Aliettite is a rare regular mixed-layer silicate mineral consisting of alternating talc-like and saponite-like layers. It typically forms soft, platy, or scaly masses in hydrothermal environments and is best identified through X-ray diffraction due to its macroscopic similarity to other clay minerals.
Is this aliettite?
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 aliettite with a known reference. Aliettite 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. Aliettite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Aliettite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, gray, yellowish, greenish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy aggregates, scaly masses.
Often confused with
Aliettite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside aliettite
Minerals reported to co-occur with aliettite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ca,Na)₀.₂Mg₆(Si,Al)₈O₂₀(OH)₄·4H₂O
- Mohs hardness
- 1-2
- Density
- 2.1-2.3 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Aggregates, Scaly Masses
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Hydrothermal Veins in Mafic and Ultramafic Rocks
- Typical price
- $20-100 per specimen depending on size and rarity
Where rockhounds find aliettite
Classic worldwide localities
- Rossena, Italy
- Banská Štiavnica, Slovakia
- Milos, Greece
Field-hunting tip
Look in hydrothermal veins in mafic and ultramafic rocks country — that is the host setting where aliettite typically forms. If you start seeing calcite, dolomite, quartz in float, you are in the right ground. Field specimens usually show a platy aggregates, scaly masses habit, so train your eye for that shape before scanning the outcrop.






