metamorphic

Unakite (likely)

Epidote–pink feldspar–quartz aggregate; commonly classified as altered granite

AI-generated identification · may be incorrect

Hardness about 6–7 Mohs; mottled pistachio-green, salmon-pink, and cream; generally opaque with a dull to weakly vitreous luster. Massive, granular, and lacking visible cleavage in the rounded specimen.

Identified September 14, 2026More metamorphic →

Explore Unakite (likely) in the encyclopedia →

Identify your own rocks.

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

App Store Google Play

Physical properties

Formation & geological history

Forms when granite undergoes hydrothermal alteration, replacing dark minerals with green epidote while preserving pink orthoclase and quartz. It is mainly Paleozoic to Precambrian in age, depending on locality.

Uses & applications

Used as tumbled stone, cabochons, beads, carvings, and decorative aggregate; occasionally used for countertops and ornamental stone. Common specimens have modest collector value.

Geological facts

The name comes from the Unaka Mountains of Tennessee and North Carolina, where classic material occurs. The image’s color pattern is consistent with unakite, though similar epidote-rich rocks can look nearly identical.

Field identification & locations

Identify by the distinctive green-and-salmon mottling, granular texture, and lack of banding; it is commonly found in altered granitic terrains and river gravels. A polished surface shows stronger color contrast.