Rock Identifier
Epidote with Quartz/Feldspar (Epidote (Ca2(Al, Fe)3(SiO4)3(OH)) with associated minerals in a host rock) — Mineral/Metamorphic rock
Mineral/Metamorphic rock

Epidote with Quartz/Feldspar

Epidote (Ca2(Al, Fe)3(SiO4)3(OH)) with associated minerals in a host rock

Pistachio green to dark green color, often massive or granular in river-tumbled stones. Hardness 6-7 on Mohs scale. Vitreous luster. Usually opaque in massive form.

Identified More mineral/metamorphic rock

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Physical properties

Pistachio green to dark green color, often massive or granular in river-tumbled stones. Hardness 6-7 on Mohs scale. Vitreous luster. Usually opaque in massive form.

Formation & geological history

Commonly forms in regionally metamorphosed rocks, hydrothermal alteration of igneous rocks (especially basalts), or contact metamorphism.

Uses & applications

A common mineral favored by collectors. High-quality transparent crystals are occasionally faceted as gemstones, but massive forms like this are typically collected as tumbled stones or lapidary rough.

Geological facts

Also known in a rock form as Epidosite (when primarily epidote and quartz) or Unakite (when combined with pink orthoclase feldspar and quartz).

Field identification & locations

Can be identified by its distinctive yellowish-green to deep green 'pistachio' color. Commonly found in riverbeds in areas of metamorphic or altered igneous rocks. Used as a semi-precious stone when tumbled.