Calcioandyrobertsite is an extremely rare arsenate mineral characterized by its delicate bladed crystal habits and pale blue coloration. It is primarily found in the secondary oxidation zones of complex hydrothermal arsenic-bearing deposits, most notably associated with the world-famous Tsumeb Mine. It is a highly sought-after species for advanced collectors of rare arsenate minerals due to its complex crystal structure and scarcity.

Hardness
3
Mohs
Luster
Vitreous
Streak
Pale blue
Transparency
Transparent

Is this calcioandyrobertsite?

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 calcioandyrobertsite with a known reference. Calcioandyrobertsite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: pale blue.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: electric blue.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: bladed crystals, radial aggregates.

Often confused with

Calcioandyrobertsite vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside calcioandyrobertsite

Minerals reported to co-occur with calcioandyrobertsite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
KCaCu₅(AsO₄)₄[As(OH)₂O₂]·2H₂O
Mohs hardness
3
Density
4.011 g/cm³
Colors
Electric blue
Streak
Pale blue
Luster
Vitreous
Transparency
Transparent
Crystal system
Monoclinic
Crystal habit
Bladed crystals, radial aggregates
Cleavage
Good on (100)
Rarity
Rare
Uses
Collector
Host rock
On a single specimen from a weathered polymetallic mineral deposit

Where rockhounds find calcioandyrobertsite

Classic worldwide localities

  • Tsumeb mine, Namibia

Field-hunting tip

Where it forms: On a single specimen from a weathered polymetallic mineral deposit. If you start seeing cuprian adamite, zincian olivenite, andyrobertsite in float, you are in the right ground. Typical habit: bladed crystals, radial aggregates. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify calcioandyrobertsite?+
Mohs hardness is 3. Luster: vitreous. The streak is pale blue. Common colors include electric blue.
Where is calcioandyrobertsite found?+
Notable localities include Tsumeb mine, Namibia.
Is calcioandyrobertsite safe to handle?+
Calcioandyrobertsite contains arsenic and copper and calls for real care. Contains arsenic, which is toxic. Handle with care, wash hands after touching, and avoid inhalation of dust.
What rocks look like calcioandyrobertsite?+
Calcioandyrobertsite is most often confused with Andyrobertsite, Cornubite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with calcioandyrobertsite?+
Calcioandyrobertsite commonly co-occurs with Cuprian adamite, Zincian olivenite, Andyrobertsite, Tennantite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does calcioandyrobertsite form in?+
Where it forms: On a single specimen from a weathered polymetallic mineral deposit. Working float back to the host body is the standard way to chase a fresh occurrence.
What is calcioandyrobertsite used for?+
Calcioandyrobertsite is used in collector.

Find calcioandyrobertsite on the map

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