Matulaite is a rare phosphate mineral that typically forms as botryoidal or crust-like coatings in phosphate-rich localities. It is frequently associated with other secondary phosphate minerals like variscite and wavellite, often requiring magnification for accurate identification due to its small size.
Is this matulaite?
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 matulaite with a known reference. Matulaite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Matulaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Matulaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: botryoidal, crusts, radial aggregates.
Often confused with
Matulaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside matulaite
Minerals reported to co-occur with matulaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaAl₇(PO₄)₄(OH)₁₃·18H₂O
- Mohs hardness
- 2.5-3
- Density
- 2.44 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Botryoidal, Crusts, Radial Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Phosphate Deposits in Hydrothermal or Weathering Environments
- Typical price
- $20-150 for micromounts or small specimens
Where rockhounds find matulaite
Classic worldwide localities
- Herd Mountain, Alabama, USA
- Hellertown, Pennsylvania, USA
Field-hunting tip
Look in phosphate deposits in hydrothermal or weathering environments country — that is the host setting where matulaite typically forms. If you start seeing variscite, wavellite, crandallite in float, you are in the right ground. Field specimens usually show a botryoidal, crusts, radial aggregates habit, so train your eye for that shape before scanning the outcrop.




