Calcioursilite is a rare secondary uranium mineral that forms in the oxidized zones of uranium deposits. It is best identified by its bright yellow color and distinct fluorescence, but it requires careful handling due to its radioactive nature.
Is this calcioursilite?
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 calcioursilite with a known reference. Calcioursilite 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. Calcioursilite leaves a pale yellow streak.
- 3Read the lusterHold the specimen under a strong light. Calcioursilite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, golden yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, fibrous, earthy masses.
Often confused with
Calcioursilite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside calcioursilite
Minerals reported to co-occur with calcioursilite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca(UO₂)₅(Si₂O₅)₃(OH)₂·~16H₂O
- Mohs hardness
- 2-3
- Density
- 3.3-3.6 g/cm³
- Colors
- Streak
- Pale Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Fibrous, Earthy Masses
- Cleavage
- Perfect Basal
- 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 intensity of radiation
Where rockhounds find calcioursilite
Classic worldwide localities
- Krivoy Rog, Ukraine
- Wölsendorf, Germany
- Lodève, France
Field-hunting tip
Look in oxidized zones of uranium-bearing hydrothermal deposits country — that is the host setting where calcioursilite typically forms. If you start seeing uraninite, autunite, quartz in float, you are in the right ground. Field specimens usually show a platy crystals, fibrous, earthy masses habit, so train your eye for that shape before scanning the outcrop.






