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.

Hardness
3-4
Mohs
Luster
Vitreous to dull
Streak
White
Transparency
Semitransparent

Is this whiteite-(cafemg)?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try 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.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous to dull.
  • 4
    Match the color range
    Compare against the expected color range: yellow, yellow brown.
  • 5
    Look at form & habit
    Crystal 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
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.

Common questions

How do you identify whiteite-(cafemg)?+
Mohs hardness is 3-4. Luster: vitreous to dull. The streak is white. Common colors include yellow, yellow brown.
Where is whiteite-(cafemg) found?+
Notable localities include 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.
What rocks look like whiteite-(cafemg)?+
Whiteite-(CaFeMg) is most often confused with Laueite, Stewartite, Wardite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with whiteite-(cafemg)?+
Whiteite-(CaFeMg) commonly co-occurs with Eosphorite, Zanazziite, Wardite, Albite, Quartz, Siderite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does whiteite-(cafemg) form in?+
Where it forms: In a complex zoned granite pegmatite (Lavra da Ilha pegmatite, Brazil); in an iron-formation (Blow River, Canada). Working float back to the host body is the standard way to chase a fresh occurrence.
What is whiteite-(cafemg) used for?+
Whiteite-(CaFeMg) is used in collector.

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