Whiteite-(CaFeMg) is a complex phosphate mineral typically found as small, distinct yellow-to-brown tabular crystals. It is highly prized by collectors of rare phosphate species, often occurring in association with other secondary phosphates in hydrothermal vein environments.
Is this whiteite-(cafemg)?
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 whiteite-(cafemg) with a known reference. Whiteite-(CaFeMg) sits at Mohs 3-4, 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 dull.
- 4Match the color rangeCompare against the expected color range: yellow, yellow brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: aggregates, tabular.
Often confused with
Whiteite-(CaFeMg) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside whiteite-(cafemg)
Minerals reported to co-occur with whiteite-(cafemg). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaFe²⁺Mg₂Al₂(PO₄)₄(OH)₂·8H₂O
- Mohs hardness
- 3-4
- Density
- 2.58 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous to dull
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Aggregates, tabular
- Cleavage
- On {001}, good to perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a complex zoned granite pegmatite (Lavra da Ilha pegmatite, Brazil); in an iron-formation (Blow River, Canada)
Where rockhounds find whiteite-(cafemg)
Classic worldwide localities
- Lavra da Ilha pegmatite, in the Jequitinhonha River, three km north of Taquaral, and at the Énio pegmatite mine, northeast of Galiléia, Minas Gerais, Brazil
- Blow River area, Yukon Territory, Canada
Field-hunting tip
Where it forms: In a complex zoned granite pegmatite (Lavra da Ilha pegmatite, Brazil); in an iron-formation (Blow River, Canada). If you start seeing eosphorite, zanazziite, wardite in float, you are in the right ground. Typical habit: aggregates, tabular. Train your eye for that shape before scanning the outcrop.








