Phoenicochroite is a rare lead chromate mineral that typically forms as bright, deep red tabular crystals or crusts. It is most famous from the Berezovskoe deposit in Russia and is highly sought after by advanced collectors for its intense color and rarity.
Is this phoenicochroite?
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 phoenicochroite with a known reference. Phoenicochroite sits at Mohs 3-3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Phoenicochroite leaves a orange-yellow streak.
- 3Read the lusterHold the specimen under a strong light. Phoenicochroite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: cochineal-red, hyacinth-red, dark red.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, massive, or crusts.
Often confused with
Phoenicochroite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside phoenicochroite
Minerals reported to co-occur with phoenicochroite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₃(CrO₄)₂O
- Mohs hardness
- 3-3.5
- Density
- 5.7-5.8 g/cm³
- Streak
- Orange-yellow
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Massive, Or Crusts
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Lead-chromium Ore Deposits
- Typical price
- $50-500 thumbnail
Where rockhounds find phoenicochroite
Classic worldwide localities
- Berezovskoe, Ural Mountains, Russia
- Mina Esperanza, Chile
- Touissit, Morocco
Field-hunting tip
Look in oxidized zones of lead-chromium ore deposits country — that is the host setting where phoenicochroite typically forms. If you start seeing crocoite, vauquelinite, quartz in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, or crusts habit, so train your eye for that shape before scanning the outcrop.




