Devilline is a striking secondary copper mineral that typically forms delicate, fan-shaped clusters of bright blue to greenish-blue platy crystals. It is most commonly found in the oxidation zones of sulfide ore deposits, often appearing as coatings on other copper minerals like malachite or azurite. Because of its fragile nature and solubility, it is highly prized by mineral collectors who appreciate its vivid color and unique crystal habits.
Is this devilline?
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 devilline with a known reference. Devilline 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: pale green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, may be pearly on {001}.
- 4Match the color rangeCompare against the expected color range: blue, blue green, blue white, white, dark green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy, spherical, tabular.
Often confused with
Devilline vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside devilline
Minerals reported to co-occur with devilline. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCu₄(SO₄)₂(OH)₆·3H₂O
- Mohs hardness
- 2.5
- Density
- 3.13 g/cm³
- Colors
- Streak
- Pale green
- Luster
- Vitreous, may be pearly on {001}
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy, spherical, tabular
- Cleavage
- On {001}, perfect; on {110}, {101}, {101}, distinct
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- An uncommon secondary mineral in the oxidized portions of copper sulfide deposits; may be of post-mining origin in dumps and on timbers
Where rockhounds find devilline
Classic worldwide localities
- Ecton mine, Montgomery Co., Pennsylvania, USA
- Sterling Hill, Ogdensburg, New Jersey, USA
- Majuba Hill, Pershing Co., Nevada, USA
- Trixie mine, Tintic district, Juab Co., Utah, USA
- Cornwall, at several mines around St. Just, St. Hilary, and Gwinear, England
- Wheal Friendship, Mary Tavy, Devon, England
Field-hunting tip
Where it forms: An uncommon secondary mineral in the oxidized portions of copper sulfide deposits; may be of post-mining origin in dumps and on timbers. If you start seeing langite, antlerite, brochantite in float, you are in the right ground. Typical habit: platy, spherical, tabular. Train your eye for that shape before scanning the outcrop.






