Rock Identifier
Epidote (Epidote (Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH))) — metamorphic
metamorphic

Epidote

Epidote (Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH))

Hardness: 6-7 Mohs; Color: Pistachio green, yellowish-green, or brownish-green; Luster: Vitreous to resinous; Crystal structure: Monoclinic; Cleavage: Perfect in one direction; Specific gravity: 3.3 to 3.5.

Hardness
6-7 Mohs
Color
Pistachio green, yellowish-green, or brownish-green
Luster
Vitreous to resinous
Identified More metamorphic

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Physical properties

Hardness: 6-7 Mohs; Color: Pistachio green, yellowish-green, or brownish-green; Luster: Vitreous to resinous; Crystal structure: Monoclinic; Cleavage: Perfect in one direction; Specific gravity: 3.3 to 3.5.

Formation & geological history

Forms during low-to-medium grade regional metamorphism of calcium-rich rocks like basalt, gabbro, or limestone. It also occurs in hydrothermal veins and contact metamorphic zones.

Uses & applications

Used primarily as a collector's mineral and sometimes as a semi-precious gemstone. In massive forms (like Unakite), it is used for decorative carvings, beads, and architectural stone.

Geological facts

The name 'Epidote' is derived from the Greek word 'epidosis', meaning 'addition', referring to its crystal geometry with one side longer than the other at the base of the prism.

Field identification & locations

Identify in the field by its distinct 'pistachio' green color. It is commonly found in metamorphic terrains such as the Alps, United States (California, North Carolina), and Brazil. It often co-occurs with quartz and feldspar.