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.

Hardness
5.5-6
Mohs
Luster
Silky, glistening
Streak
White
Transparency
Semitransparent

Is this carpholite?

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 carpholite with a known reference. Carpholite sits at Mohs 5.5-6, 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: silky, glistening.
  • 4
    Match the color range
    Compare against the expected color range: straw yellow, greenish gray, yellowish brown.
  • 5
    Look at form & habit
    Crystal 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.

Common questions

How do you identify carpholite?+
Mohs hardness is 5.5-6. Luster: silky, glistening. The streak is white. Common colors include straw yellow, greenish gray, yellowish brown.
Where is carpholite found?+
Notable localities include 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.
What rocks look like carpholite?+
Carpholite is most often confused with Pectolite, Tremolite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with carpholite?+
Carpholite commonly co-occurs with Sudoite, Manganoan garnet, Chlorotoid, Fluorite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does carpholite form in?+
Where it forms: In low-grade metamorphosed shales. Working float back to the host body is the standard way to chase a fresh occurrence.
What is carpholite used for?+
Carpholite is used in collector.

Find carpholite on the map

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