Spurrite is a relatively uncommon calcium silicate carbonate mineral typically formed during the contact metamorphism of limestone. Collectors should look for its distinctive bright yellow fluorescence under short-wave ultraviolet light, which is its most reliable diagnostic feature in field settings.
Is this spurrite?
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 spurrite with a known reference. Spurrite 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. Spurrite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Spurrite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, gray, pale blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular, massive, rarely in flattened crystals.
Often confused with
Spurrite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside spurrite
Minerals reported to co-occur with spurrite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₅(SiO₄)₂(CO₃)
- Mohs hardness
- 5
- Density
- 2.71 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Granular, Massive, Rarely in Flattened Crystals
- Cleavage
- Distinct in One Direction
- Fluorescence
- Bright Yellow Under SW UV
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Contact Metamorphic Zones in Limestone
- Typical price
- $10-50 per specimen
Where rockhounds find spurrite
Classic worldwide localities
- Chukotka, Russia
- County Antrim, Northern Ireland
- Riverside County, California, USA
- Velardena, Mexico
Field-hunting tip
Look in contact metamorphic zones in limestone country — that is the host setting where spurrite typically forms. If you start seeing calcite, gehlenite, larnite in float, you are in the right ground. Field specimens usually show a granular, massive, rarely in flattened crystals habit, so train your eye for that shape before scanning the outcrop.





