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 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Creedite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Creedite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, orange, purple, pink.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, radial sprays, botryoidal crusts.
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(F,OH)₁₀·2H₂O
- Mohs hardness
- 3.5-4
- Density
- 2.7 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Radial Sprays, Botryoidal Crusts
- Cleavage
- Perfect in One Direction
- Fluorescence
- Bright Orange or Yellow Under UV
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $10-150 thumbnail, $50-500 cabinet
Where rockhounds find creedite
Classic worldwide localities
- Creede, Colorado, USA
- Durango, Mexico
- Tajikistan
- China
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where creedite typically forms. If you start seeing fluorite, quartz, barite in float, you are in the right ground. Field specimens usually show a prismatic crystals, radial sprays, botryoidal crusts habit, so train your eye for that shape before scanning the outcrop.







