Cuspidine is a rare nesosilicate typically found in contact metamorphic skarns associated with limestone. It is most easily identified by its characteristic bright yellow fluorescence under short-wave UV light and its elongated, prismatic crystal habit. It is highly sought after by mineral collectors for its unique fluorescent properties and occurrence in complex skarn assemblages.
Is this cuspidine?
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 cuspidine with a known reference. Cuspidine sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cuspidine leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Cuspidine typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: red, yellow, brown, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, granular aggregates.
Often confused with
Cuspidine vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside cuspidine
Minerals reported to co-occur with cuspidine. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄Si₂O₇(F,OH)₂
- Mohs hardness
- 5-6
- Density
- 2.98 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Granular Aggregates
- Cleavage
- Distinct On {100}
- Fluorescence
- Bright Yellow Under SW UV
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- Metamorphosed Limestone, Contact Skarns
- Typical price
- $20-150 for thumbnail to small cabinet specimens
Where rockhounds find cuspidine
Classic worldwide localities
- Monte Somma, Italy
- Franklin, New Jersey, USA
- Khibiny Massif, Russia
- Skellefte District, Sweden
Field-hunting tip
Look in metamorphosed limestone, contact skarns country — that is the host setting where cuspidine typically forms. If you start seeing calcite, diopside, vesuvianite in float, you are in the right ground. Field specimens usually show a prismatic crystals, granular aggregates habit, so train your eye for that shape before scanning the outcrop.






