Iranite is a rare lead copper chromate silicate mineral known primarily from its type locality in Iran. It typically forms attractive orange-to-yellow tabular crystal aggregates in the oxidized zones of base metal deposits.
Is this iranite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch iranite with a known reference. Iranite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Iranite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Iranite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: orange, yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, crusts.
Often confused with
Iranite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Streak differs — Iranite leaves yellow, Phoenicochroite leaves orange-yellow; luster reads vitreous on Iranite and adamantine on Phoenicochroite.

How to tell apart: Streak differs — Iranite leaves yellow, Wulfenite leaves white; luster reads vitreous on Iranite and resinous on Wulfenite.
Often found alongside iranite
Minerals reported to co-occur with iranite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₁₀Cu(CrO₄)₆(SiO₄)₂(OH)₂
- Mohs hardness
- 3.5
- Density
- 5.68 g/cm³
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Lead-copper Hydrothermal Deposits
- Typical price
- $50-500 thumbnail, $300-2000 cabinet
Where rockhounds find iranite
Classic worldwide localities
- Seh-Changi mine, Iran
- Kavner, Iran
Field-hunting tip
Look in oxidized lead-copper hydrothermal deposits country — that is the host setting where iranite typically forms. If you start seeing phoenicochroite, wulfenite, cerussite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts habit, so train your eye for that shape before scanning the outcrop.


