Anthophyllite is a magnesium-rich amphibole typically found in regionally metamorphosed rocks. It is easily identified by its characteristic clove-brown to grayish color and its fibrous or lamellar habit, though it should be handled with extreme caution due to its asbestiform nature.
Is this anthophyllite?
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 anthophyllite with a known reference. Anthophyllite 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. Anthophyllite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Anthophyllite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, gray, white, greenish.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: fibrous, columnar, or lamellar.
Often confused with
Anthophyllite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside anthophyllite
Minerals reported to co-occur with anthophyllite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₂Mg₅Si₈O₂₂(OH)₂
- Mohs hardness
- 5.5-6
- Density
- 2.8-3.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Fibrous, Columnar, Or Lamellar
- Cleavage
- Perfect in Two Directions
- Rarity
- Common
- Uses
- Collector, Geological Study
- Host rock
- Metamorphic Rocks Like Schist and Gneiss
- Typical price
- $10-50 per specimen
Where rockhounds find anthophyllite
2 mapped spotsClassic worldwide localities
- Kongsberg, Norway
- Amity, New York, USA
- Finland
- Greenland
Field-hunting tip
Look in metamorphic rocks like schist and gneiss country, the host setting where anthophyllite typically forms. If you start seeing garnet, cordierite, talc in float, you are in the right ground. Field specimens usually show a fibrous, columnar, or lamellar habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in California, New York. Start trip planning there.







