Weeksite is a distinctive radioactive uranium mineral typically found as radiating clusters of yellow, fan-shaped crystals or crusts. It is highly prized by collectors of radioactive species for its vibrant yellow-green fluorescence under ultraviolet light.
Is this weeksite?
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 weeksite with a known reference. Weeksite 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. Weeksite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Weeksite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: radiating globular aggregates, crusts, fan-shaped sprays.
Often confused with
Weeksite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside weeksite
Minerals reported to co-occur with weeksite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂(UO₂)₂(Si₂O₅)₃·4H₂O
- Mohs hardness
- 2
- Density
- 3.9-4.1 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Radiating Globular Aggregates, Crusts, Fan-shaped Sprays
- Cleavage
- Perfect
- Fluorescence
- Bright Yellow-green Under UV
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Rhyolitic Volcanic Rocks, Hydrothermal Veins
- Typical price
- $30-200 depending on specimen size and radioactivity levels
Where rockhounds find weeksite
Classic worldwide localities
- Thomas Range, Utah, USA
- Wheeler County, Georgia, USA
- Kazakhstan
Field-hunting tip
Look in rhyolitic volcanic rocks, hydrothermal veins country — that is the host setting where weeksite typically forms. If you start seeing fluorite, quartz, chalcedony in float, you are in the right ground. Field specimens usually show a radiating globular aggregates, crusts, fan-shaped sprays habit, so train your eye for that shape before scanning the outcrop.






