Uramphite is an extremely rare ammonium uranyl phosphate mineral that typically forms as bright emerald green, thin platy crystals. It is a secondary mineral found in the oxidation zones of uranium-bearing deposits, often mistaken for similar-looking autunite or torbernite.
Is this uramphite?
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 uramphite with a known reference. Uramphite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: greenish white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: bottle green, light green.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: encrustations.
Often confused with
Uramphite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside uramphite
Minerals reported to co-occur with uramphite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (NH₄)(UO₂)(PO₄)·3H₂O
- Mohs hardness
- 2-2.5
- Density
- 3.7 g/cm³
- Colors
- Bottle greenLight green
- Streak
- Greenish white
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Tetragonal
- Crystal habit
- Encrustations
- Cleavage
- Distinct in two directions
- Fluorescence
- Medium yellow-green under SW and LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxidized zone of a uranium-coal deposit, in fractures in the coal at depths between 20 and 50 m
Where rockhounds find uramphite
Classic worldwide localities
- Tura-Kavak uranium-coal deposit, Kyrgyzstan
Field-hunting tip
Where it forms: In the oxidized zone of a uranium-coal deposit, in fractures in the coal at depths between 20 and 50 m. If you start seeing uraninite, limonite, other secondary uranium minerals in float, you are in the right ground. Typical habit: encrustations. Train your eye for that shape before scanning the outcrop.




