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, 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.




