Carpholite is a distinct sorosilicate typically found as delicate, straw-like radiating fibers or sheaves in metamorphic environments. It is highly valued by collectors for its aesthetic radiating habits and vibrant straw-yellow color. It is most frequently encountered in low-grade regional metamorphic belts.
Is this carpholite?
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 carpholite with a known reference. Carpholite sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: silky, glistening.
- 4Match the color rangeCompare against the expected color range: straw yellow, greenish gray, yellowish brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: fibrous, massive, radial.
Often confused with
Carpholite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside carpholite
Minerals reported to co-occur with carpholite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MnAl₂Si₂O₆(OH)₄
- Mohs hardness
- 5.5-6
- Density
- 2.935-3.031 g/cm³
- Streak
- White
- Luster
- Silky, glistening
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Fibrous, massive, radial
- Cleavage
- Perfect on {010}
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- In low-grade metamorphosed shales
Where rockhounds find carpholite
Classic worldwide localities
- Meuville, Ardennes Mountains, Belgium
- Wippra, Harz Mountains, Germany
- Carrock mine, Caldbeck Fells, Cumbria, England
- Kit Hill Consols, Stokeclimsland, in the Hingston Down Consols mine, near Calstock, and in the Stenna Gwynn mine, St. Stephen-in-Brannel, Cornwall, England
- Fukuzumi mine, Kyoto Prefecture, Japan
Field-hunting tip
Where it forms: In low-grade metamorphosed shales. If you start seeing sudoite, manganoan garnet, chlorotoid in float, you are in the right ground. Typical habit: fibrous, massive, radial. Train your eye for that shape before scanning the outcrop.




