Jáchymovite is a rare secondary uranium sulfate mineral discovered in the historic mines of Jáchymov. It typically occurs as delicate, bright yellow crystalline crusts or aggregates associated with other uranium minerals in oxidized zones.
Is this jáchymovite?
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 jáchymovite with a known reference. Jáchymovite 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. 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: monoclinic. Typical habit: acicular.
Often confused with
Jáchymovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside jáchymovite
Minerals reported to co-occur with jáchymovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (UO₂)₈(SO₄)(OH)₁₄·~13H₂O
- Mohs hardness
- 2-3
- Density
- 4.79 g/cm³
- Colors
- Streak
- Pale yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular
- Cleavage
- On {010}, very good
- Fluorescence
- Bright yellow-green under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Found on a museum specimen from the heavily oxidized portions of a uraninite-bearing vein in dolomite
Where rockhounds find jáchymovite
Classic worldwide localities
- Jáchymov (Joachimsthal), Czech Republic
Field-hunting tip
Where it forms: Found on a museum specimen from the heavily oxidized portions of a uraninite-bearing vein in dolomite. If you start seeing gypsum, uranopilite, uraninite in float, you are in the right ground. Typical habit: acicular. Train your eye for that shape before scanning the outcrop.




