Creedite is a highly sought-after mineral by collectors due to its vibrant orange to purple prismatic crystals and striking radial sprays. It typically forms in the oxidation zones of ore deposits and is famous for its intense fluorescence under ultraviolet light.
Is this creedite?
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 creedite with a known reference. Creedite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, violet, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular, prismatic, radial.
Often confused with
Creedite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside creedite
Minerals reported to co-occur with creedite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Al₂(SO₄)(OH)₂F₈·2H₂O
- Mohs hardness
- 4
- Density
- 2.713-2.730 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Granular, prismatic, radial
- Cleavage
- {100}, perfect
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Uncommon in fluorite-rich hydrothermal mineral deposits
Where rockhounds find creedite
Classic worldwide localities
- Wagon Wheel Gap, near Creede, Mineral Co., Colorado, USA
- Liberty and Hall mines and at Granite, near Tonopah, Nye Co., Nevada, USA
- Grand Reef mine, Graham Co., Arizona, USA
- Thompson and Defiance mines, Darwin district, Inyo Co., California, USA
- Potosí and other mines, Santa Eulalia district, Chihuahua, Mexico
- Colquiri, La Paz, Bolivia
Field-hunting tip
Where it forms: Uncommon in fluorite-rich hydrothermal mineral deposits. If you start seeing fluorite, barite, kaolinite in float, you are in the right ground. Typical habit: granular, prismatic, radial. Train your eye for that shape before scanning the outcrop.






