Challacolloite is a very rare potassium lead chloride mineral discovered at its namesake locality in the Challacollo mine of Chile. It typically forms as thin crusts or coatings in volcanic fumarole environments and is often associated with other halide minerals. Due to its extreme rarity and tendency to form small, fragile aggregates, it is primarily sought after by advanced systematic mineral collectors.
Is this challacolloite?
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 challacolloite with a known reference. Challacolloite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Challacolloite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Challacolloite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: cubic. Typical habit: crusts, aggregates of minute crystals.
Often confused with
Challacolloite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside challacolloite
Minerals reported to co-occur with challacolloite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KPb₂Cl₅
- Mohs hardness
- 2
- Density
- 2.83 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Crusts, Aggregates of Minute Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Fumarolic Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find challacolloite
Classic worldwide localities
- Challacollo mine, Chile
Field-hunting tip
Look in fumarolic deposits country — that is the host setting where challacolloite typically forms. If you start seeing cotunnite, halite, sylvite in float, you are in the right ground. Field specimens usually show a crusts, aggregates of minute crystals habit, so train your eye for that shape before scanning the outcrop.



