Metaschoepite is a secondary uranium mineral that forms through the dehydration of schoepite. It is typically found as small, bright yellow, platy crystals in the oxidation zones of uranium-rich ore bodies.
Is this metaschoepite?
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 metaschoepite with a known reference. Metaschoepite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Metaschoepite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Metaschoepite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, platy aggregates, crusts.
Often confused with
Metaschoepite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside metaschoepite
Minerals reported to co-occur with metaschoepite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- UO₃·2H₂O
- Mohs hardness
- 2.5
- Density
- 4.8 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Platy Aggregates, Crusts
- Cleavage
- Perfect
- Fluorescence
- Bright Yellow-green Under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Uranium-bearing Hydrothermal Deposits
- Typical price
- $50-300 per thumbnail specimen
Where rockhounds find metaschoepite
Classic worldwide localities
- Shinkolobwe Mine, DR Congo
- Johanngeorgenstadt, Germany
- Great Bear Lake, Canada
Field-hunting tip
Look in oxidized zones of uranium-bearing hydrothermal deposits country — that is the host setting where metaschoepite typically forms. If you start seeing uraninite, soddyite, becquerelite in float, you are in the right ground. Field specimens usually show a tabular crystals, platy aggregates, crusts habit, so train your eye for that shape before scanning the outcrop.






