Schröckingerite is a rare secondary uranium mineral often found as bright yellow, platy or rosette-like aggregates. It is highly prized by collectors for its brilliant yellow-green fluorescence under ultraviolet light. It typically occurs as an efflorescence in oxidized zones of uranium deposits.
Is this schröckingerite?
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 schröckingerite with a known reference. Schröckingerite sits at Mohs 2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Schröckingerite leaves a pale yellow streak.
- 3Read the lusterHold the specimen under a strong light. Schröckingerite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, greenish yellow.
- 5Look at form & habitCrystal system: triclinic. Typical habit: platy crystals, rosettes, globular aggregates, crusts.
Often confused with
Schröckingerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside schröckingerite
Minerals reported to co-occur with schröckingerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCa₃(UO₂)(CO₃)₃(SO₄)F·10H₂O
- Mohs hardness
- 2.5
- Density
- 2.5 g/cm³
- Colors
- Streak
- Pale Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Platy Crystals, Rosettes, Globular Aggregates, Crusts
- Cleavage
- Perfect Basal
- Fluorescence
- Bright Yellowish-green Under UV Light
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Oxidized Uranium Deposits, Hydrothermal Veins
- Typical price
- $20-150 for thumbnail to small cabinet specimens
Where rockhounds find schröckingerite
Classic worldwide localities
- Jachymov, Czech Republic
- Wamsutter, Wyoming, USA
- Marysvale, Utah, USA
- Schneeberg, Germany
Field-hunting tip
Look in oxidized uranium deposits, hydrothermal veins country, the host setting where schröckingerite typically forms. If you start seeing uraninite, gypsum, liebigite in float, you are in the right ground. Field specimens usually show a platy crystals, rosettes, globular aggregates, crusts habit, so train your eye for that shape before scanning the outcrop.





