Joesmithite is an extremely rare lead-bearing silicate mineral characterized by its complex chemical structure involving beryllium. It is primarily found in the metamorphosed iron-manganese deposits of Långban, Sweden, often appearing as dark, inconspicuous grains within a mineralized matrix. Collectors prize it as a rare mineralogical oddity rather than for its aesthetic qualities.
Is this joesmithite?
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 joesmithite with a known reference. Joesmithite sits at Mohs 4-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Joesmithite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Joesmithite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark brown, brownish black, reddish brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular, massive, anhedral to subhedral crystals.
Often found alongside joesmithite
Minerals reported to co-occur with joesmithite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb(CaPb)Fe²⁺₂Be₂Si₂O₈(OH)₂
- Mohs hardness
- 4-5
- Density
- 3.84 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Granular, Massive, Anhedral to Subhedral Crystals
- Cleavage
- Good in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Iron-manganese Ore Deposits
- Typical price
- $100-500+ depending on matrix quality
Where rockhounds find joesmithite
Classic worldwide localities
- Långban, Filipstad, Värmland, Sweden
Field-hunting tip
Look in metamorphosed iron-manganese ore deposits country — that is the host setting where joesmithite typically forms. If you start seeing magnetite, jacobsite, hedyphane in float, you are in the right ground. Field specimens usually show a granular, massive, anhedral to subhedral crystals habit, so train your eye for that shape before scanning the outcrop.





