Mascagnite is an ammonium sulfate mineral typically found as a sublimated crust around volcanic fumaroles or in areas of burning coal seams. It is highly water-soluble, meaning specimens must be kept in sealed containers in a dry, cool environment to prevent deliquescence or dissolution.
Is this mascagnite?
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 mascagnite with a known reference. Mascagnite sits at Mohs 2-2.5, 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 to dull.
- 4Match the color rangeCompare against the expected color range: white, colorless, gray, grayish yellow, yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: stalactitic, water soluble.
Often confused with
Mascagnite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside mascagnite
Minerals reported to co-occur with mascagnite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (NH₄)₂SO₄
- Mohs hardness
- 2-2.5
- Density
- 1.768 g/cm³
- Streak
- White
- Luster
- Vitreous to dull
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Stalactitic, water soluble
- Cleavage
- {100}, good
- Rarity
- Uncommon
- Uses
- Collector, Scientific
- Host rock
- A sublimation product in fumaroles and solfataras; formed by burning coal seams
Where rockhounds find mascagnite
Classic worldwide localities
- Geysers, Sonoma Co., California, USA
- Kehley’s Run mine, near Shenandoah, Schuylkill Co., and Glen Lyon, Luzerne Co., Pennsylvania, USA
- Bitter Creek, near Wamsutter, Sweetwater Co., Wyoming, USA
- Vesuvius, Campania, and Etna, Sicily, Italy
- Volcanoes on the Kamchatka Peninsula, Russia
- Clara mine, near Oberwolfach, Black Forest, and on the dump of the Paul-Berndt mine, Freital, Saxony, Germany
Field-hunting tip
Where it forms: A sublimation product in fumaroles and solfataras; formed by burning coal seams. If you start seeing sal ammoniac, tschermigite, sylvite in float, you are in the right ground. Typical habit: stalactitic, water soluble. Train your eye for that shape before scanning the outcrop.








