Mendipite is a rare lead oxychloride mineral that typically forms as pearly or adamantine prismatic crystals within oxidized ore zones. It is most famous from the type locality in the Mendip Hills of England where it occurs as distinctively fibrous or elongated white to pale yellow masses.
Is this mendipite?
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 mendipite with a known reference. Mendipite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Mendipite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Mendipite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: white, yellow, light yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, massive, fibrous.
Often confused with
Mendipite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside mendipite
Minerals reported to co-occur with mendipite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₃Cl₂O₂
- Mohs hardness
- 2.5
- Density
- 7.0-7.5 g/cm³
- Colors
- Streak
- White
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic Crystals, Massive, Fibrous
- Cleavage
- Perfect On {110}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Lead-manganese Ore Deposits in Limestone
- Typical price
- $50-500 thumbnail to miniature
Where rockhounds find mendipite
Classic worldwide localities
- Mendip Hills, Somerset, England
- Langban, Sweden
- Brilon, Germany
Field-hunting tip
Look in oxidized lead-manganese ore deposits in limestone country — that is the host setting where mendipite typically forms. If you start seeing cerussite, hydrocerussite, pyrolusite in float, you are in the right ground. Field specimens usually show a prismatic crystals, massive, fibrous habit, so train your eye for that shape before scanning the outcrop.





