Paradocrasite is a rare antimonide-arsenide mineral that typically forms as small, metallic inclusions within hydrothermal veins. Because it is chemically similar to stibarsen and pure arsenic, identification often requires analytical methods like X-ray diffraction or electron microprobe analysis.

Hardness
3-4
Mohs
Luster
Metallic
Streak
Black
Transparency
Opaque

Is this paradocrasite?

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 paradocrasite with a known reference. Paradocrasite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Paradocrasite leaves a black streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Paradocrasite typically shows a metallic luster.
  • 4
    Match the color range
    Compare against the expected color range: silver-white, tin-white.
  • 5
    Look at form & habit
    Crystal system: cubic. Typical habit: massive, granular, as inclusions in other minerals.

Often confused with

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

Often found alongside paradocrasite

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

All properties

Chemical formula
Sb₂As
Mohs hardness
3-4
Density
9.9-10.0 g/cm³
Streak
Black
Luster
Metallic
Transparency
Opaque
Crystal system
Cubic
Crystal habit
Massive, Granular, As Inclusions in Other Minerals
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
Hydrothermal Veins
Typical price
$50-300 per small specimen

Where rockhounds find paradocrasite

Classic worldwide localities

  • Ijol-Kha-Sere, Kazakhstan
  • Broken Hill, Australia
  • Vallone della Valletta, Italy

Field-hunting tip

Look in hydrothermal veins country — that is the host setting where paradocrasite typically forms. If you start seeing arsenic, antimony, stibarsen in float, you are in the right ground. Field specimens usually show a massive, granular, as inclusions in other minerals habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify paradocrasite?+
Mohs hardness is 3-4. It typically shows a metallic luster. The streak is black. Common colors include silver-white, tin-white.
Where is paradocrasite found?+
Notable localities include Ijol-Kha-Sere, Kazakhstan; Broken Hill, Australia; Vallone della Valletta, Italy.
How much is paradocrasite worth?+
Typical asking prices fall in the range of $50-300 per small specimen. Quality, size, and provenance can move individual specimens well outside that range.
Is paradocrasite safe to handle?+
It contains toxic constituents. Contains arsenic and antimony; avoid inhaling dust or ingesting particles and wash hands thoroughly after handling. Handle with care, avoid grinding or breathing dust, and store separately.
What rocks look like paradocrasite?+
Paradocrasite is most often confused with Stibarsen, Arsenic, Antimony. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with paradocrasite?+
Paradocrasite commonly co-occurs with Arsenic, Antimony, Stibarsen, Dyscrasite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does paradocrasite form in?+
Paradocrasite typically forms in hydrothermal veins. Working float back to the host body is the standard way to chase a fresh occurrence.
What is paradocrasite used for?+
Paradocrasite is used in collector.

Find paradocrasite on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

Download on the App StoreGet it on Google Play