Paradamite is a rare zinc arsenate mineral that is structurally related to hopeite. It typically forms as sharp, gemmy yellow to colorless crystals in the oxidized zones of ore deposits, most famously at the Ojuela Mine in Mexico. Collectors prize it for its high transparency and delicate crystal geometry.
Is this paradamite?
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 paradamite with a known reference. Paradamite 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. Paradamite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Paradamite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, colorless, white.
- 5Look at form & habitCrystal system: triclinic. Typical habit: prismatic to tabular crystals.
Often confused with
Paradamite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside paradamite
Minerals reported to co-occur with paradamite. 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
- 3.36 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Prismatic to Tabular Crystals
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Hydrothermal Base Metal Deposits
- Typical price
- $50-500 depending on crystal size and clarity
Where rockhounds find paradamite
Classic worldwide localities
- Mapimi, Mexico
Field-hunting tip
Look in oxidized zones of hydrothermal base metal deposits country — that is the host setting where paradamite typically forms. If you start seeing adamite, smithsonite, goethite in float, you are in the right ground. Field specimens usually show a prismatic to tabular crystals habit, so train your eye for that shape before scanning the outcrop.






