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, 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.




