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. Chlorapatite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Chlorapatite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale green, pale blue.
- 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
- 3.17-3.23 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic Crystals, Massive, Granular
- Cleavage
- Poor Basal
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphic Limestones, Skarns, Alkaline Igneous Rocks
- Typical price
- $20-100 for small crystals
Where rockhounds find chlorapatite
Classic worldwide localities
- Kola Peninsula, Russia
- Pargas, Finland
- Bamle, Norway
- Grenville Province, Canada
Field-hunting tip
Look in metamorphic limestones, skarns, alkaline igneous rocks country — that is the host setting where chlorapatite typically forms. If you start seeing calcite, diopside, phlogopite in float, you are in the right ground. Field specimens usually show a prismatic crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.






