Arsenocrandallite is a rare phosphate-arsenate mineral belonging to the crandallite group, typically found in the oxidized zones of arsenic-rich ore deposits. It usually forms as small, inconspicuous crusts or fine-grained aggregates that require careful identification through X-ray diffraction or microprobe analysis. Collectors seek it out as a specialized species from specific localities such as the Reaphook Hill occurrence in Australia.
Is this arsenocrandallite?
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 arsenocrandallite with a known reference. Arsenocrandallite sits at Mohs 5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Arsenocrandallite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Arsenocrandallite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: microcrystalline aggregates, crusts, rhombohedral crystals.
Often confused with
Arsenocrandallite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside arsenocrandallite
Minerals reported to co-occur with arsenocrandallite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaAl₃(AsO₄)(PO₄)(OH)₆
- Mohs hardness
- 5
- Density
- 3.37 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Microcrystalline Aggregates, Crusts, Rhombohedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Arsenic-rich Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find arsenocrandallite
Classic worldwide localities
- Reaphook Hill, South Australia
- Gold Hill, Utah, USA
- Laurani, Bolivia
Field-hunting tip
Look in oxidized hydrothermal arsenic-rich deposits country — that is the host setting where arsenocrandallite typically forms. If you start seeing arsenic, olivenite, cornubite in float, you are in the right ground. Field specimens usually show a microcrystalline aggregates, crusts, rhombohedral crystals habit, so train your eye for that shape before scanning the outcrop.






