Cannonite is a rare bismuth sulfate mineral that typically occurs as small, transparent tabular crystals in oxidized mineral deposits. It is most famous from the Tintic district in Utah where it forms as a secondary mineral in mine dumps. Collectors prize it for its rarity and its distinct association with other secondary bismuth minerals.
Is this cannonite?
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 cannonite with a known reference. Cannonite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cannonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Cannonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals.
Often confused with
Cannonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside cannonite
Minerals reported to co-occur with cannonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Bi₂O(OH)₂SO₄
- Mohs hardness
- 2-3
- Density
- 5.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Veins
- Typical price
- $50-300 per thumbnail specimen
Where rockhounds find cannonite
Classic worldwide localities
- Tunnel Extension mine, Utah, USA
- Tintic district, Utah, USA
- Gold Hill, Utah, USA
Field-hunting tip
Look in oxidized hydrothermal veins country — that is the host setting where cannonite typically forms. If you start seeing bismutite, quartz, pyrite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.




