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 — 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 — that is 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.


