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 — that is 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.







