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 — that is 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.





