Pauladamsite is a rare lead-copper selenite mineral that occurs as delicate, pale green platy crystals. It is primarily found within the oxidized zones of selenium-rich deposits, typically associated with other secondary minerals like anglesite and cerussite.
Is this pauladamsite?
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 pauladamsite with a known reference. Pauladamsite sits at Mohs ~2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to silky.
- 4Match the color rangeCompare against the expected color range: green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals.
Often confused with
Pauladamsite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pauladamsite
Minerals reported to co-occur with pauladamsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₄(SeO₃)(SO₄)(OH)₄(H₂O)₂
- Mohs hardness
- ~2
- Density
- 3.535 g/cm³
- Colors
- Streak
- Pale green
- Luster
- Vitreous to silky
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Platy crystals
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxidation-zone of a polymetallic hydrothermal sulfide deposit
Where rockhounds find pauladamsite
Classic worldwide localities
- Santa Rosa mine, Darwin district, Inyo County, California, USA
Field-hunting tip
Where it forms: In the oxidation-zone of a polymetallic hydrothermal sulfide deposit. If you start seeing brochantite, chalcanthite, gypsum in float, you are in the right ground. Typical habit: platy crystals. Train your eye for that shape before scanning the outcrop.







