Bergenite is a rare secondary uranium phosphate mineral that typically occurs as small tabular crystals or radiating sprays in hydrothermal deposits. It is highly valued by radioactive mineral collectors for its vibrant yellow color and strong fluorescence under ultraviolet light.
Is this bergenite?
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 bergenite with a known reference. Bergenite sits at Mohs 2-3, 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, greenish yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular, tabular.
Often confused with
Bergenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside bergenite
Minerals reported to co-occur with bergenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Ba₄(UO₂)₉O₆(PO₄)₆·16H₂O
- Mohs hardness
- 2-3
- Density
- 4.1 g/cm³
- Colors
- Streak
- Pale yellow
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular, tabular
- Cleavage
- Perfect
- Fluorescence
- Pale orange brown green under SW and LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- On a mine dump (Streuberg, Germany) and in uranium deposits (Black Forest, Germany)
Where rockhounds find bergenite
Classic worldwide localities
- Streuberg, near Bergen, Saxony, and at Menzenschwand, Black Forest, Germany
- Black Slate Formation, Republic of South Korea
Field-hunting tip
Where it forms: On a mine dump (Streuberg, Germany) and in uranium deposits (Black Forest, Germany). If you start seeing uranocircite, torbernite, autunite in float, you are in the right ground. Typical habit: acicular, tabular. Train your eye for that shape before scanning the outcrop.




