Proto-anthophyllite is a rare magnesium-rich orthorhombic amphibole that is the high-temperature polymorph of the anthophyllite series. It typically occurs as small prismatic crystals or fibrous aggregates in magnesium-rich metamorphic rocks and can be very difficult to distinguish from common anthophyllite without specialized XRD analysis.
Is this proto-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 proto-anthophyllite with a known reference. Proto-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. Proto-anthophyllite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Proto-anthophyllite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: gray, brown, green, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, fibrous, lamellar.
Often confused with
Proto-anthophyllite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside proto-anthophyllite
Minerals reported to co-occur with proto-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
- 3.1-3.3 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic Crystals, Fibrous, Lamellar
- Cleavage
- Perfect in Two Directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Rocks of Amphibolite Facies
- Typical price
- $20-150 for small specimens
Where rockhounds find proto-anthophyllite
Classic worldwide localities
- Bamble, Norway
- Kola Peninsula, Russia
- Omi, Japan
- Madagascar
Field-hunting tip
Look in metamorphic rocks of amphibolite facies country — that is the host setting where proto-anthophyllite typically forms. If you start seeing talc, olivine, serpentine in float, you are in the right ground. Field specimens usually show a prismatic crystals, fibrous, lamellar habit, so train your eye for that shape before scanning the outcrop.







