Fougèrite is a member of the hydrotalcite supergroup often referred to as 'green rust' due to its appearance in soil chemistry and anaerobic environments. It occurs as microscopic, hexagonal, platy crystals that are highly sensitive to oxidation, making it difficult to collect and preserve in its primary form.
Is this fougèrite?
3-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 fougèrite with a known reference. Fougèrite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: bluish gray.
- 3Look at form & habitCrystal system: trigonal. Typical habit: platy crystals, fine-grained aggregates, crusts.
Often confused with
Fougèrite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside fougèrite
Minerals reported to co-occur with fougèrite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₄Fe₂(OH)₁₂(CO₃)·3H₂O
- Mohs hardness
- 2
- Density
- 2.2-2.5 g/cm³
- Colors
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Platy crystals, fine-grained aggregates, crusts
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- Forms by partial oxidation and hydrolysis of aqueous Fe2+
Where rockhounds find fougèrite
Classic worldwide localities
- Discovered coloring (green) the soil of the Fougères Forest in the Ille-et-Vilaine region of France (type locality)
Field-hunting tip
Where it forms: Forms by partial oxidation and hydrolysis of aqueous Fe2+. If you start seeing kaolinite, vermiculite, quartz in float, you are in the right ground. Typical habit: platy crystals, fine-grained aggregates, crusts. Train your eye for that shape before scanning the outcrop.







