Proto-ferro-anthophyllite is a rare member of the amphibole group found in high-grade metamorphic environments. It typically occurs as prismatic or fibrous crystals and is often chemically related to anthophyllite and grunerite, requiring laboratory analysis for definitive identification.
Is this proto-ferro-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-ferro-anthophyllite with a known reference. Proto-ferro-anthophyllite sits at Mohs 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: vitreous.
- 4Match the color rangeCompare against the expected color range: brown, greenish-brown, dark gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: fibrous, prismatic, or massive aggregates.
Often confused with
Proto-ferro-anthophyllite vs. its common look-alikes, and how to tell them apart in the field.


How to tell apart: Streak differs, so Proto-ferro-anthophyllite leaves white, Cummingtonite leaves grayish white.

How to tell apart: Streak differs, so Proto-ferro-anthophyllite leaves white, Grunerite leaves colorless.
Often found alongside proto-ferro-anthophyllite
Minerals reported to co-occur with proto-ferro-anthophyllite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₇Si₈O₂₂(OH)₂
- Mohs hardness
- 5-6
- Density
- 3.3-3.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Fibrous, prismatic, or massive aggregates
- Cleavage
- Perfect in two directions
- Rarity
- Rare
- Uses
- Collector
- Host rock
- metamorphic rocks
Where rockhounds find proto-ferro-anthophyllite
Classic worldwide localities
- Norway
- Sweden
- Finland
Field-hunting tip
Where it forms: metamorphic rocks. If you start seeing quartz, garnet, staurolite in float, you are in the right ground. Typical habit: fibrous, prismatic, or massive aggregates. Train your eye for that shape before scanning the outcrop.




