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, 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.






