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 — that is 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.





