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, 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.





