Adamite is a secondary mineral found in the oxidation zones of zinc-rich mineral deposits. Collectors prize it for its vibrant yellow to green colors and frequently lustrous, radial crystal sprays or botryoidal crusts.
Is this adamite?
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 adamite with a known reference. Adamite 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: yellow, green, colorless, white, violet, pink, yellowish green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: druse, encrustations, tabular.
Often confused with
Adamite vs. its common look-alikes, and how to tell them apart in the field.


How to tell apart: Hemimorphite is the harder of the two (Mohs 4.5-5 vs. 3.5).

How to tell apart: Conichalcite is the harder of the two (Mohs 4.5 vs. 3.5); streak differs, so Adamite leaves white, Conichalcite leaves green.
Often found alongside adamite
Minerals reported to co-occur with adamite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn₂(AsO₄)(OH)
- Mohs hardness
- 3.5
- Density
- 4.32-4.48 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Druse, encrustations, tabular
- Cleavage
- {101}, good; {010}, poor
- Fluorescence
- Yellow green under SW and LW UV
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- A secondary mineral in the oxidized zone of zinc- and arsenic-bearing hydrothermal mineral deposits
Where rockhounds find adamite
Classic worldwide localities
- Gold Hill, Tooele Co., Utah, and in the Mohawk mine, Clark Mountains, San Bernardino Co., California, USA
- Chañarcillo, south of Copiapó, Atacama, Chile
- Ojuela mine, Mapimí, Durango, Mexico
- Hidalgo mine, Zimapán, Hidalgo, Mexico
- Santa Eulalia, Chihuahua, Mexico
- Cap Garonne mine, near le Pradet, Var, France
Field-hunting tip
Where it forms: A secondary mineral in the oxidized zone of zinc- and arsenic-bearing hydrothermal mineral deposits. If you start seeing smithsonite, hemimorphite, scorodite in float, you are in the right ground. Typical habit: druse, encrustations, tabular. Train your eye for that shape before scanning the outcrop.




