Derriksite is an extremely rare secondary copper uranyl selenite mineral typically found as small, vibrant emerald-green platy crystals. It occurs primarily in the oxidation zones of uranium deposits where selenium is present. Due to its scarcity and radioactivity, it is highly sought after by advanced systematic mineral collectors.
Is this derriksite?
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 derriksite with a known reference. Derriksite sits at Mohs 2-3, 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: adamantine.
- 4Match the color rangeCompare against the expected color range: bottle green, green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals, crusts, tabular.
Often confused with
Derriksite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside derriksite
Minerals reported to co-occur with derriksite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₄(UO₂)(SeO₃)₂(OH)₆
- Mohs hardness
- 2-3
- Density
- 4.72 g/cm³
- Colors
- Bottle greenGreen
- Streak
- Pale green
- Luster
- Adamantine
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy crystals, crusts, tabular
- Cleavage
- On {010}, very good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Very rare in the oxidized portions of a selenium-bearing Cu–Co deposit
Where rockhounds find derriksite
Classic worldwide localities
- Musonoi Cu–Co mine, near Kolwezi, Katanga Province, Congo (Shaba Province, Zaire)
Field-hunting tip
Where it forms: Very rare in the oxidized portions of a selenium-bearing Cu–Co deposit. If you start seeing selenian digenite, chalcomenite, demesmaekerite in float, you are in the right ground. Typical habit: platy crystals, crusts, tabular. Train your eye for that shape before scanning the outcrop.




