Kladnoite is an extremely rare organic mineral found as sublimation crusts in burning coal mine waste piles. It is highly unstable and water-soluble, requiring careful preservation away from humidity. Collectors prize it for its unique chemical origin as a naturally occurring organic phthalimide derivative.
Is this kladnoite?
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 kladnoite with a known reference. Kladnoite sits at Mohs 1.5, 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: dull.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: sublimation crusts, fine crystalline aggregates.
Often found alongside kladnoite
Minerals reported to co-occur with kladnoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- C₆H₄(CO)₂NH
- Mohs hardness
- 1.5
- Density
- 1.47 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Sublimation crusts, fine crystalline aggregates
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Formed as a result of fires in coal heaps
Where rockhounds find kladnoite
Classic worldwide localities
- Scholler coal mine, Libušín, Kladno coal basin, about 30 km west-northwest of Prague, and at Radvanice, Czech Republic
Field-hunting tip
Where it forms: Formed as a result of fires in coal heaps. If you start seeing sal-ammoniac, sulfur, boussingaultite in float, you are in the right ground. Typical habit: sublimation crusts, fine crystalline aggregates. Train your eye for that shape before scanning the outcrop.


