George-ericksenite is a very rare hydrated sodium-manganese-chromium arsenate mineral known primarily from the Chuquicamata mine in Chile. Collectors look for its characteristic pale yellow, radiating acicular crystal sprays found in sulfate-rich oxidized mineral assemblages.
Is this george-ericksenite?
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 george-ericksenite with a known reference. George-ericksenite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: pale yellow, bright lemon yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular, prismatic.
Often confused with
George-ericksenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside george-ericksenite
Minerals reported to co-occur with george-ericksenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₆CaMg(IO₃)₆(CrO₄)₂·12H₂O
- Mohs hardness
- 3-4
- Density
- 3.035 g/cm³
- Colors
- Pale yellowBright lemon yellow
- Streak
- Pale yellow
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular, prismatic
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- On a museum specimen from a nitrate deposit
Where rockhounds find george-ericksenite
Classic worldwide localities
- Oficina Chacabuco, Taltal district, Antofagasta, Chile
Field-hunting tip
Where it forms: On a museum specimen from a nitrate deposit. If you start seeing halite, nitratine, niter in float, you are in the right ground. Typical habit: acicular, prismatic. Train your eye for that shape before scanning the outcrop.




