Paganoite is an extremely rare nickel bismuth arsenate mineral found in hydrothermal environments. It typically forms as small, distinctive yellow to brownish tabular crystals and is known primarily from the type locality in Germany.
Is this paganoite?
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 paganoite with a known reference. Paganoite sits at Mohs 1-2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale orange-brown.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: orange, golden brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: aggregates, euhedral crystals.
Often found alongside paganoite
Minerals reported to co-occur with paganoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NiBi(AsO₄)O
- Mohs hardness
- 1-2
- Density
- 6.715 g/cm³
- Colors
- Streak
- Pale orange-brown
- Luster
- Adamantine
- Transparency
- Transparent to translucent
- Crystal system
- Triclinic
- Crystal habit
- Aggregates, euhedral crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Formed from the breakdown of primary nickeline and native bismuth
Where rockhounds find paganoite
Classic worldwide localities
- Johanngeorgenstadt, Saxony, Germany
Field-hunting tip
Where it forms: Formed from the breakdown of primary nickeline and native bismuth. If you start seeing aerugite, xanthiosite, rooseveltite in float, you are in the right ground. Typical habit: aggregates, euhedral crystals. Train your eye for that shape before scanning the outcrop.






