Quick Facts

FormulaCa₂(Al,Fe)₃(SiO₄)(Si₂O₇)O(OH)
Crystal SystemMonoclinic
LusterVitreous
StreakGray
TransparencyTransparent to Translucent
Specific Gravity3.45

Formation & Origin

Epidote is a calcium aluminum iron silicate that forms in regional and contact metamorphic rocks, particularly in greenschist facies conditions. Its name comes from the Greek 'epidosis' meaning 'increase' - referring to the crystal's base having one side longer than the other.

Epidote's distinctive pistachio to dark olive green color comes from iron (Fe³⁺) in its structure. The more iron present, the darker the green - the finest gem-quality specimens are deeply colored but still translucent. Austrian specimens from the Knappenwand locality in the Hohe Tauern mountains are considered among the finest epidote crystals ever found.

Epidote is geologically important as a key indicator mineral in metamorphic petrology. Its presence tells geologists about the pressure, temperature, and chemistry of the metamorphic event that formed the rock. It's also the green component in unakite (epidote + pink feldspar + quartz).

Identification Guide

Epidote is identified by its distinctive pistachio-to-olive green color, monoclinic prismatic crystals with a characteristic elongated habit, and hardness of 6-7. The green is distinctly different from the greens of tourmaline, emerald, or jade.

Distinguish from green tourmaline (different crystal cross-section), actinolite (fibrous habit, different crystal system), and olivine (orthorhombic, different green tone). Epidote's one-sided elongation and specific pistachio green are diagnostic.

Spotting Fakes

Epidote is a collector mineral not commonly sold in the general crystal market, so faking isn't an issue. The main identification challenge is distinguishing it from other green metamorphic minerals in hand specimen. The distinctive pistachio color, prismatic habit, and hardness provide good diagnostics.

Some links in this post go to Amazon. Crystal Almanac earns a commission from qualifying purchases at no extra cost to you. Tools recommended here are ones we would use ourselves to run the tests described - the recommendation comes first, the link is downstream of it.

Cultural & Metaphysical Traditions

Presented as cultural traditions, not scientific evidence

The 'increase' etymology has been embraced by crystal practitioners who associate epidote with amplifying whatever energy is present - positive or negative. This makes it unusual in the crystal healing world: practitioners warn that epidote will increase negative patterns as readily as positive ones, making it a stone that requires self-awareness. It's associated with personal growth, truth-facing, and releasing patterns that no longer serve.

Metaphysical and “healing” associations are cultural traditions, not medical advice or scientific fact. Crystals are not a substitute for professional medical care.

Where It's Found

Austria - Knappenwand (Untersulzbachtal)

World-class crystal specimens, classic locality

Pakistan - Various

Fine transparent crystals

Peru - Various

Good quality dark green crystals

United States - Alaska, California

Good specimens from metamorphic terrain

Price Guide

Entry$3-10 small crystals
Mid-Range$15-80 quality specimens
Collector$100-1,000+ Austrian or large crystalline

Good to Know

💎

Scratch test: At hardness 6.5, Epidote resists scratching from a knife but can be scratched by quartz. Best for pendants and earrings rather than rings.

🌍

Global supply: Found in 4 notable locations worldwide, from Austria to United States.

⚖️

Heft test: Epidote has average mineral density (3.45). It feels about as heavy as you'd expect from a stone its size.

Care & Safety

What epidote can and cannot tolerate, based on its hardness (Mohs 6.5) and chemistry (Ca₂(Al,Fe)₃(SiO₄)(Si₂O₇)O(OH)).

Can Epidote go in water?

Not recommended. Epidote can react with water, absorb moisture, or degrade with wet contact. Clean it with a dry or barely damp cloth and dry it immediately.

Can Epidote go in salt water?

No. Epidote should stay away from water in general, and salt water is worse on every count: dissolved salt is corrosive while the stone is wet, and abrasive salt crystals are left behind in cracks and crevices as it dries. Epidote's iron content also makes rust staining likely if salt residue sits on the surface.

Sources & References

The mineralogical and gemological data on this page is drawn from and can be cross-checked against these external references.

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