Chlorocalcite is a rare potassium calcium chloride mineral that typically forms as a fumarolic deposit or efflorescence. It is highly hygroscopic and requires careful storage in a dry environment to prevent it from deliquescing or dissolving due to atmospheric moisture.
Is this chlorocalcite?
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 chlorocalcite with a known reference. Chlorocalcite 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. Chlorocalcite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Chlorocalcite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: crusts, efflorescent coatings, granular aggregates.
Often confused with
Chlorocalcite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside chlorocalcite
Minerals reported to co-occur with chlorocalcite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KCaCl₃
- Mohs hardness
- 2.5
- Density
- 2.19 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Crusts, Efflorescent Coatings, Granular Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Fumarole Deposits
- Typical price
- $20-100 per specimen depending on size
Where rockhounds find chlorocalcite
Classic worldwide localities
- Mount Vesuvius, Italy
- Solikamsk, Russia
- Katzenbuckel, Germany
Field-hunting tip
Look in fumarole deposits country — that is the host setting where chlorocalcite typically forms. If you start seeing sylvite, halite, hematite in float, you are in the right ground. Field specimens usually show a crusts, efflorescent coatings, granular aggregates habit, so train your eye for that shape before scanning the outcrop.



