Rock Identifier
Polished granite sphere (Granite, chiefly quartz, alkali feldspar, and plagioclase with dark biotite/amphibole minerals) — igneous
igneous

Polished granite sphere

Granite, chiefly quartz, alkali feldspar, and plagioclase with dark biotite/amphibole minerals

AI-generated identification · may be incorrect

Fine- to medium-grained, pale gray with black mineral speckles and a polished surface; hardness about 6–7 Mohs, granular crystal structure, no prominent cleavage as a whole, and specific gravity around 2.6–2.8.

Identified More igneous
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Physical properties

Fine- to medium-grained, pale gray with black mineral speckles and a polished surface; hardness about 6–7 Mohs, granular crystal structure, no prominent cleavage as a whole, and specific gravity around 2.6–2.8.

Formation & geological history

An intrusive igneous rock crystallized slowly from silica-rich magma deep underground, generally during Precambrian to Phanerozoic mountain-building events. The sphere is human-cut and polished.

Uses & applications

Used for decorative spheres, countertops, monuments, flooring, and construction aggregate; collectible value is usually modest unless the stone has unusual color or provenance.

Geological facts

The black grains are commonly biotite mica or hornblende, while the light grains are feldspar and quartz. Granite’s visible interlocking crystals indicate slow cooling rather than volcanic eruption.

Field identification & locations

Identify it by its hard, speckled, interlocking texture and resistance to scratching; a steel knife usually will not scratch it. Common sources include India, Brazil, China, Scandinavia, and North America.