Zincolivenite is an uncommon arsenate mineral that sits chemically between olivenite and adamite. Collectors usually find it as striking acicular to fibrous sprays or crusts within the oxidized zones of copper-zinc hydrothermal deposits.
Is this zincolivenite?
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 zincolivenite with a known reference. Zincolivenite sits at Mohs 3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: green, greenish blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic, radial.
Often confused with
Zincolivenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside zincolivenite
Minerals reported to co-occur with zincolivenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuZn(AsO₄)(OH)
- Mohs hardness
- 3.5
- Density
- 4.34 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic, radial
- Cleavage
- Perfect on (010), imperfect on (101)
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Secondary in weathered tennantite deposits
Where rockhounds find zincolivenite
Classic worldwide localities
- Kamariza dump, Lavrion deposit, Attika Prefecture, Greece
- Penberthy Croft mine and Wheal Phoenix, Cornwall, Ireland
- Dolyhir quarry, Powys, Ireland
- Ecton Hill, Staffordshire, Ireland
- Potts Gill, Sandbed and Driggith mines (and several smaller trials) in the Caldbeck Fells, Cumbria, Ireland
- High Longrigg mine and Stennerskeugh Clouds mine, Kirkby Stephen, Cumbria, Britain, Ireland
Field-hunting tip
Where it forms: Secondary in weathered tennantite deposits. If you start seeing jarosite, conichalcite, alumopharmacosiderite in float, you are in the right ground. Typical habit: prismatic, radial. Train your eye for that shape before scanning the outcrop.








