Rock Identifier
Polished granite egg (Granite, chiefly quartz, feldspar, and dark mica or amphibole) — igneous
igneous

Polished granite egg

Granite, chiefly quartz, feldspar, and dark mica or amphibole

AI-generated identification · may be incorrect

Hardness about 6–7 Mohs; mottled gray, black, and cream with a yellow-brown patch, polished surface, and interlocking crystalline texture. Individual grains show no obvious cleavage; typical granite specific gravity is about 2.6–2.7.

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Physical properties

Hardness about 6–7 Mohs; mottled gray, black, and cream with a yellow-brown patch, polished surface, and interlocking crystalline texture. Individual grains show no obvious cleavage; typical granite specific gravity is about 2.6–2.7.

Formation & geological history

Granite forms when silica-rich magma cools slowly underground, allowing visible crystals to grow; granites range widely in age, from ancient Precambrian rocks to younger intrusions. The egg shape and polish are human-made.

Uses & applications

Decorative carving, desk ornament, or collectible; granite is also widely used for countertops, monuments, and building stone.

Geological facts

Granite is a rock rather than a single mineral, and its exact appearance depends on the proportions and types of feldspar, quartz, and dark minerals.

Field identification & locations

Identify it by its coarse, interlocking light and dark grains; the polished surface can make grains harder to distinguish. Granite is found on every continent, especially in continental crust and mountain belts.