common in continental shields, mountain belts, and glacial or stream deposits. Identify with a hand lens, hardness test, and dilute acid test (no fizz expected); feldspar cleavage and quartz grains help distinguish it from limestone.