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. Adamite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Adamite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, green, colorless, white, violet.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: bladed, drusy, botryoidal, radial clusters.
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 light 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
- 4.3-4.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Bladed, Drusy, Botryoidal, Radial Clusters
- Cleavage
- Distinct On {101}
- Fluorescence
- Often Bright Yellow-green Under SW/LW UV
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Oxidized Zones of Zinc Deposits
- Typical price
- $20-200 for specimens depending on crystal size and color quality
Where rockhounds find adamite
Classic worldwide localities
- Mapimi, Mexico
- Tsumeb, Namibia
- Laurion, Greece
- Gold Hill, Utah, USA
Field-hunting tip
Look in oxidized zones of zinc deposits country, the host setting where adamite typically forms. If you start seeing smithsonite, hemimorphite, limonite in float, you are in the right ground. Field specimens usually show a bladed, drusy, botryoidal, radial clusters habit, so train your eye for that shape before scanning the outcrop.


