Ferri-winchite is a rare member of the amphibole supergroup characterized by its distinct blue to violet coloration. It is primarily found in metamorphic environments and alkaline igneous complexes as prismatic to fibrous crystals.
Is this ferri-winchite?
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 ferri-winchite with a known reference. Ferri-winchite 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. Ferri-winchite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ferri-winchite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, violet, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, fibrous aggregates.
Often confused with
Ferri-winchite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ferri-winchite
Minerals reported to co-occur with ferri-winchite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na(NaCa)Mg₄Fe³⁺(Si₈O₂₂)(OH)₂
- Mohs hardness
- 5-6
- Density
- 3.3-3.4 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Fibrous Aggregates
- Cleavage
- Perfect in Two Directions
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphic Rocks, Alkaline Igneous Rocks
- Typical price
- $20-100 per specimen
Where rockhounds find ferri-winchite
Classic worldwide localities
- Khandivali, India
- Fen Complex, Norway
- Siberia, Russia
Field-hunting tip
Look in metamorphic rocks, alkaline igneous rocks country — that is the host setting where ferri-winchite typically forms. If you start seeing calcite, diopside, apatite in float, you are in the right ground. Field specimens usually show a prismatic crystals, fibrous aggregates habit, so train your eye for that shape before scanning the outcrop.







