Ferrotochilinite is a rare, complex sulfide-hydroxide mineral belonging to the tochilinite group, typically found as microscopic platy or foliated aggregates. It is characterized by its metallic luster and black color, often occurring as an alteration product within serpentinized rocks associated with magnetite. Due to its scarcity, it is primarily sought after by advanced mineral collectors focusing on rare sulfide species.
Is this ferrotochilinite?
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 ferrotochilinite with a known reference. Ferrotochilinite 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. Ferrotochilinite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Ferrotochilinite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals or massive aggregates.
Often confused with
Ferrotochilinite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ferrotochilinite
Minerals reported to co-occur with ferrotochilinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₅₊ₓS₆(Mg,Fe,Ni)₉(OH)₁₈
- Mohs hardness
- 1-2
- Density
- 3.3-3.4 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals or Massive Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Serpentinized Ultramafic Rocks and Skarn Deposits
- Typical price
- $50-200 per specimen
Where rockhounds find ferrotochilinite
Classic worldwide localities
- Korshunovskoye iron deposit, Russia
- Kovdor, Kola Peninsula, Russia
- Chrysotile deposits, Canada
Field-hunting tip
Look in serpentinized ultramafic rocks and skarn deposits country — that is the host setting where ferrotochilinite typically forms. If you start seeing magnetite, serpentine, calcite in float, you are in the right ground. Field specimens usually show a platy crystals or massive aggregates habit, so train your eye for that shape before scanning the outcrop.







