Studtite is a rare uranyl peroxide mineral that typically forms as delicate, needle-like crystals or yellow crusts on uranium-bearing rocks. It is most famous as the first peroxide mineral discovered in nature, often forming in the oxidation zones of uranium deposits where it acts as a secondary alteration product.

Hardness
2
Mohs
Luster
Earthy
Streak
White
Transparency
Translucent

Is this studtite?

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 studtite with a known reference. Studtite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Studtite leaves a white streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Studtite typically shows a earthy luster.
  • 4
    Match the color range
    Compare against the expected color range: white, yellow, pale yellow.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: acicular crystals, fibrous, crusts, tufts.

Often confused with

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

Often found alongside studtite

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

All properties

Chemical formula
[(UO₂)O₂(H₂O)₂]·2H₂O
Mohs hardness
2
Density
3.55 g/cm³
Streak
White
Luster
Earthy
Transparency
Translucent
Crystal system
Monoclinic
Crystal habit
Acicular Crystals, Fibrous, Crusts, Tufts
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
Oxidized Zones of Uranium-rich Hydrothermal Deposits
Typical price
$50-500 depending on specimen size and clarity

Where rockhounds find studtite

Classic worldwide localities

  • Shinkolobwe Mine, Democratic Republic of the Congo
  • Jáchymov, Czech Republic
  • Wölsendorf, Germany

Field-hunting tip

Look in oxidized zones of uranium-rich hydrothermal deposits country — that is the host setting where studtite typically forms. If you start seeing curite, vandenbrandeite, kasolite in float, you are in the right ground. Field specimens usually show a acicular crystals, fibrous, crusts, tufts habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify studtite?+
Mohs hardness is 2. It typically shows a earthy luster. The streak is white. Common colors include white, yellow, pale yellow.
Where is studtite found?+
Notable localities include Shinkolobwe Mine, Democratic Republic of the Congo; Jáchymov, Czech Republic; Wölsendorf, Germany.
How much is studtite worth?+
Typical asking prices fall in the range of $50-500 depending on specimen size and clarity. Quality, size, and provenance can move individual specimens well outside that range.
Is studtite safe to handle?+
This mineral is radioactive. It contains toxic constituents. Studtite is highly radioactive and contains uranium. Handle with extreme care, store in a lead-lined container, and always wash hands thoroughly after contact. Handle with care, avoid grinding or breathing dust, and store separately.
What rocks look like studtite?+
Studtite is most often confused with Metastudtite, Becquerelite, Schoepite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with studtite?+
Studtite commonly co-occurs with Curite, Vandenbrandeite, Kasolite, Uraninite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does studtite form in?+
Studtite typically forms in oxidized zones of uranium-rich hydrothermal deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is studtite used for?+
Studtite is used in collector.

Find studtite on the map

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