Lausenite is a rare iron sulfate mineral that typically forms as an efflorescence or crust on decomposing iron sulfide minerals. It is highly unstable in humid conditions and can easily dehydrate or dissolve, making it a challenging mineral for collectors to store and display.
Is this lausenite?
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 lausenite with a known reference. Lausenite sits at Mohs 2-3, 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: silky.
- 4Match the color rangeCompare against the expected color range: white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous.
Often confused with
Lausenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside lausenite
Minerals reported to co-occur with lausenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₂(SO₄)₃(H₂O)₅
- Mohs hardness
- 2-3
- Density
- 2.2-2.3 g/cm³
- Colors
- Streak
- White
- Luster
- Silky
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A very rare mineral, formed as the result of burning of a pyritic orebody (United Verde mine, Arizona, USA); on a burning waste heap formed by oxidation of pyrite reacting with clay (Velikomostov-2 mine, Ukraine)
Where rockhounds find lausenite
Classic worldwide localities
- United Verde mine, Jerome, Yavapai Co., Arizona, USA
- Velikomostov-2 coal mine, L’vov-Volyn’ Basin, Ukraine
Field-hunting tip
Where it forms: A very rare mineral, formed as the result of burning of a pyritic orebody (United Verde mine, Arizona, USA); on a burning waste heap formed by oxidation of pyrite reacting with clay (Velikomostov-2 mine, Ukraine). If you start seeing copiapite, kieserite in float, you are in the right ground. Typical habit: fibrous. Train your eye for that shape before scanning the outcrop.



