Nickelzippeite is a rare secondary uranium mineral typically forming as vibrant yellow acicular or lath-like crystals in oxidized uranium ore deposits. It is known for its intense yellow-green fluorescence under ultraviolet light. Due to its radioactive nature, it is primarily sought after by advanced collectors of secondary uranium minerals.
Is this nickelzippeite?
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 nickelzippeite with a known reference. Nickelzippeite 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. Nickelzippeite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Nickelzippeite 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: acicular crystals, laths, crusts.
Often confused with
Nickelzippeite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside nickelzippeite
Minerals reported to co-occur with nickelzippeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ni(UO₂)₂(SO₄)(OH)₄·16H₂O
- Mohs hardness
- 2
- Density
- 4.1 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular Crystals, Laths, Crusts
- Cleavage
- Perfect On {001}
- Fluorescence
- Bright Yellow-green Under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Uranium-bearing Hydrothermal Deposits
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find nickelzippeite
Classic worldwide localities
- Jachymov, Czech Republic
- Great Bear Lake, Canada
- Utah, USA
- Colorado, USA
Field-hunting tip
Look in oxidized zones of uranium-bearing hydrothermal deposits country — that is the host setting where nickelzippeite typically forms. If you start seeing uraninite, gypsum, jarosite in float, you are in the right ground. Field specimens usually show a acicular crystals, laths, crusts habit, so train your eye for that shape before scanning the outcrop.





