Ammoniomagnesiovoltaite is a very rare sulfate mineral in the voltaite group, typically found as small, dark octahedral crystals. It forms primarily in the oxidized zones of mining environments where ammonium-rich solutions interact with magnesium and iron sulfides.
Is this ammoniomagnesiovoltaite?
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 ammoniomagnesiovoltaite with a known reference. Ammoniomagnesiovoltaite 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. Ammoniomagnesiovoltaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ammoniomagnesiovoltaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: black, dark green, brown.
- 5Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals, often with cube faces.
Often confused with
Ammoniomagnesiovoltaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ammoniomagnesiovoltaite
Minerals reported to co-occur with ammoniomagnesiovoltaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (NH₄)₂Mg₅Fe³⁺₃Al(SO₄)₁₂·18H₂O
- Mohs hardness
- 2.5-3
- Density
- 2.55 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Octahedral Crystals, Often with Cube Faces
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Sulfide-rich Ore Deposits, Coal Mine Dumps
Where rockhounds find ammoniomagnesiovoltaite
Classic worldwide localities
- Near Köves Hill, Pécs-Vasas, Mecsek Mountains, southern Hungary
Field-hunting tip
Look in oxidized zones of sulfide-rich ore deposits, coal mine dumps country, the host setting where ammoniomagnesiovoltaite typically forms. If you start seeing gypsum, alunogen, jarosite in float, you are in the right ground. Field specimens usually show a octahedral crystals, often with cube faces habit, so train your eye for that shape before scanning the outcrop.





