Natrowalentaite is a rare phosphate mineral typically occurring as thin, tabular, yellowish crystals within pegmatite pockets. It is primarily found as a secondary mineral resulting from the alteration of primary phosphate minerals. Collectors prize it for its vibrant color and delicate, localized crystal growth patterns.
Is this natrowalentaite?
4-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 natrowalentaite with a known reference. Natrowalentaite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: bright greenish yellow.
- 4Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, subparallel aggregates.
Often confused with
Natrowalentaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside natrowalentaite
Minerals reported to co-occur with natrowalentaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- [Fe₀.₅Na₀.₅(H₂O)₆][NaAs₂(Fe₂.₃₃W₀.₆₇)(PO₄)₂O₇]
- Mohs hardness
- 2-3
- Density
- 2.91 g/cm³
- Colors
- Bright greenish yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular crystals, subparallel aggregates
- Cleavage
- Perfect on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- On fracture surfaces in iron-stained heavily weathered rock as a product of supergene alteration of primary sulfide and arsenide minerals
Where rockhounds find natrowalentaite
Classic worldwide localities
- Griffins Find gold deposit, ~15 km northwest of Lake Grace and 275 km southeast of Perth, Western Australia
Field-hunting tip
Where it forms: On fracture surfaces in iron-stained heavily weathered rock as a product of supergene alteration of primary sulfide and arsenide minerals. If you start seeing natropharmacosiderite, jarosite in float, you are in the right ground. Typical habit: tabular crystals, subparallel aggregates. Train your eye for that shape before scanning the outcrop.




