Rock Identifier
Weathered granite or granitic gneiss pebble (Granite, primarily quartz, feldspar, and mica; exact identification is uncertain from the image) — igneous
igneous

Weathered granite or granitic gneiss pebble

Granite, primarily quartz, feldspar, and mica; exact identification is uncertain from the image

AI-generated identification · may be incorrect

Light gray, fine- to medium-grained, with faint darker mineral flecks and a dull weathered luster; likely hardness 6–7 Mohs, massive or weakly foliated, with no obvious cleavage as a whole rock.

Identified More igneous
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Physical properties

Light gray, fine- to medium-grained, with faint darker mineral flecks and a dull weathered luster; likely hardness 6–7 Mohs, massive or weakly foliated, with no obvious cleavage as a whole rock.

Formation & geological history

Likely formed by slow crystallization of silica-rich magma deep in the crust, commonly during Precambrian to younger continental tectonic events, then exposed and rounded by weathering and transport.

Uses & applications

Common granitic material is used as crushed aggregate, dimension stone, pavers, and monuments; this small specimen has mainly educational or modest collecting value.

Geological facts

The pale grains are probably feldspar and quartz, while darker specks may be biotite or amphibole. The subtle banding could indicate gneiss rather than ordinary granite.

Field identification & locations

Look for interlocking visible grains, abundant pale feldspar/quartz, and scattered dark mica; a fresh broken surface, streak, and hand lens would improve identification. Granitic rocks occur widely on continental shields and mountain belts worldwide.