Rock Identifier
Likely weathered granite or granitic gneiss (Granite; mainly quartz, feldspar, and minor mica/amphibole) — igneous
igneous

Likely weathered granite or granitic gneiss

Granite; mainly quartz, feldspar, and minor mica/amphibole

AI-generated identification · may be incorrect

Gray, coarse-grained, dull to weakly sparkly, with rounded weathered surfaces and possible feldspar/quartz grains. Typical hardness is about 6–7 Mohs; massive texture and poor cleavage overall, though feldspar cleavage may be visible.

Identified More igneous
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Physical properties

Gray, coarse-grained, dull to weakly sparkly, with rounded weathered surfaces and possible feldspar/quartz grains. Typical hardness is about 6–7 Mohs; massive texture and poor cleavage overall, though feldspar cleavage may be visible.

Formation & geological history

Formed by slow crystallization of silica-rich magma deep underground, generally during Precambrian to Phanerozoic continental crust formation; surface weathering rounded the fragment.

Uses & applications

Commonly used as crushed stone, aggregate, paving, countertops, monuments, and building stone; ordinary hand specimens have little commercial value.

Geological facts

The image is slightly blurred, so exact identification is uncertain; its pale gray color and granular appearance are consistent with granite, but quartz-rich sandstone or another weathered silicate rock is possible.

Field identification & locations

Look for interlocking visible grains: glassy gray quartz, white or pink feldspar, and black mica. Common worldwide, especially in continental shield and mountain regions; a fresh broken surface is more diagnostic than the weathered exterior.