Metanatroautunite is a rare secondary uranium mineral formed by the dehydration of natroautunite. It typically appears as bright yellow or yellow-green platy crusts and is highly sought after by collectors for its brilliant yellow-green fluorescence under ultraviolet light.
Is this metanatroautunite?
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 metanatroautunite with a known reference. Metanatroautunite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, pearly on {001}.
- 4Match the color rangeCompare against the expected color range: lemon-yellow, lettuce-yellow, greenish yellow.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: platy crystals, micaceous aggregates, crusts.
Often confused with
Metanatroautunite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Metanatroautunite leaves yellow, Autunite leaves pale yellow.

How to tell apart: Streak differs, so Metanatroautunite leaves yellow, Torbernite leaves pale green.

How to tell apart: Luster reads vitreous, pearly on {001} on Metanatroautunite and pearly to dull on Meta-autunite.
Often found alongside metanatroautunite
Minerals reported to co-occur with metanatroautunite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂(UO₂)₂(PO₄)₂·6H₂O
- Mohs hardness
- 2-2.5
- Density
- 3.62 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous, pearly on {001}
- Transparency
- Semitransparent
- Crystal system
- Tetragonal
- Crystal habit
- Platy crystals, micaceous aggregates, crusts
- Cleavage
- {001}, perfect; {100}, less perfect
- Fluorescence
- Yellow-green fluorescence under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxidized zone of a uranium deposit in a granodiorite massif (Tajikistan)
Where rockhounds find metanatroautunite
Classic worldwide localities
- Found in the Kuruk uranium deposit, 15 km northeast of Khodzhent, Samgar Steppe, northern Tajikistan
- Lake Boga Granite, Victoria, Australia
Field-hunting tip
Where it forms: In the oxidized zone of a uranium deposit in a granodiorite massif (Tajikistan). If you start seeing schoepite, gypsum, kaolinite in float, you are in the right ground. Typical habit: platy crystals, micaceous aggregates, crusts. Train your eye for that shape before scanning the outcrop.




