Seelite is a rare magnesium-uranium arsenate mineral known for its vibrant yellow, micaceous platy crystals. It is typically found as a secondary mineral in uranium-rich ore deposits, often forming thin crusts or small crystal sprays on matrix.
Is this seelite?
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 seelite with a known reference. Seelite sits at Mohs ~3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: canary-yellow, apple-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts.
Often confused with
Seelite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Seelite leaves white, Autunite leaves pale yellow.

How to tell apart: Streak differs, so Seelite leaves white, Meta-autunite leaves yellow; luster reads vitreous on Seelite and pearly to dull on Meta-autunite.

How to tell apart: Streak differs, so Seelite leaves white, Torbernite leaves pale green.
Often found alongside seelite
Minerals reported to co-occur with seelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₃(UO₂)₂(AsO₄)₂·10H₂O
- Mohs hardness
- ~3
- Density
- 3.70 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, crusts
- Cleavage
- Perfect
- Fluorescence
- Bright yellow under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare mineral in the oxidation zone of uranium-bearing hydrothermal deposits
Where rockhounds find seelite
Classic worldwide localities
- Talmessi mine, 35 km west of Anarak, Iran
- Rabéjac uranium deposit, seven km south-southeast of Lodève, Hérault, France
Field-hunting tip
Where it forms: A rare mineral in the oxidation zone of uranium-bearing hydrothermal deposits. If you start seeing annabergite, talmessite, zaratite in float, you are in the right ground. Typical habit: platy crystals, crusts. Train your eye for that shape before scanning the outcrop.





