Torbernite is a highly sought-after secondary uranium mineral known for its vibrant emerald-green, thin tabular or micaceous crystal clusters. It is an oxidation product of primary uranium minerals and is most commonly found in the weathered zones of uranium-bearing hydrothermal deposits.
Is this torbernite?
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 torbernite with a known reference. Torbernite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, subadamantine, waxy, pearly on cleavages; becoming dull on dehydration to metatorbernite.
- 4Match the color rangeCompare against the expected color range: emerald green, grass green, leek green, green, apple green, siskin green.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: earthy, foliated, tabular.
Often confused with
Torbernite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside torbernite
Minerals reported to co-occur with torbernite. 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)₂·10-12H₂O
- Mohs hardness
- 2-2.5
- Density
- 3.22 g/cm³
- Colors
- Streak
- Pale green
- Luster
- Vitreous, subadamantine, waxy, pearly on cleavages; becoming dull on dehydration to metatorbernite
- Transparency
- Transparent to translucent
- Crystal system
- Tetragonal
- Crystal habit
- Earthy, foliated, tabular
- Cleavage
- Perfect on {001}, micaceous; indistinct on {100}
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- An uncommon secondary mineral formed in the oxidized zone of some uraniferous copper deposits
Where rockhounds find torbernite
3 mapped spotsClassic worldwide localities
- Chalk Mountain, near Spruce Pine, Mitchell Co., North Carolina, USA
- Majuba Hill mine, Antelope district, Pershing Co., Nevada, USA
- Jáchymov (Joachimsthal), Czech Republic
- Schneeberg, Johanngeorgenstadt, Saxony, Germany
- Margabal, Aveyron, and at Les Bois Noirs, Puy-de-Dôme, France
- A number of mines in Cornwall, as Wheal Basset, Stenna Gwyn, England
Field-hunting tip
Where it forms: An uncommon secondary mineral formed in the oxidized zone of some uraniferous copper deposits. If you start seeing metatorbernite, autunite, zeunerite in float, you are in the right ground. Typical habit: earthy, foliated, tabular. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah, Connecticut. Start trip planning there.




