Swartzite is a rare uranyl carbonate mineral that typically forms distinct, thin tabular crystals with a bright yellow-green color. Collectors prize it for its intense green fluorescence under ultraviolet light. It is primarily found as a secondary mineral in oxidized uranium deposits in the western United States.
Is this swartzite?
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 swartzite with a known reference. Swartzite 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. Swartzite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Swartzite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, yellow-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Swartzite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside swartzite
Minerals reported to co-occur with swartzite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaMg(UO₂)(CO₃)₃·12H₂O
- Mohs hardness
- 2.5
- Density
- 2.12 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect
- Fluorescence
- Bright Yellow-green Under UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Uranium-bearing Hydrothermal Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find swartzite
Classic worldwide localities
- Grants, New Mexico, USA
- Utah, USA
- Czech Republic
Field-hunting tip
Look in oxidized zones of uranium-bearing hydrothermal deposits country — that is the host setting where swartzite typically forms. If you start seeing andersonite, liebigite, bayleyite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.




