Nollmotzite is an extremely rare secondary uranium mineral typically found as small, deep violet-brown crusts or powdery aggregates. It occurs as an alteration product of primary uranium minerals in hydrothermal vein environments and requires professional laboratory analysis for positive identification.

Hardness
2.5
Mohs
Luster
Vitreous
Transparency
Transparent

Is this nollmotzite?

4-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 nollmotzite with a known reference. Nollmotzite sits at Mohs 2.5, softer than the next harder reference, harder than the previous one.
  • 2
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 3
    Match the color range
    Compare against the expected color range: deep violet-brown.
  • 4
    Look at form & habit
    Crystal system: monoclinic. Typical habit: microcrystalline aggregates.

Often confused with

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

Often found alongside nollmotzite

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

All properties

Chemical formula
Mg[U(UO₂)₂O₄F₃](H₂O)₄
Mohs hardness
2.5
Colors
Deep violet-brown
Luster
Vitreous
Transparency
Transparent
Crystal system
Monoclinic
Crystal habit
Microcrystalline aggregates
Cleavage
Perfect on {001}
Rarity
Rare
Uses
Collector
Host rock
Formed by precipitation from U-containing aqueous solutions under partially reducing conditions most probably enhanced by consumption of oxygen during the oxidation of abundant pyrite present in the gangue

Where rockhounds find nollmotzite

Classic worldwide localities

  • Grüner Grunde Mine, Germany
  • Schachberg, Germany

Field-hunting tip

Where it forms: Formed by precipitation from U-containing aqueous solutions under partially reducing conditions most probably enhanced by consumption of oxygen during the oxidation of abundant pyrite present in the gangue. If you start seeing fluorite, barite in float, you are in the right ground. Typical habit: microcrystalline aggregates. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify nollmotzite?+
Mohs hardness is 2.5. Luster: vitreous. Common colors include deep violet-brown.
Where is nollmotzite found?+
Notable localities include Grüner Grunde Mine, Germany; Schachberg, Germany.
Is nollmotzite safe to handle?+
Nollmotzite contains uranium or thorium and calls for real care. Contains uranium; handle with gloves and store in a lead-lined container. Avoid inhalation of dust, as the mineral is toxic and emits ionizing radiation.
What rocks look like nollmotzite?+
Nollmotzite 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 nollmotzite?+
Nollmotzite commonly co-occurs with Fluorite, Barite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does nollmotzite form in?+
Where it forms: Formed by precipitation from U-containing aqueous solutions under partially reducing conditions most probably enhanced by consumption of oxygen during the oxidation of abundant pyrite present in the gangue. Working float back to the host body is the standard way to chase a fresh occurrence.
What is nollmotzite used for?+
Nollmotzite is used in collector.

Find nollmotzite on the map

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