Magnesiozippeite is a rare secondary uranium mineral that forms as thin, delicate crusts and acicular crystals in the oxidation zones of uranium deposits. It is most easily identified by its vibrant yellow-green fluorescence under shortwave UV light and its close association with other secondary uranium sulfates.

Hardness
5-5.5
Mohs
Luster
Earthy
Streak
Light yellow
Transparency
Transparent

Is this magnesiozippeite?

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 magnesiozippeite with a known reference. Magnesiozippeite sits at Mohs 5-5.5, 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: earthy.
  • 4
    Match the color range
    Compare against the expected color range: yellow, yellowish orange.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: encrustations.

Often confused with

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

Often found alongside magnesiozippeite

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

All properties

Chemical formula
Mg(UO₂)₂(SO₄)O₂·3.5H₂O
Mohs hardness
5-5.5
Density
3.3 g/cm³
Streak
Light yellow
Luster
Earthy
Transparency
Transparent
Crystal system
Monoclinic
Crystal habit
Encrustations
Cleavage
Perfect on {001}
Fluorescence
Bright yellow-green under UV
Rarity
Rare
Uses
Collector
Host rock
Secondary mineral formed at low pH (<5) from the oxidation of sulfides in uranium-bearing deposits

Where rockhounds find magnesiozippeite

Classic worldwide localities

  • Lucky Strike Mine, Utah, USA
  • Jachymov, Czech Republic
  • Musonoi Mine, DR Congo

Field-hunting tip

Where it forms: Secondary mineral formed at low pH (<5) from the oxidation of sulfides in uranium-bearing deposits. If you start seeing gypsum, johannite, uraninite in float, you are in the right ground. Typical habit: encrustations. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify magnesiozippeite?+
Mohs hardness is 5-5.5. Luster: earthy. The streak is light yellow. Common colors include yellow, yellowish orange.
Where is magnesiozippeite found?+
Notable localities include Lucky Strike Mine, Utah, USA; Jachymov, Czech Republic; Musonoi Mine, DR Congo.
Is magnesiozippeite safe to handle?+
Magnesiozippeite contains uranium or thorium and calls for real care. This mineral is radioactive and contains uranium. Handle with extreme care, store in a lead-lined container, and wash hands thoroughly after handling. Do not inhale dust or allow to contaminate living spaces.
What rocks look like magnesiozippeite?+
Magnesiozippeite is most often confused with Zippeite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with magnesiozippeite?+
Magnesiozippeite commonly co-occurs with Gypsum, Johannite, Uraninite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does magnesiozippeite form in?+
Where it forms: Secondary mineral formed at low pH (<5) from the oxidation of sulfides in uranium-bearing deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is magnesiozippeite used for?+
Magnesiozippeite is used in collector.

Find magnesiozippeite on the map

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