Rock Identifier
Polished unakite (Unakite: epidote, pink feldspar (commonly orthoclase), and quartz; a granitic rock altered by epidotization) — metamorphic
metamorphic

Polished unakite

Unakite: epidote, pink feldspar (commonly orthoclase), and quartz; a granitic rock altered by epidotization

AI-generated identification · may be incorrect

Hardness about 6–7 Mohs; mottled orange-pink and olive green, with a polished vitreous-to-waxy luster. It is a coarse-grained aggregate, not a single crystal, so cleavage varies by constituent mineral.

Identified More metamorphic →
Explore Polished unakite in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness about 6–7 Mohs; mottled orange-pink and olive green, with a polished vitreous-to-waxy luster. It is a coarse-grained aggregate, not a single crystal, so cleavage varies by constituent mineral.

Formation & geological history

Forms when fluids alter granitic rock, converting some minerals to green epidote while feldspar and quartz remain. Its age depends on the source granite; classic unakite comes from the Appalachian region.

Uses & applications

Used for beads, cabochons, carvings, and decorative stone; generally unsuitable for heavy-duty construction.

Geological facts

Named after the Unaka Mountains of North Carolina, where it was first described.

Field identification & locations

Identify by its distinctive mottled salmon-pink/orange feldspar and green epidote pattern; it is commonly collected in the Appalachians and sold as polished pieces. The photograph is consistent with unakite, though image-only identification is not definitive.