Brugnatellite is a rare layered double hydroxide mineral typically found as soft, platy, or micaceous aggregates. It is most commonly identified in serpentinite rocks where it forms alongside other magnesium-rich minerals in low-temperature alteration zones.
Is this brugnatellite?
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 brugnatellite with a known reference. Brugnatellite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Brugnatellite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Brugnatellite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: pale pink, pale brownish, pale yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: platy or foliated aggregates, crusts.
Often confused with
Brugnatellite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside brugnatellite
Minerals reported to co-occur with brugnatellite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₆Fe³⁺(CO₃)(OH)₁₃·4H₂O
- Mohs hardness
- 2
- Density
- 2.12 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Platy or Foliated Aggregates, Crusts
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Serpentinite and Alkaline Igneous Rocks
- Typical price
- $20-100 per specimen depending on size
Where rockhounds find brugnatellite
Classic worldwide localities
- Brugnato, Liguria, Italy
- Khibiny Massif, Russia
- Mont Saint-Hilaire, Canada
Field-hunting tip
Look in serpentinite and alkaline igneous rocks country — that is the host setting where brugnatellite typically forms. If you start seeing aragonite, calcite, brucite in float, you are in the right ground. Field specimens usually show a platy or foliated aggregates, crusts habit, so train your eye for that shape before scanning the outcrop.






