Chlorapatite is a rare member of the apatite group characterized by a chlorine-dominant composition. It usually presents as hexagonal prisms or granular masses in metamorphosed limestones and certain igneous environments, and it is visually indistinguishable from other apatite species without chemical analysis.
Is this chlorapatite?
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 chlorapatite with a known reference. Chlorapatite sits at Mohs ~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: vitreous.
- 4Match the color rangeCompare against the expected color range: greenish yellow, pinkish white.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals, massive, granular.
Often confused with
Chlorapatite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chlorapatite
Minerals reported to co-occur with chlorapatite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₅(PO₄)₃Cl
- Mohs hardness
- ~5
- Density
- 3.17-3.18 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic crystals, massive, granular
- Cleavage
- Poor on {0001} and {1010}
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- Relatively much rarer than fluorapatite or hydroxylapatite, formed in F-deficient environments
Where rockhounds find chlorapatite
Classic worldwide localities
- Fairfax quarry, Centreville, Fairfax Co., and Bull Run quarry, Loudoun Co., Virginia, USA
- Stillwater complex, Montana, USA
- White Picacho district, Maricopa and Yavapai Cos., Arizona, USA
- Bob’s Lake, Frontenac Co., Quebec, Canada
- Bushveld complex, Transvaal, South Africa
- Angarf-Sud pegmatite, Tazenakht Plain, Morocco
Field-hunting tip
Where it forms: Relatively much rarer than fluorapatite or hydroxylapatite, formed in F-deficient environments. If you start seeing actinolite, diopside, calcite in float, you are in the right ground. Typical habit: prismatic crystals, massive, granular. Train your eye for that shape before scanning the outcrop.








