Juansilvaite is an extremely rare arsenic-bearing silicate mineral discovered at the Torrecillas mine in Chile. It typically forms thin, platy, bright pink 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 ~2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: bright pink.
- 5Look at form & habitCrystal system: monoclinic. 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
- Na₅Al₃[AsO₃(OH)]₄[AsO₂(OH)₂]₂(SO₄)₂·4H₂O
- Mohs hardness
- ~2.5
- Density
- 3.01 g/cm³
- Colors
- Bright pink
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, crusts
- Cleavage
- Very good on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- From the oxidation of native arsenic and other As-bearing primary phases, followed by later alteration by saline fluids derived from evaporating meteoric water under hyperarid conditions
Where rockhounds find juansilvaite
Classic worldwide localities
- Torrecillas mine, northern Atacama Desert, Iquique Province, Chile
Field-hunting tip
Where it forms: From the oxidation of native arsenic and other As-bearing primary phases, followed by later alteration by saline fluids derived from evaporating meteoric water under hyperarid conditions. If you start seeing anhydrite, canutite, halite in float, you are in the right ground. Typical habit: platy crystals, crusts. Train your eye for that shape before scanning the outcrop.






