Sailaufite is a rare calcium-manganese arsenate mineral discovered in the Spessart mountains of Germany. It typically forms thin, yellow to orange-yellow platy crystals within hydrothermal cavities, often associated with altered arsenic-bearing minerals.
Is this sailaufite?
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 sailaufite with a known reference. Sailaufite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Sailaufite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Sailaufite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-orange.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals.
Often confused with
Sailaufite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside sailaufite
Minerals reported to co-occur with sailaufite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Mn₃(AsO₄)₂(AsO₃OH)₂(H₂O)₄
- Mohs hardness
- 3
- Density
- 2.88 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Sedimentary Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find sailaufite
Classic worldwide localities
- Sailauf, Bavaria, Germany
Field-hunting tip
Look in hydrothermal veins in sedimentary rocks country, the host setting where sailaufite typically forms. If you start seeing arsenopyrite, hematite, quartz in float, you are in the right ground. Field specimens usually show a platy crystals habit, so train your eye for that shape before scanning the outcrop.





