Mopungite is a rare secondary mineral typically occurring in the oxidized zones of antimony deposits. It is best identified by its colorless to white tetragonal bipyramidal crystals, usually found associated with other antimony oxidation products like stibiconite.
Is this mopungite?
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 mopungite with a known reference. Mopungite 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: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, milky white.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: encrustations, pseudo cubic, pseudomorphous.
Often confused with
Mopungite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside mopungite
Minerals reported to co-occur with mopungite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaSb(OH)₆
- Mohs hardness
- 3
- Density
- 3.21 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Tetragonal
- Crystal habit
- Encrustations, pseudo cubic, pseudomorphous
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An oxidation product of stibnite
Where rockhounds find mopungite
Classic worldwide localities
- Green prospect, Mopung Hills, Lake district, Churchill Co., Nevada, USA
- Cetine mine, 20 km southwest of Siena, Tuscany, Italy
Field-hunting tip
Where it forms: An oxidation product of stibnite. If you start seeing selenium, sulfur, stibiconite in float, you are in the right ground. Typical habit: encrustations, pseudo cubic, pseudomorphous. Train your eye for that shape before scanning the outcrop.





