Przhevalskite is a rare secondary uranium phosphate mineral that typically forms as bright yellow tabular crystals or crusts. It is most commonly found in the oxidation zones of uranium-rich hydrothermal deposits and is highly prized by collectors for its strong fluorescence.

Hardness
2-3
Mohs
Luster
Adamantine, vitreous to pearly
Streak
Light yellow
Transparency
Semitransparent

Is this przhevalskite?

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 przhevalskite with a known reference. Przhevalskite 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: light yellow.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: adamantine, vitreous to pearly.
  • 4
    Match the color range
    Compare against the expected color range: yellow, bright greenish yellow.
  • 5
    Look at form & habit
    Crystal system: tetragonal. Typical habit: aggregates, foliated.

Often confused with

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

Often found alongside przhevalskite

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

All properties

Chemical formula
Pb(UO₂)₂(PO₄)₂·4H₂O
Mohs hardness
2-3
Density
3.38 g/cm³
Colors
YellowBright greenish yellow
Streak
Light yellow
Luster
Adamantine, vitreous to pearly
Transparency
Semitransparent
Crystal system
Tetragonal
Crystal habit
Aggregates, foliated
Cleavage
On {001}, good
Rarity
Rare
Uses
Collector
Host rock
A rare secondary mineral in the oxidized zone of a uranium deposit

Where rockhounds find przhevalskite

Classic worldwide localities

  • Dzherkamar uranium deposit, ten km southeast of Adraman, Karamazar Mountains, Tajikistan

Field-hunting tip

Where it forms: A rare secondary mineral in the oxidized zone of a uranium deposit. If you start seeing torbernite, autunite, dumontite in float, you are in the right ground. Typical habit: aggregates, foliated. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify przhevalskite?+
Mohs hardness is 2-3. Luster: adamantine, vitreous to pearly. The streak is light yellow. Common colors include yellow, bright greenish yellow.
Where is przhevalskite found?+
Notable localities include Dzherkamar uranium deposit, ten km southeast of Adraman, Karamazar Mountains, Tajikistan.
Is przhevalskite safe to handle?+
Przhevalskite contains lead and uranium or thorium and calls for real care. This mineral is radioactive due to its uranium content and contains lead. Handle with care, wear gloves, avoid inhalation of dust, and store in a lead-lined container or away from human living spaces.
What rocks look like przhevalskite?+
Przhevalskite is most often confused with Autunite, Torbernite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with przhevalskite?+
Przhevalskite commonly co-occurs with Torbernite, Autunite, Dumontite, Dewindtite, Uranophane, Wulfenite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does przhevalskite form in?+
Where it forms: A rare secondary mineral in the oxidized zone of a uranium deposit. Working float back to the host body is the standard way to chase a fresh occurrence.
What is przhevalskite used for?+
Przhevalskite is used in collector.

Find przhevalskite on the map

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