Rock Identifier
Tumbled unakite (Unakite: epidote, pink potassium feldspar (orthoclase), and commonly quartz) — metamorphic
metamorphic

Tumbled unakite

Unakite: epidote, pink potassium feldspar (orthoclase), and commonly quartz

AI-generated identification · may be incorrect

Opaque, mottled green and salmon-pink, with a polished surface and granular texture. Epidote and feldspar are about 6–7 on the Mohs scale; the rock has no consistent overall crystal structure or cleavage.

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Physical properties

Opaque, mottled green and salmon-pink, with a polished surface and granular texture. Epidote and feldspar are about 6–7 on the Mohs scale; the rock has no consistent overall crystal structure or cleavage.

Formation & geological history

A metamorphosed granite, formed when hydrothermal alteration converted some feldspar to epidote; unakite occurs in ancient crystalline rocks, including the Proterozoic Blue Ridge region.

Uses & applications

Used for tumbled stones, beads, carvings, and decorative objects; it has little industrial or construction use.

Geological facts

The name comes from the Unaka Mountains of North Carolina and Tennessee, where it was first described.

Field identification & locations

Identify it by its distinctive salmon-pink feldspar mixed with pistachio-green epidote, often with quartz. It is found in parts of the Appalachian Mountains and is widely sold as tumbled material.