Metatyuyamunite is a secondary uranium mineral formed by the dehydration of tyuyamunite in arid environments. It is characterized by its bright yellow to yellow-green color and intense fluorescence under UV light, typically appearing as delicate crusts or microscopic plates.
Is this metatyuyamunite?
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 metatyuyamunite with a known reference. Metatyuyamunite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Metatyuyamunite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Metatyuyamunite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals, crusts, or pulverulent masses.
Often confused with
Metatyuyamunite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside metatyuyamunite
Minerals reported to co-occur with metatyuyamunite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca(UO₂)₂(VO₄)₂·(5-8)H₂O
- Mohs hardness
- 2
- Density
- 3.8-4.0 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals, Crusts, Or Pulverulent Masses
- Cleavage
- Perfect Basal
- Fluorescence
- Bright Yellow-green Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sedimentary Uranium-vanadium Deposits in Sandstone
- Typical price
- $20-200 per specimen depending on size and intensity of fluorescence
Where rockhounds find metatyuyamunite
Classic worldwide localities
- Tyuya-Muyun, Kyrgyzstan
- Colorado Plateau, USA
- Utah, USA
- New Mexico, USA
Field-hunting tip
Look in sedimentary uranium-vanadium deposits in sandstone country, the host setting where metatyuyamunite typically forms. If you start seeing tyuyamunite, carnotite, vanadinite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, or pulverulent masses habit, so train your eye for that shape before scanning the outcrop.





