Rock Identifier
Epidotite (Epidotite (Epidote content > 50%)) — metamorphic
metamorphic

Epidotite

Epidotite (Epidote content > 50%)

Hardness: 6-7 Mohs; 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 Mohs
Color
Pistachio-green to yellowish-green
Luster
Vitreous to pearly
Identified More metamorphic
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Physical properties

Hardness: 6-7 Mohs; 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 the regional or hydrothermal metamorphism of mafic igneous rocks (like basalt) or calcium-rich sediments. It typically develops in low to medium-grade metamorphic facies like the greenschist facies.

Uses & applications

Mostly used as decorative stone, for cabochons in jewelry, and as a component in aggregate for construction. It is also a significant specimen for collectors studying metamorphic sequences.

Geological facts

The characteristic pistachio-green color is diagnostic and caused by the presence of iron. It is often found associated with quartz, chlorite, and calcite.

Field identification & locations

Identify in the field by its distinct 'pistachio' green color and high hardness (will scratch glass). Commonly found in the Alps, Ural Mountains, and parts of the United States like New England and North Carolina.