Rock Identifier
Tumbled granite (Granite, chiefly quartz, feldspar, and mica) — igneous
igneous

Tumbled granite

Granite, chiefly quartz, feldspar, and mica

AI-generated identification · may be incorrect

Coarse-grained, massive texture with pale pink/white feldspar, gray quartz, and dark mica or amphibole; vitreous to dull luster, no obvious cleavage as a whole, Mohs hardness about 6–7, and specific gravity roughly 2.63–2.75.

Identified More igneous
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Physical properties

Coarse-grained, massive texture with pale pink/white feldspar, gray quartz, and dark mica or amphibole; vitreous to dull luster, no obvious cleavage as a whole, Mohs hardness about 6–7, and specific gravity roughly 2.63–2.75.

Formation & geological history

Granite is an intrusive igneous rock formed when silica-rich magma cooled slowly deep within continental crust, producing visible crystals. Its exact age cannot be determined from the image; granite ranges from Precambrian to geologically recent.

Uses & applications

Used for countertops, building stone, monuments, paving, aggregate, and decorative tumbled specimens; this piece has modest lapidary and collecting value.

Geological facts

The rounded shape and polished surface indicate human tumbling, while the contrasting mineral patches are typical of weathered or altered granite.

Field identification & locations

Identify it by visible interlocking quartz and feldspar grains, pink coloration, and scattered dark minerals; common sources include continental mountain belts worldwide, especially India, Brazil, Canada, and the United States.