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.

Hardness
5-6
Mohs
Luster
Vitreous
Streak
White
Transparency
Translucent

Is this cuspidine?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch cuspidine with a known reference. Cuspidine sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Cuspidine leaves a white streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Cuspidine typically shows a vitreous luster.
  • 4
    Match the color range
    Compare against the expected color range: red, yellow, brown, colorless.
  • 5
    Look at form & habit
    Crystal 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.

Common questions

How do you identify cuspidine?+
Mohs hardness is 5-6. It typically shows a vitreous luster. The streak is white. Common colors include red, yellow, brown, colorless.
Where is cuspidine found?+
Notable localities include Monte Somma, Italy; Franklin, New Jersey, USA; Khibiny Massif, Russia; Skellefte District, Sweden.
How much is cuspidine worth?+
Typical asking prices fall in the range of $20-150 for thumbnail to small cabinet specimens. Quality, size, and provenance can move individual specimens well outside that range.
What rocks look like cuspidine?+
Cuspidine is most often confused with Monticellite, Wollastonite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with cuspidine?+
Cuspidine commonly co-occurs with Calcite, Diopside, Vesuvianite, Grossular. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does cuspidine form in?+
Cuspidine typically forms in metamorphosed limestone, contact skarns. Working float back to the host body is the standard way to chase a fresh occurrence.
What is cuspidine used for?+
Cuspidine is used in collector, research.

Find cuspidine on the map

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