Chlormanganokalite is a very rare potassium manganese chloride mineral typically found in volcanic fumaroles. It is highly hygroscopic and will rapidly deliquesce when exposed to ambient humidity, meaning it must be stored in a sealed, dry container to prevent dissolution.
Is this chlormanganokalite?
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 chlormanganokalite with a known reference. Chlormanganokalite sits at Mohs 2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Chlormanganokalite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Chlormanganokalite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellowish.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular to rhombohedral crystals, often massive or as efflorescent crusts.
Often confused with
Chlormanganokalite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chlormanganokalite
Minerals reported to co-occur with chlormanganokalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₄MnCl₆
- Mohs hardness
- 2.5
- Density
- 2.14 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Tabular to Rhombohedral Crystals, Often Massive or as Efflorescent Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarolic Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find chlormanganokalite
Classic worldwide localities
- Vesuvius (Italy)
- Mount Rasvumchorr (Russia)
Field-hunting tip
Look in fumarolic deposits country, the host setting where chlormanganokalite typically forms. If you start seeing halite, sylvite, hematite in float, you are in the right ground. Field specimens usually show a tabular to rhombohedral crystals, often massive or as efflorescent crusts habit, so train your eye for that shape before scanning the outcrop.




