Rock Identifier
Rounded quartz-rich rock, likely granitic pebble (Weathered granite or granitic pegmatite; chiefly quartz (SiO₂) with feldspar and minor mica) — igneous
igneous

Rounded quartz-rich rock, likely granitic pebble

Weathered granite or granitic pegmatite; chiefly quartz (SiO₂) with feldspar and minor mica

AI-generated identification · may be incorrect

Light cream-gray, coarse granular texture with visible interlocking crystals and dull-to-glassy luster; quartz hardness 7, feldspar 6, overall hardness about 6–7 Mohs. No obvious cleavage is visible because the specimen is naturally rounded and weathered.

Identified More igneous
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Physical properties

Light cream-gray, coarse granular texture with visible interlocking crystals and dull-to-glassy luster; quartz hardness 7, feldspar 6, overall hardness about 6–7 Mohs. No obvious cleavage is visible because the specimen is naturally rounded and weathered.

Formation & geological history

Likely crystallized slowly from silica-rich magma deep underground, then exposed and rounded by stream or glacial transport. Precise geological age and locality cannot be determined from the photograph.

Uses & applications

Common granite is used for aggregate, landscaping, countertops, and building stone; ordinary hand specimens generally have little commercial or collector value.

Geological facts

The pale grains are probably feldspar and quartz, while darker specks may be biotite or amphibole. The rounded shape and smoothed surface indicate significant physical weathering or transport.

Field identification & locations

Identify it by its speckled, interlocking quartz–feldspar texture, lack of layering, and inability to scratch quartz with a steel knife. Common worldwide, especially in granitic terrains and gravel deposits.