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 2.5-3, 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 to adamantine.
- 4Match the color rangeCompare against the expected color range: greenish yellow, light 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
- NaFe³⁺(SO₄)₂·6H₂O
- Mohs hardness
- 2.5-3
- Density
- 2.19-2.20 g/cm³
- Streak
- White
- Luster
- Vitreous to adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals, crusts
- Cleavage
- {110}, good, but difficult
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Formed in the oxidation zones of sulfide deposits
Where rockhounds find amarillite
Classic worldwide localities
- Tierra Amarilla, southeast of Copiapó, Atacama, Chile
- Xitieshan Pb–Zn mine, south of Mt. Qilianshan, Chaidamu, Qinghai Province, China
Field-hunting tip
Where it forms: Formed in the oxidation zones of sulfide deposits. If you start seeing coquimbite in float, you are in the right ground. Typical habit: prismatic crystals, crusts. Train your eye for that shape before scanning the outcrop.



