Ammoniozippeite is a rare secondary uranium sulfate mineral typically found as yellow-orange crusts or small platy crystals in oxidized uranium-bearing ore deposits. Due to its radioactive nature, it is primarily sought after by advanced mineral collectors who specialize in uranium minerals.
Is this ammoniozippeite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch ammoniozippeite with a known reference. Ammoniozippeite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ammoniozippeite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Ammoniozippeite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange-yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts, aggregates.
Often confused with
Ammoniozippeite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ammoniozippeite
Minerals reported to co-occur with ammoniozippeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (NH₄)₂(UO₂)₄(SO₄)₂(OH)₆·3H₂O
- Mohs hardness
- 2
- Density
- 3.9 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Crusts, Aggregates
- Cleavage
- Perfect On {001}
- Fluorescence
- Bright Yellow-green Under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Uranium Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find ammoniozippeite
Classic worldwide localities
- Utah (USA)
- Colorado (USA)
- Czech Republic
Field-hunting tip
Look in oxidized uranium deposits country — that is the host setting where ammoniozippeite typically forms. If you start seeing gypsum, schroeckingerite, uraninite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, aggregates habit, so train your eye for that shape before scanning the outcrop.



