Grimselite is a rare uranyl carbonate mineral typically found as small, bright yellow to yellow-green tabular crystals. It is most famous from its type locality at the Grimsel Pass in Switzerland, where it occurs as a secondary mineral on granite surfaces. Collectors value it for its vibrant appearance and strong fluorescence under ultraviolet light.
Is this grimselite?
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 grimselite with a known reference. Grimselite sits at Mohs 2-2.5, 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.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: tabular crystals, crusts, or coatings.
Often confused with
Grimselite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside grimselite
Minerals reported to co-occur with grimselite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₃Na(UO₂)(CO₃)₃·H₂O
- Mohs hardness
- 2-2.5
- Density
- 3.3 g/cm³
- Colors
- Streak
- Pale yellow
- Luster
- Vitreous
- Transparency
- Translucent to transparent
- Crystal system
- Hexagonal
- Crystal habit
- Tabular crystals, crusts, or coatings
- Cleavage
- None
- Fluorescence
- Bright green under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral in veins in mineralized granodiorite
Where rockhounds find grimselite
Classic worldwide localities
- Gerstenegg (Kabelstollen Gerstenegg-Grimsel I), Grimsel, Bern, Switzerland (type locality)
Field-hunting tip
Where it forms: A rare secondary mineral in veins in mineralized granodiorite. If you start seeing schrockingerite, baylissite, monohydrocalcite in float, you are in the right ground. Typical habit: tabular crystals, crusts, or coatings. Train your eye for that shape before scanning the outcrop.




