Metaschoepite is a secondary uranium mineral that forms through the dehydration of schoepite. It is typically found as small, bright yellow, platy crystals in the oxidation zones of uranium-rich ore bodies.

Hardness
2.5
Mohs
Luster
Adamantine
Streak
Light yellow
Transparency
Semitransparent

Is this metaschoepite?

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 metaschoepite with a known reference. Metaschoepite sits at Mohs 2.5, 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.
  • 4
    Match the color range
    Compare against the expected color range: yellow, golden yellow.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: tabular crystals, platy aggregates, crusts.

Often confused with

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

Often found alongside metaschoepite

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

All properties

Chemical formula
UO₃·2H₂O
Mohs hardness
2.5
Density
4.69 g/cm³
Streak
Light yellow
Luster
Adamantine
Transparency
Semitransparent
Crystal system
Orthorhombic
Crystal habit
Tabular crystals, platy aggregates, crusts
Cleavage
{001} (by analogy to schoepite and paraschoepite, with which this is an intermediate dehydration product)
Fluorescence
Bright yellow-green under UV
Rarity
Rare
Uses
Collector
Host rock
An irreversible alteration product of schoepite from the oxidized zone of uranium-bearing mineral deposits

Where rockhounds find metaschoepite

Classic worldwide localities

  • Shinkolobwe, Katanga Province, Congo (Shaba Province, Zaire)

Field-hunting tip

Where it forms: An irreversible alteration product of schoepite from the oxidized zone of uranium-bearing mineral deposits. If you start seeing schoepite, paraschoepite in float, you are in the right ground. Typical habit: tabular crystals, platy aggregates, crusts. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify metaschoepite?+
Mohs hardness is 2.5. Luster: adamantine. The streak is light yellow. Common colors include yellow, golden yellow.
Where is metaschoepite found?+
Notable localities include Shinkolobwe, Katanga Province, Congo (Shaba Province, Zaire).
Is metaschoepite safe to handle?+
Metaschoepite contains uranium or thorium and calls for real care. This mineral is radioactive and contains uranium; handle with gloves, store in a lead-lined container, and wash hands thoroughly after contact. Do not inhale dust or ingest particles.
What rocks look like metaschoepite?+
Metaschoepite is most often confused with Schoepite, Becquerelite, Autunite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with metaschoepite?+
Metaschoepite commonly co-occurs with Schoepite, Paraschoepite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does metaschoepite form in?+
Where it forms: An irreversible alteration product of schoepite from the oxidized zone of uranium-bearing mineral deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is metaschoepite used for?+
Metaschoepite is used in collector.

Find metaschoepite on the map

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