Meisserite is a rare uranyl sulfate mineral typically found as small, bright yellow tabular crystals in oxidized uranium deposits. It is primarily known from the Blue Lizard mine in Utah, where it occurs as a secondary mineral in association with other rare sulfates. Due to its radioactive nature and extreme rarity, it is a highly specialized specimen for advanced mineral collectors.
Is this meisserite?
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 meisserite with a known reference. Meisserite 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. Meisserite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Meisserite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange-yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, subparallel aggregates.
Often confused with
Meisserite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside meisserite
Minerals reported to co-occur with meisserite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₆(UO₂)(SO₄)₄
- Mohs hardness
- 3
- Density
- 3.37 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Subparallel Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Uranium-bearing Sandstone
- Typical price
- $100-500 per specimen
Where rockhounds find meisserite
Classic worldwide localities
- Blue Lizard mine, San Juan County, Utah, USA
Field-hunting tip
Look in uranium-bearing sandstone country — that is the host setting where meisserite typically forms. If you start seeing johannite, zippeite, gypsum in float, you are in the right ground. Field specimens usually show a tabular crystals, subparallel aggregates habit, so train your eye for that shape before scanning the outcrop.




