Juansilvaite is an extremely rare arsenic-bearing silicate mineral discovered at the Torrecillas mine in Chile. It typically forms thin, platy, colorless to white crystal aggregates associated with other rare arsenic-rich species.
Is this juansilvaite?
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 juansilvaite with a known reference. Juansilvaite 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. Juansilvaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Juansilvaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals, crusts.
Often confused with
Juansilvaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside juansilvaite
Minerals reported to co-occur with juansilvaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Al₂As₂Si₂O₁₀(OH)₄·4H₂O
- Mohs hardness
- 2
- Density
- 2.16 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals, Crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Sedimentary Rocks
- Typical price
- $50-300+ per specimen
Where rockhounds find juansilvaite
Classic worldwide localities
- Torrecillas mine, Chile
Field-hunting tip
Look in hydrothermal veins in sedimentary rocks country — that is the host setting where juansilvaite typically forms. If you start seeing realgar, arsenolite, leucophanite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts habit, so train your eye for that shape before scanning the outcrop.





