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 ~5.5, 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, blue.
- 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)(AsO₃OH)(OH)₆
- Mohs hardness
- ~5.5
- Density
- 3.25 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Trigonal
- Crystal habit
- Microcrystalline aggregates, crusts, rhombohedral crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral on specimens from a mine dump (Neubulach, Germany)
Where rockhounds find arsenocrandallite
Classic worldwide localities
- Centennial Eureka mine, Tintic district, Juab Co., Utah, USA
- Neubulach, and in the Clara mine, near Oberwolfach, Black Forest, Germany
Field-hunting tip
Where it forms: A secondary mineral on specimens from a mine dump (Neubulach, Germany). If you start seeing brochantite, chalcophyllite, parnauite in float, you are in the right ground. Typical habit: microcrystalline aggregates, crusts, rhombohedral crystals. Train your eye for that shape before scanning the outcrop.








