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
Transparent to 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. Streak: white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: colorless, green, white, light pink.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: acicular, massive.

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
Ca₄(Si₂O₇)F₂
Mohs hardness
5-6
Density
2.85-2.96 g/cm³
Streak
White
Luster
Vitreous
Transparency
Transparent to translucent
Crystal system
Monoclinic
Crystal habit
Acicular, massive
Cleavage
Very good on {001}; distinct on {110}
Rarity
Rare
Uses
Collector, Research
Host rock
In tu® ejecta (Monte Somma, Italy); in contact metamorphosed limestone (Franklin, New Jersey, USA); in melilite skarn (Dupezeh Mountain, Iraq)

Where rockhounds find cuspidine

Classic worldwide localities

  • Franklin, Sussex Co., New Jersey, USA
  • Alder district, Custer Co., Idaho, USA
  • Crestmore, Riverside Co., California, USA
  • Cascade Mountain, Adirondack Mountains, Essex Co., New York, USA
  • Monte Somma and Vesuvius, Campania, and in the Alban Hills, as at Ariccia, Lazio, Italy
  • Carlingford, Co. Louth, Ireland

Field-hunting tip

Where it forms: In tu® ejecta (Monte Somma, Italy); in contact metamorphosed limestone (Franklin, New Jersey, USA); in melilite skarn (Dupezeh Mountain, Iraq). If you start seeing augite, hornblende, diopside in float, you are in the right ground. Typical habit: acicular, massive. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify cuspidine?+
Mohs hardness is 5-6. Luster: vitreous. The streak is white. Common colors include colorless, green, white, light pink.
Where is cuspidine found?+
Notable localities include Franklin, Sussex Co., New Jersey, USA; Alder district, Custer Co., Idaho, USA; Crestmore, Riverside Co., California, USA; Cascade Mountain, Adirondack Mountains, Essex Co., New York, USA; Monte Somma and Vesuvius, Campania, and in the Alban Hills, as at Ariccia, Lazio, Italy.
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 Augite, Hornblende, Diopside, Grossular, Biotite, Phlogopite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does cuspidine form in?+
Where it forms: In tu® ejecta (Monte Somma, Italy); in contact metamorphosed limestone (Franklin, New Jersey, USA); in melilite skarn (Dupezeh Mountain, Iraq). 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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