Ferroalluaudite is a relatively rare phosphate mineral typically occurring as a secondary alteration product in phosphate-rich granite pegmatites. It is best identified by its distinct yellowish-brown to greenish hues and its association with other phosphate minerals in hydrothermal veins or weathered zones.

Hardness
5
Mohs
Luster
Vitreous
Streak
Light yellow
Transparency
Semitransparent

Is this ferroalluaudite?

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 ferroalluaudite with a known reference. Ferroalluaudite sits at Mohs 5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: light yellow.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: blue green.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: massive.

Often confused with

Ferroalluaudite vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside ferroalluaudite

Minerals reported to co-occur with ferroalluaudite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
Na(Fe³⁺,Fe²⁺)₂(PO₄)₂
Mohs hardness
5
Density
3.67 g/cm³
Streak
Light yellow
Luster
Vitreous
Transparency
Semitransparent
Crystal system
Monoclinic
Crystal habit
Massive
Cleavage
Good in one direction
Rarity
Rare
Uses
Collector, Scientific research
Host rock
From zoned granite pegmatites; in phosphatic nodules

Where rockhounds find ferroalluaudite

Classic worldwide localities

  • Pleasant Valley pegmatite and the Helen Beryl mine, near Custer, Custer Co., South Dakota, USA
  • Rapid Creek, Yukon Territory, Canada
  • Angarf-Sud pegmatite, Tazenakht Plain, Anti-Atlas Mountains, Morocco
  • Norrö pegmatite, on Rånö Island, Sweden
  • Kiluli, Rwanda

Field-hunting tip

Where it forms: From zoned granite pegmatites; in phosphatic nodules. If you start seeing triphylite, barbosalite, ferrisicklerite in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify ferroalluaudite?+
Mohs hardness is 5. Luster: vitreous. The streak is light yellow. Common colors include blue green.
Where is ferroalluaudite found?+
Notable localities include Pleasant Valley pegmatite and the Helen Beryl mine, near Custer, Custer Co., South Dakota, USA; Rapid Creek, Yukon Territory, Canada; Angarf-Sud pegmatite, Tazenakht Plain, Anti-Atlas Mountains, Morocco; Norrö pegmatite, on Rånö Island, Sweden; Kiluli, Rwanda.
What rocks look like ferroalluaudite?+
Ferroalluaudite is most often confused with Alluaudite, Hagendorfite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with ferroalluaudite?+
Ferroalluaudite commonly co-occurs with Triphylite, Barbosalite, Ferrisicklerite, Apatite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does ferroalluaudite form in?+
Where it forms: From zoned granite pegmatites; in phosphatic nodules. Working float back to the host body is the standard way to chase a fresh occurrence.
What is ferroalluaudite used for?+
Ferroalluaudite is used in collector, scientific research.

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