Amarillite is an extremely rare thallium-bearing sulfate mineral primarily known from the copper mines of northern Chile. It typically forms as delicate, pale yellow prismatic crystals or crusts within the oxidized zones of ore deposits. Due to its thallium content and rarity, it is a specialized collector's mineral that requires careful handling.
Is this amarillite?
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 amarillite with a known reference. Amarillite 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. Amarillite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Amarillite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, crusts.
Often confused with
Amarillite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside amarillite
Minerals reported to co-occur with amarillite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaTl(SO₄)₂·6H₂O
- Mohs hardness
- 2
- Density
- 2.33 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Hydrothermal Ore Deposits
- Typical price
- $50-500 depending on specimen quality and size
Where rockhounds find amarillite
Classic worldwide localities
- Chuquicamata, Chile
Field-hunting tip
Look in oxidized zones of hydrothermal ore deposits country — that is the host setting where amarillite typically forms. If you start seeing chalcanthite, copiapite, gypsum in float, you are in the right ground. Field specimens usually show a prismatic crystals, crusts habit, so train your eye for that shape before scanning the outcrop.





