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. Proto-ferro-anthophyllite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Proto-ferro-anthophyllite typically shows a vitreous luster.
- 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.
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
- □Fe²⁺₂(Mg₅Fe²⁺₂)Si₈O₂₂(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
- Typical price
- $20-100 per specimen
Where rockhounds find proto-ferro-anthophyllite
Classic worldwide localities
- Norway
- Sweden
- Finland
Field-hunting tip
Look in metamorphic rocks country — that is the host setting where proto-ferro-anthophyllite typically forms. If you start seeing quartz, garnet, staurolite in float, you are in the right ground. Field specimens usually show a fibrous, prismatic, or massive aggregates habit, so train your eye for that shape before scanning the outcrop.







