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, 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.



