Annabergite is a secondary mineral commonly found as an alteration product of nickel arsenides in oxidized mineral veins. It is prized by collectors for its distinctive bright apple-green color, though it is very soft and delicate to handle. It is chemically related to erythrite, which typically forms pink rather than green crystals.
Is this annabergite?
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 annabergite with a known reference. Annabergite sits at Mohs 1.5-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale green to white.
- 3Read the lusterHold the specimen under a strong light. Luster: subadamantine, pearly on cleavages, may be dull, earthy.
- 4Match the color rangeCompare against the expected color range: apple-green, pale green, white, greenish white, gray, yellow green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: earthy, encrustations, massive.
Often confused with
Annabergite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Annabergite leaves pale green to white, Parabrandtite leaves white; luster reads subadamantine, pearly on cleavages, may be dull, earthy on Annabergite and vitreous on Parabrandtite.
Often found alongside annabergite
Minerals reported to co-occur with annabergite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ni₃(AsO₄)₂·8H₂O
- Mohs hardness
- 1.5-2.5
- Density
- 3.07 g/cm³
- Streak
- Pale green to white
- Luster
- Subadamantine, pearly on cleavages, may be dull, earthy
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Earthy, encrustations, massive
- Cleavage
- {010}, perfect; {100}, {102}, indistinct
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- An uncommon secondary mineral, formed by the alteration of Co–Ni-bearing arsenides and sulfides, in the oxidized zone of hydrothermal mineral deposits
Where rockhounds find annabergite
Classic worldwide localities
- Ore Hill mine, Pacoima Canyon, Los Angeles Co., and in the Kalkar quarry, Santa Cruz, Santa Cruz Co., California, USA
- Nickel and Lovelock mines, Table Mountain district, Churchill Co., Nevada, USA
- Snowbird mine, Mineral Co., Montana, USA
- Alhambra mine, Grant Co., New Mexico, USA
- Annaberg and Schneeberg, Saxony, Germany
- Richelsdorf, Hesse, Germany
Field-hunting tip
Where it forms: An uncommon secondary mineral, formed by the alteration of Co–Ni-bearing arsenides and sulfides, in the oxidized zone of hydrothermal mineral deposits. If you start seeing erythrite, retgersite, gersdorffite in float, you are in the right ground. Typical habit: earthy, encrustations, massive. Train your eye for that shape before scanning the outcrop.




