Kettnerite is a rare secondary bismuth mineral that typically occurs as small, delicate platy or tabular crystals in oxidized bismuth-bearing ore deposits. It is most frequently found as thin crusts or aggregates in association with other bismuth species and quartz, primarily in historical mining districts of Central Europe.
Is this kettnerite?
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 kettnerite with a known reference. Kettnerite 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. Kettnerite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kettnerite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-white, colorless.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: platy crystals, crusts, tabular.
Often confused with
Kettnerite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kettnerite
Minerals reported to co-occur with kettnerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaBi(CO₃)OF
- Mohs hardness
- 3
- Density
- 4.56 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Tetragonal
- Crystal habit
- Platy Crystals, Crusts, Tabular
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Bismuth-bearing Veins
- Typical price
- $50-300 per specimen
Where rockhounds find kettnerite
Classic worldwide localities
- Schneeberg, Saxony, Germany
- Wittichen, Black Forest, Germany
- Jáchymov, Czech Republic
Field-hunting tip
Look in hydrothermal bismuth-bearing veins country — that is the host setting where kettnerite typically forms. If you start seeing bismutite, bismuth, fluorite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, tabular habit, so train your eye for that shape before scanning the outcrop.




