Rock Identifier
Epidote (Calcium aluminum iron silicate (Ca2(Al, Fe)3(SiO4)3(OH))) — mineral
mineral

Epidote

Calcium aluminum iron silicate (Ca2(Al, Fe)3(SiO4)3(OH))

Hardness: 6-7 on Mohs scale; Color: Pistachio-green to yellowish-green; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in one direction; Specific gravity: 3.3-3.6

Hardness
6-7 on Mohs scale
Color
Pistachio-green to yellowish-green
Luster
Vitreous to pearly
Identified More mineral
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Physical properties

Hardness: 6-7 on Mohs scale; Color: Pistachio-green to yellowish-green; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect in one direction; Specific gravity: 3.3-3.6

Formation & geological history

Formed through regional or contact metamorphism of calcium-rich rocks like basalt, limestone, or shale. It also occurs in hydrothermal veins and altered igneous rocks.

Uses & applications

Primarily a collector mineral and used as a minor gemstone (Unakite) in jewelry and landscaping. In industry, it can be an indicator mineral for copper and gold deposits.

Geological facts

The name comes from the Greek word 'epidosis,' meaning 'addition,' in reference to its characteristic crystal geometry being unequal in length at the base.

Field identification & locations

Identify in the field by its distinct 'pistachio green' color and hardness. Commonly found in metamorphic terrains such as the Alps and the Blue Ridge Mountains.