Mapimite is a rare zinc-iron arsenate mineral primarily found in the oxidized zones of the Ojuela Mine in Mexico. It is most recognized for its beautiful, honey-yellow, lath-like or bladed crystals that often form radial sprays or distinct clusters.
Is this mapimite?
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 mapimite with a known reference. Mapimite sits at Mohs 3, 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: blue, green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: bladed crystals, radial sprays.
Often confused with
Mapimite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside mapimite
Minerals reported to co-occur with mapimite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn₂Fe₃(AsO₄)₃(OH)₄(H₂O)₄·6H₂O
- Mohs hardness
- 3
- Density
- 2.95 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Bladed crystals, radial sprays
- Cleavage
- On {001} and {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral in the oxidized zone of an arsenic-rich hydrothermal polymetallic ore deposit
Where rockhounds find mapimite
Classic worldwide localities
- Ojuela mine, Mapimí, Durango, Mexico
Field-hunting tip
Where it forms: A rare secondary mineral in the oxidized zone of an arsenic-rich hydrothermal polymetallic ore deposit. If you start seeing scorodite, adamite, smithsonite in float, you are in the right ground. Typical habit: bladed crystals, radial sprays. Train your eye for that shape before scanning the outcrop.






