Chladniite is an exceptionally rare phosphate mineral discovered primarily in pallasite meteorites. It typically occurs as tiny, transparent tabular crystals associated with olivine and metallic iron-nickel phases.
Is this chladniite?
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 chladniite with a known reference. Chladniite sits at Mohs 4.5-5, 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 to resinous.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: trigonal. Typical habit: granular, selvage.
Often confused with
Chladniite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chladniite
Minerals reported to co-occur with chladniite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₃CaMg₁₁(PO₄)₉
- Mohs hardness
- 4.5-5
- Density
- 3.01 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous to resinous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Granular, selvage
- Cleavage
- Rhombohedral, probable
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As a single grain in a phosphate-rich inclusion in an iron meteorite (Carleton meteorite); in phosphate-rich portions of an acapulcoite-lodranite meteorite
Where rockhounds find chladniite
Classic worldwide localities
- Carleton type IIICD iron and GRA 95209 primitive achrondite meteorites (type locality)
Field-hunting tip
Where it forms: As a single grain in a phosphate-rich inclusion in an iron meteorite (Carleton meteorite); in phosphate-rich portions of an acapulcoite-lodranite meteorite. If you start seeing chlorapatite, olivine, pyroxene in float, you are in the right ground. Typical habit: granular, selvage. Train your eye for that shape before scanning the outcrop.








