Llantenesite is a rare magnesium-iron sulfate mineral belonging to the copiapite group. It is typically found as small, fragile tabular crystals or yellow powdery crusts in the oxidized zones of sulfate-rich mineral deposits.
Is this llantenesite?
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 llantenesite with a known reference. Llantenesite 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. Llantenesite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Llantenesite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-orange.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, crusts, efflorescent aggregates.
Often confused with
Llantenesite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside llantenesite
Minerals reported to co-occur with llantenesite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MgFe₄³⁺(SO₄)₆(OH)₂·20H₂O
- Mohs hardness
- 2.5-3
- Density
- 2.16 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Crusts, Efflorescent Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Sulfide Ore Deposits
- Typical price
- $20-100 for small specimen
Where rockhounds find llantenesite
Classic worldwide localities
- La Alcaparrosa mine, Argentina
- Sierra Gorda, Chile
- Chuquicamata, Chile
Field-hunting tip
Look in oxidized zones of sulfide ore deposits country — that is the host setting where llantenesite typically forms. If you start seeing copiapite, jarosite, melanterite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts, efflorescent aggregates habit, so train your eye for that shape before scanning the outcrop.





