Clinohedrite is a prized fluorescent mineral best known from the Franklin-Sterling Hill mining district. It typically forms prismatic crystals or radial sprays that exhibit a characteristic, vivid orange fluorescence under shortwave ultraviolet light.
Is this clinohedrite?
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 clinohedrite with a known reference. Clinohedrite sits at Mohs 5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Clinohedrite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Clinohedrite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellow, pink, green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, radial aggregates, massive.
Often confused with
Clinohedrite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside clinohedrite
Minerals reported to co-occur with clinohedrite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaZn(SiO₄)·H₂O
- Mohs hardness
- 5
- Density
- 3.3 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Radial Aggregates, Massive
- Cleavage
- Perfect On {010}
- Fluorescence
- Bright Orange Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Zinc Ore Deposits
- Typical price
- $20-150 thumbnail, $200+ cabinet specimen
Where rockhounds find clinohedrite
Classic worldwide localities
- Franklin, New Jersey, USA
- Sterling Hill, New Jersey, USA
- Tsumeb, Namibia
Field-hunting tip
Look in metamorphosed zinc ore deposits country, the host setting where clinohedrite typically forms. If you start seeing willemite, franklinite, hardystonite in float, you are in the right ground. Field specimens usually show a prismatic crystals, radial aggregates, massive habit, so train your eye for that shape before scanning the outcrop.





