Metavoltine is a rare sulfate mineral that forms as a secondary alteration product in the oxidation zones of sulfide ore deposits. It is most easily identified by its characteristic hexagonal, micaceous plate habit and distinct yellow-orange coloration. Due to its solubility, it is best found in extremely arid environments where it can persist as thin crusts or small crystalline aggregates.
Is this metavoltine?
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 metavoltine with a known reference. Metavoltine sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Metavoltine leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Metavoltine typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange, brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: hexagonal plates, micaceous aggregates, encrustations.
Often confused with
Metavoltine vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside metavoltine
Minerals reported to co-occur with metavoltine. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂Na₆Fe³⁺₃(SO₄)₁₂(OH)₂·18H₂O
- Mohs hardness
- 2.5
- Density
- 2.55 g/cm³
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Hexagonal Plates, Micaceous Aggregates, Encrustations
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Arid Oxidation Zones of Iron-bearing Sulfide Deposits
- Typical price
- $20-150 for micromounts and thumbnails
Where rockhounds find metavoltine
Classic worldwide localities
- Alcaparrosa mine, Chile
- Chuquicamata, Chile
- Sierra Gorda, Chile
- Iron Mountain, California, USA
Field-hunting tip
Look in arid oxidation zones of iron-bearing sulfide deposits country — that is the host setting where metavoltine typically forms. If you start seeing copiapite, coquimbite, fibroferrite in float, you are in the right ground. Field specimens usually show a hexagonal plates, micaceous aggregates, encrustations habit, so train your eye for that shape before scanning the outcrop.





