Metatorbernite is a dehydration product of torbernite, characterized by its vibrant emerald-green, tabular crystals. Collectors should look for distinct square, micaceous plates typically found in the weathered zones of uranium deposits.
Is this metatorbernite?
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 metatorbernite with a known reference. Metatorbernite 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. Streak: light green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, subadamantine, pearly on {001}.
- 4Match the color rangeCompare against the expected color range: light green, dark green.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: tabular crystals, micaceous aggregates, crusts.
Often confused with
Metatorbernite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Metatorbernite leaves light green, Torbernite leaves pale green.

How to tell apart: Streak differs, so Metatorbernite leaves light green, Autunite leaves pale yellow.

How to tell apart: Streak differs, so Metatorbernite leaves light green, Meta-autunite leaves yellow; luster reads vitreous, subadamantine, pearly on {001} on Metatorbernite and pearly to dull on Meta-autunite.
Often found alongside metatorbernite
Minerals reported to co-occur with metatorbernite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu(UO₂)₂(PO₄)₂·8H₂O
- Mohs hardness
- 2.5
- Density
- 3.52-3.70 g/cm³
- Colors
- Streak
- Light green
- Luster
- Vitreous, subadamantine, pearly on {001}
- Transparency
- Transparent to translucent
- Crystal system
- Tetragonal
- Crystal habit
- Tabular crystals, micaceous aggregates, crusts
- Cleavage
- Perfect on {001}; indistinct on {010}
- Rarity
- Uncommon
- Uses
- Collector, Reference specimen
- Host rock
- Typically a secondary mineral, a dehydration product of torbernite formed during weathering; formed directly above 75 °C
Where rockhounds find metatorbernite
Classic worldwide localities
- First described from Schneeberg, Saxony, Germany
- Gunnislake mine, Calstock, Cornwall, England, is thought to be primary
Field-hunting tip
Where it forms: Typically a secondary mineral, a dehydration product of torbernite formed during weathering; formed directly above 75 °C. If you start seeing torbernite, meta-autunite in float, you are in the right ground. Typical habit: tabular crystals, micaceous aggregates, crusts. Train your eye for that shape before scanning the outcrop.
