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.

Hardness
~5.5
Mohs
Luster
Vitreous
Streak
White
Transparency
Semitransparent

Is this arsenocrandallite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch arsenocrandallite with a known reference. Arsenocrandallite sits at Mohs ~5.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: blue green, blue.
  • 5
    Look at form & habit
    Crystal 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
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.

Common questions

How do you identify arsenocrandallite?+
Mohs hardness is ~5.5. Luster: vitreous. The streak is white. Common colors include blue green, blue.
Where is arsenocrandallite found?+
Notable localities include Centennial Eureka mine, Tintic district, Juab Co., Utah, USA; Neubulach, and in the Clara mine, near Oberwolfach, Black Forest, Germany.
Is arsenocrandallite safe to handle?+
Arsenocrandallite contains arsenic and calls for real care. Contains arsenic, which is toxic. Wash hands thoroughly after handling and avoid inhaling dust.
What rocks look like arsenocrandallite?+
Arsenocrandallite is most often confused with Crandallite, Gorceixite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with arsenocrandallite?+
Arsenocrandallite commonly co-occurs with Brochantite, Chalcophyllite, Parnauite, Barian pharmacosiderite, Bulachite, Arseniosiderite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does arsenocrandallite form in?+
Where it forms: A secondary mineral on specimens from a mine dump (Neubulach, Germany). Working float back to the host body is the standard way to chase a fresh occurrence.
What is arsenocrandallite used for?+
Arsenocrandallite is used in collector.

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