Ferripyrophyllite is a rare phyllosilicate mineral that represents the iron-dominant analog of pyrophyllite. It typically occurs as soft, pearly, foliated masses or coatings in metamorphosed, iron-rich sedimentary environments, often requiring X-ray diffraction for definitive identification due to its similarity to other clay minerals.
Is this ferripyrophyllite?
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 ferripyrophyllite with a known reference. Ferripyrophyllite sits at Mohs 1-2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ferripyrophyllite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ferripyrophyllite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, greenish-yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, foliated, lamellar.
Often confused with
Ferripyrophyllite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ferripyrophyllite
Minerals reported to co-occur with ferripyrophyllite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaFe³⁺Si₂O₅(OH)₂
- Mohs hardness
- 1-2
- Density
- 2.8-2.9 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Massive, Foliated, Lamellar
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphic Iron-rich Formations
- Typical price
- $20-150 per specimen depending on rarity
Where rockhounds find ferripyrophyllite
Classic worldwide localities
- Krivoy Rog, Ukraine
- Kola Peninsula, Russia
- Western Australia
Field-hunting tip
Look in metamorphic iron-rich formations country — that is the host setting where ferripyrophyllite typically forms. If you start seeing quartz, hematite, magnetite in float, you are in the right ground. Field specimens usually show a massive, foliated, lamellar habit, so train your eye for that shape before scanning the outcrop.






