Quick Facts

FormulaCa₂(Al,Mn³⁺,Fe³⁺)₃(SiO₄)(Si₂O₇)O(OH)
Crystal SystemMonoclinic
LusterVitreous
StreakRed
TransparencyTranslucent to Opaque
Specific Gravity3.45-3.52

Formation & Origin

Piemontite is the manganese-bearing variety of epidote, where manganese (Mn³⁺) substitutes for aluminum and iron in the crystal structure to produce a distinctive deep red to reddish-brown color. It forms during regional metamorphism of manganese-rich sedimentary rocks, particularly in the greenschist to amphibolite facies.

The mineral was first described from the Piedmont (Piemonte) region of northwestern Italy, giving it its name. It occurs as prismatic crystals or massive aggregates in schists and quartzites that originally contained manganese-rich sediments.

Piemontite is not particularly rare as a mineral, but gem-quality transparent material is extremely scarce. The deep red color is among the richest of any naturally occurring silicate mineral. In thin section under a microscope, piemontite shows pleochroism from red to yellow to purple, making it one of the most visually dramatic minerals in petrography.

Identification Guide

Piemontite is identified by its deep red to reddish-brown color, epidote-group crystal habit (prismatic, often striated), and red streak. Hardness 6.5 and monoclinic crystal system match the broader epidote group.

Distinguish from common epidote (pistachio green vs. red), garnet (isometric crystal system), and thulite (pink zoisite, different color and crystal system). Piemontite's red streak and prismatic habit within metamorphic rock are diagnostic.

Spotting Fakes

Piemontite is too obscure to be commonly faked. The main issue is misidentification with other red minerals in metamorphic rocks. The red streak, epidote-type crystal habit, and metamorphic rock context help confirm identity. Some sellers may label any red inclusion in quartz or feldspar as piemontite when it could be hematite or garnet.

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

Piemontite is relatively unknown in mainstream crystal healing but has a small following among mineral-informed practitioners. It's associated with vitality, passion, and the courage to follow unconventional paths. Its epidote-group membership connects it to themes of growth and enhancement. Some practitioners use it for strengthening physical endurance.

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

Italy - Piedmont (Piemonte)

Type locality, named after the region

Japan - Various

Fine crystal specimens

Pakistan - Balochistan

Good mineral specimens

United States - Arizona, California

Some occurrences in metamorphic rocks

Price Guide

Entry$10-30 rough specimens
Mid-Range$30-100 matrix specimens
Collector$100-500 fine crystal specimens

Good to Know

💎

Scratch test: At hardness 6.5, Piemontite 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 Italy to United States.

⚖️

Heft test: Piemontite has average mineral density (3.45-3.52). It feels about as heavy as you'd expect from a stone its size.

Care & Safety

What piemontite can and cannot tolerate, based on its hardness (Mohs 6.5) and chemistry (Ca₂(Al,Mn³⁺,Fe³⁺)₃(SiO₄)(Si₂O₇)O(OH)).

Can Piemontite go in water?

Yes. Piemontite is not water-soluble and durable enough (Mohs 6.5), so plain water is fine for rinsing and cleaning with mild soap. Avoid prolonged soaking, which serves no purpose, and dry the stone afterward.

Can Piemontite go in salt water?

Not recommended, even though piemontite itself is hard and not water-soluble. Salt is corrosive and mildly abrasive: it can dull a polished surface, attack metal settings, and crystallize inside small fractures as the stone dries. Piemontite's iron content also makes rust staining likely if salt residue sits on the surface. A brief dip will not destroy piemontite, but rinse it with fresh water afterward and dry it. For routine cleaning, plain water is the safer choice.

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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