Mrázekite is a highly sought-after secondary copper-bismuth phosphate mineral known for its intense deep blue color and distinctive thin, platy crystals. It typically forms in the oxidized zones of copper deposits where bismuth is present, often appearing as delicate rosettes or sprays on matrix.

Hardness
2-3
Mohs
Luster
Vitreous
Streak
Blue
Transparency
Translucent to transparent

Is this mrázekite?

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 mrázekite with a known reference. Mrázekite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: 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: blue, cerulean blue.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: prismatic, spherical.

Often confused with

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

Often found alongside mrázekite

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

All properties

Chemical formula
Bi₂Cu₃(PO₄)₂O₂(OH)₂·2H₂O
Mohs hardness
2-3
Density
4.90 g/cm³
Colors
BlueCerulean blue
Streak
Blue
Luster
Vitreous
Transparency
Translucent to transparent
Crystal system
Monoclinic
Crystal habit
Prismatic, spherical
Cleavage
On {201}
Rarity
Rare
Uses
Collector
Host rock
A rare secondary mineral formed by oxidization of polymetallic sulfides

Where rockhounds find mrázekite

Classic worldwide localities

  • L’ubietová, near Baňská Bystrica (Libethen, near Neusohl), Slovakia
  • Gadernheim and Reichenbach, near Bensheim, Hesse, Germany
  • Sainte-Marie-aux-Mines, Haut-Rhin, France
  • Morass Creek Gorge, 15 km north of Benambra, Victoria, Australia

Field-hunting tip

Where it forms: A rare secondary mineral formed by oxidization of polymetallic sulfides. If you start seeing chalcopyrite, tetrahedrite, chalcocite in float, you are in the right ground. Typical habit: prismatic, spherical. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify mrázekite?+
Mohs hardness is 2-3. Luster: vitreous. The streak is blue. Common colors include blue, cerulean blue.
Where is mrázekite found?+
Notable localities include L’ubietová, near Baňská Bystrica (Libethen, near Neusohl), Slovakia; Gadernheim and Reichenbach, near Bensheim, Hesse, Germany; Sainte-Marie-aux-Mines, Haut-Rhin, France; Morass Creek Gorge, 15 km north of Benambra, Victoria, Australia.
Is mrázekite safe to handle?+
Mrázekite contains copper. Contains bismuth and copper; wash hands thoroughly after handling and avoid ingestion or inhalation of dust.
What rocks look like mrázekite?+
Mrázekite is most often confused with Veszelyite, Liroconite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with mrázekite?+
Mrázekite commonly co-occurs with Chalcopyrite, Tetrahedrite, Chalcocite, Malachite, Pyromorphite, Pseudomalachite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does mrázekite form in?+
Where it forms: A rare secondary mineral formed by oxidization of polymetallic sulfides. Working float back to the host body is the standard way to chase a fresh occurrence.
What is mrázekite used for?+
Mrázekite is used in collector.

Find mrázekite on the map

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