Smamite is an extremely rare antimonate mineral typically found as small, colorless to white tabular crystals. It is primarily known from the historic Långban mine in Sweden, occurring within metamorphosed manganese-rich skarns.
Is this smamite?
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 smamite with a known reference. Smamite sits at Mohs ~3.5, 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: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals.
Often confused with
Smamite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Stibiconite is the harder of the two (Mohs 5.5-7 vs. ~3.5); streak differs, so Smamite leaves white, Stibiconite leaves light yellow; luster reads vitreous on Smamite and pearly, opaline, glassy to earthy on Stibiconite.
Often found alongside smamite
Minerals reported to co-occur with smamite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Sb(OH)₄[H(AsO₄)₂](H₂O)₆
- Mohs hardness
- ~3.5
- Density
- 2.72 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A supergene mineral from the oxidative weathering of primary As-mineralization [native arsenic, tennantite-tetrahedrite (fahlore), arsenides of Co and Ni, löllingite and chalcopyrite]
Where rockhounds find smamite
Classic worldwide localities
- Giftgrube mine, Rauenthal, Sainte-Marie-Aux-Mines district, Haut-Rhin department, Grand Est, France
Field-hunting tip
Where it forms: A supergene mineral from the oxidative weathering of primary As-mineralization [native arsenic, tennantite-tetrahedrite (fahlore), arsenides of Co and Ni, löllingite and chalcopyrite]. If you start seeing picropharmacolite, fluckite, pharmacolite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.





