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, 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.





