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, 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.






