Rösslerite is a rare magnesium arsenate mineral that typically forms as a secondary product in the oxidation zones of arsenic-rich ore deposits. It is most frequently encountered as delicate acicular crystals or white, fibrous efflorescent crusts on associated arsenate minerals.
Is this rösslerite?
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 rösslerite with a known reference. Rösslerite 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. Rösslerite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Rösslerite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow, pale green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular crystals, efflorescent crusts, radial aggregates.
Often confused with
Rösslerite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside rösslerite
Minerals reported to co-occur with rösslerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg(HAsO₄)·7H₂O
- Mohs hardness
- 2-3
- Density
- 2.44 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular Crystals, Efflorescent Crusts, Radial Aggregates
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Arsenic-rich Hydrothermal Deposits
- Typical price
- $20-150 thumbnail
Where rockhounds find rösslerite
Classic worldwide localities
- Jachymov, Czech Republic
- Schneeberg, Germany
- Guiting Power, UK
Field-hunting tip
Look in oxidized zones of arsenic-rich hydrothermal deposits country — that is the host setting where rösslerite typically forms. If you start seeing pharmacolite, scorodite, arsenopyrite in float, you are in the right ground. Field specimens usually show a acicular crystals, efflorescent crusts, radial aggregates habit, so train your eye for that shape before scanning the outcrop.




