Natrouranospinite is a rare uranyl arsenate mineral characterized by its distinctive yellow-green color and platy, micaceous habit. It is found in the oxidized zones of uranium-bearing hydrothermal veins and is highly prized by collectors for its strong fluorescence under ultraviolet light.
Is this natrouranospinite?
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 natrouranospinite with a known reference. Natrouranospinite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Natrouranospinite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Natrouranospinite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-green.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: platy crystals, micaceous aggregates.
Often confused with
Natrouranospinite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside natrouranospinite
Minerals reported to co-occur with natrouranospinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na₂,Ca)(UO₂)₂(AsO₄)₂·5H₂O
- Mohs hardness
- 2-3
- Density
- 3.32 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Tetragonal
- Crystal habit
- Platy Crystals, Micaceous Aggregates
- Cleavage
- Perfect Basal
- Fluorescence
- Bright Green Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Uranium Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find natrouranospinite
Classic worldwide localities
- Schwarzwald, Germany
- Jachymov, Czech Republic
- Dalnegorsk, Russia
Field-hunting tip
Look in hydrothermal uranium deposits country — that is the host setting where natrouranospinite typically forms. If you start seeing uraninite, gummite, quartz in float, you are in the right ground. Field specimens usually show a platy crystals, micaceous aggregates habit, so train your eye for that shape before scanning the outcrop.




