Caracolite is a rare lead-sodium sulfate-chloride mineral typically found in the oxidation zones of Chilean mines. It often appears as small, pearly, tabular crystals or crusts coating other minerals in copper and lead-rich deposits.
Is this caracolite?
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 caracolite with a known reference. Caracolite 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. Caracolite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Caracolite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, massive, crusts.
Often confused with
Caracolite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside caracolite
Minerals reported to co-occur with caracolite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃Pb₂(SO₄)₃Cl
- Mohs hardness
- 3
- Density
- 5.38 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Massive, Crusts
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Lead-bearing Ore Deposits
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find caracolite
Classic worldwide localities
- Sierra Gorda, Chile
- Antofagasta, Chile
Field-hunting tip
Look in oxidized zones of lead-bearing ore deposits country — that is the host setting where caracolite typically forms. If you start seeing paratacamite, quartz, jarosite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, crusts habit, so train your eye for that shape before scanning the outcrop.





