Rock Identifier
Rounded granite pebble (Granite, chiefly quartz, potassium feldspar, and plagioclase with minor mica or amphibole) — igneous
igneous

Rounded granite pebble

Granite, chiefly quartz, potassium feldspar, and plagioclase with minor mica or amphibole

AI-generated identification · may be incorrect

Fine- to medium-grained, gray and speckled, with a dull to slightly granular luster; hardness about 6–7 Mohs, massive structure, no cleavage as a whole, and typical specific gravity 2.6–2.7.

Identified More igneous →
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Physical properties

Fine- to medium-grained, gray and speckled, with a dull to slightly granular luster; hardness about 6–7 Mohs, massive structure, no cleavage as a whole, and typical specific gravity 2.6–2.7.

Formation & geological history

An intrusive igneous rock crystallized slowly from silica-rich magma, commonly millions to billions of years ago; its rounded shape reflects river, beach, or glacial abrasion.

Uses & applications

Used as aggregate, paving stone, building stone, countertops, and landscaping material; this small specimen has minimal commercial value.

Geological facts

The interlocking grains indicate slow underground cooling. Individual quartz grains should scratch glass, while feldspar commonly shows flat cleavage surfaces.

Field identification & locations

Common worldwide, especially in continental shields and mountain ranges. Identify it by its coarse interlocking gray, white, and black grains, lack of layering, and inability to fizz with dilute acid; exact identification is limited by the small image.