Paralammerite is a rare secondary mineral typically found in the oxidation zones of arsenic-rich hydrothermal deposits. It is recognized by its distinct yellow, platy crystal morphology and is often associated with other rare arsenate minerals like its parent-like species lammerite.
Is this paralammerite?
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 paralammerite with a known reference. Paralammerite 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: yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: yellow, brownish-yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, granular aggregates.
Often confused with
Paralammerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside paralammerite
Minerals reported to co-occur with paralammerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃(AsO₄)₂
- Mohs hardness
- 3
- Density
- 3.88 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, granular aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- oxidized hydrothermal zones
Where rockhounds find paralammerite
Classic worldwide localities
- Gold Hill mine, Utah, USA
Field-hunting tip
Where it forms: oxidized hydrothermal zones. If you start seeing lammerite, austinite, conichalcite in float, you are in the right ground. Typical habit: platy crystals, granular aggregates. Train your eye for that shape before scanning the outcrop.





