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 2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish orange.
- 5Look at form & habitCrystal system: orthorhombic. 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)₂(SO₄)O₂]·H₂O
- Mohs hardness
- 2.5
- Density
- 4.427-4.470 g/cm³
- Colors
- Streak
- Pale yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy crystals, crusts, aggregates
- Cleavage
- Perfect on {010} and {001}, good on {100}
- Fluorescence
- Bright yellow-green under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral on the walls of mines in U-V deposits that replaced wood and other organic material in sandstones and conglomerate (roll-front type U-V deposits)
Where rockhounds find ammoniozippeite
Classic worldwide localities
- Utah (USA)
- Colorado (USA)
- Czech Republic
Field-hunting tip
Where it forms: A secondary mineral on the walls of mines in U-V deposits that replaced wood and other organic material in sandstones and conglomerate (roll-front type U-V deposits). If you start seeing blödite, bobcookite, brochantite in float, you are in the right ground. Typical habit: platy crystals, crusts, aggregates. Train your eye for that shape before scanning the outcrop.







