Somersetite is an extremely rare lead carbonate mineral first discovered in the Mendip Hills of England. It typically forms as small, colorless to white tabular crystals in cavities of oxidized lead-bearing ores. Collectors value it highly due to its rarity and specific type locality association.
Is this somersetite?
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 somersetite with a known reference. Somersetite sits at Mohs ~3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: white, green.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: tabular crystals.
Often confused with
Somersetite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside somersetite
Minerals reported to co-occur with somersetite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₈O(OH)₄(CO₃)₅
- Mohs hardness
- ~3
- Density
- 7.01 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Tabular crystals
- Cleavage
- Perfect on {0001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In hydrothermal veins of remobilized components derived from older veins containing galena, fluorite, calcite and baryte, hosted by limestone
Where rockhounds find somersetite
Classic worldwide localities
- Torr Works quarry (‘Merehead quarry’), near Cranmore, Mendip Hills, Somerset, England
Field-hunting tip
Where it forms: In hydrothermal veins of remobilized components derived from older veins containing galena, fluorite, calcite and baryte, hosted by limestone. If you start seeing plumbonacrite, cerussite, symesite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.





