Rock Identifier
Rounded granitic pebble (likely granite or granodiorite) (Granite–granodiorite; chiefly quartz, feldspar, and mica/amphibole) — igneous
igneous

Rounded granitic pebble (likely granite or granodiorite)

Granite–granodiorite; chiefly quartz, feldspar, and mica/amphibole

AI-generated identification · may be incorrect

Coarse crystalline, speckled gray, white, tan, and black grains with a dull to weakly vitreous luster; quartz hardness ~7, feldspar ~6, overall Mohs ~6–7. No obvious cleavage on the rounded surface; density typically 2.6–2.8 g/cm³.

Identified More igneous
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Physical properties

Coarse crystalline, speckled gray, white, tan, and black grains with a dull to weakly vitreous luster; quartz hardness ~7, feldspar ~6, overall Mohs ~6–7. No obvious cleavage on the rounded surface; density typically 2.6–2.8 g/cm³.

Formation & geological history

Slowly cooled silica-rich magma formed intrusive igneous rock, commonly during Precambrian–Phanerozoic mountain-building; its smooth shape results from stream or beach abrasion. Exact age and provenance require petrographic or geochemical testing.

Uses & applications

Used as aggregate, road stone, building stone, monuments, and landscaping material; attractive pieces may be polished as decorative specimens, but this rounded example has modest commercial value.

Geological facts

The visible interlocking crystals and mixed light/dark minerals distinguish it from homogeneous basalt or sedimentary pebbles. Brown coloration likely reflects iron-oxide weathering.

Field identification & locations

Identify by visible quartz and feldspar grains, granular texture, and lack of layering or foliation; common worldwide in glacial deposits, rivers, beaches, and areas exposing continental crust.