Tschermigite is a rare ammonium aluminum sulfate that typically forms as a white efflorescent crust or small octahedral crystals near burning coal seams. It is highly soluble in water and must be kept in a cool, dry environment to prevent dehydration and breakdown of the specimen.
Is this tschermigite?
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 tschermigite with a known reference. Tschermigite sits at Mohs 1.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, silky if fibrous.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: cubic. Typical habit: crystalline, deliquescent, fibrous.
Often confused with
Tschermigite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tschermigite
Minerals reported to co-occur with tschermigite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (NH₄)Al(SO₄)₂·12H₂O
- Mohs hardness
- 1.5
- Density
- 1.645 g/cm³
- Streak
- White
- Luster
- Vitreous, silky if fibrous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Crystalline, deliquescent, fibrous
- Cleavage
- Perfect on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An uncommon secondary mineral in lignite and brown coal deposits and bituminous shales and on burning coal seams or waste heaps; as efflorescences around solfataras or geothermal gas vents and fumaroles
Where rockhounds find tschermigite
1 mapped spotsClassic worldwide localities
- Burning coal waste piles at Glen Lyon, Luzerne Co., and Williamstown, Dauphin Co., Pennsylvania, USA
- Geysers, Sonoma Co., and at Sulfur Bank, Lake Co., California, USA
- Wamsutter, Sweetwater Co., Wyoming, USA
- Čermníky (Tschermig), east of Kaaden, at Libušín, near Kladno, Zastávka, near Brno, in the brown coal basins near Most and Bílina, Czech Republic
- Voinesti, Romania
- Magyarórosbánya, Hungary
Field-hunting tip
Where it forms: An uncommon secondary mineral in lignite and brown coal deposits and bituminous shales and on burning coal seams or waste heaps; as efflorescences around solfataras or geothermal gas vents and fumaroles. If you start seeing gypsum, ammoniojarosite, epsomite in float, you are in the right ground. Typical habit: crystalline, deliquescent, fibrous. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Wyoming. Start trip planning there.








