Fillowite is a rare phosphate mineral typically found as granular or massive aggregates in complex granite pegmatites. It is often identified by its yellowish-brown color and vitreous luster, frequently occurring alongside other rare phosphate minerals in pockets. Collectors prize it as a significant, though obscure, member of the phosphate-rich zones in pegmatites.

Hardness
4.5
Mohs
Luster
Subresinous to greasy
Streak
White
Transparency
Transparent to translucent

Is this fillowite?

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 fillowite with a known reference. Fillowite sits at Mohs 4.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: subresinous to greasy.
  • 4
    Match the color range
    Compare against the expected color range: yellow, reddish brown, colorless.
  • 5
    Look at form & habit
    Crystal system: trigonal. Typical habit: euhedral crystals, granular.

Often confused with

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

Often found alongside fillowite

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

All properties

Chemical formula
Na₃CaMn₁₁(PO₄)₉
Mohs hardness
4.5
Density
3.43 g/cm³
Streak
White
Luster
Subresinous to greasy
Transparency
Transparent to translucent
Crystal system
Trigonal
Crystal habit
Euhedral crystals, granular
Cleavage
{0001}, nearly perfect
Rarity
Rare
Uses
Collector
Host rock
A primary accessory mineral in a zoned granite pegmatite (Branchville, Connecticut, USA)

Where rockhounds find fillowite

Classic worldwide localities

  • Branchville, Fairfield Co., Connecticut, USA
  • White Picacho district, Maricopa and Yavapai Cos., Arizona, USA
  • Animike Red Ace pegmatite, Florence Co., Wisconsin, USA
  • Buranga, Kiluli, and Rusororo, Rwanda
  • Kabira, Uganda

Field-hunting tip

Where it forms: A primary accessory mineral in a zoned granite pegmatite (Branchville, Connecticut, USA). If you start seeing triploidite, fairfieldite, reddingite in float, you are in the right ground. Typical habit: euhedral crystals, granular. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify fillowite?+
Mohs hardness is 4.5. Luster: subresinous to greasy. The streak is white. Common colors include yellow, reddish brown, colorless.
Where is fillowite found?+
Notable localities include Branchville, Fairfield Co., Connecticut, USA; White Picacho district, Maricopa and Yavapai Cos., Arizona, USA; Animike Red Ace pegmatite, Florence Co., Wisconsin, USA; Buranga, Kiluli, and Rusororo, Rwanda; Kabira, Uganda.
What rocks look like fillowite?+
Fillowite is most often confused with Triplite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with fillowite?+
Fillowite commonly co-occurs with Triploidite, Fairfieldite, Reddingite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does fillowite form in?+
Where it forms: A primary accessory mineral in a zoned granite pegmatite (Branchville, Connecticut, USA). Working float back to the host body is the standard way to chase a fresh occurrence.
What is fillowite used for?+
Fillowite is used in collector.

Find fillowite on the map

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