Metavandendriesscheite is a rare secondary uranium mineral formed through the alteration of uraninite. Collectors should look for thin, platy yellow crystals often found as crusts or tiny radial sprays in the oxidation zones of uranium deposits.
Is this metavandendriesscheite?
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 metavandendriesscheite with a known reference. Metavandendriesscheite sits at Mohs 3, 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: adamantine.
- 4Match the color rangeCompare against the expected color range: orange, amber.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic.
Often confused with
Metavandendriesscheite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside metavandendriesscheite
Minerals reported to co-occur with metavandendriesscheite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbU₇O₂₂·nH₂O
- Mohs hardness
- 3
- Density
- 5.45 g/cm³
- Streak
- Yellow
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxidized zone of a uranium-bearing mineral deposit
Where rockhounds find metavandendriesscheite
Classic worldwide localities
- Shinkolobwe, Katanga Province, Congo (Shaba Province, Zaire)
Field-hunting tip
Where it forms: In the oxidized zone of a uranium-bearing mineral deposit. If you start seeing vandendriesscheite, fourmarierite, becquerelite in float, you are in the right ground. Typical habit: prismatic. Train your eye for that shape before scanning the outcrop.






