Ondrušite is a rare hydrated calcium copper arsenate mineral found in the hydrothermal veins of the Jáchymov district. It typically occurs as small tabular crystals or crusts that form in association with other arsenic-bearing secondary minerals.
Is this ondrušite?
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 ondrušite with a known reference. Ondrušite sits at Mohs 4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ondrušite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Ondrušite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, aggregates.
Often confused with
Ondrušite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ondrušite
Minerals reported to co-occur with ondrušite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCu₆(AsO₄)₂(AsO₃OH)₂·10H₂O
- Mohs hardness
- 4
- Density
- 3.1-3.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Aggregates
- Cleavage
- Distinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find ondrušite
Classic worldwide localities
- Jáchymov, Czech Republic
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where ondrušite typically forms. If you start seeing arsenolite, picropharmacolite, guerinite in float, you are in the right ground. Field specimens usually show a tabular crystals, aggregates habit, so train your eye for that shape before scanning the outcrop.




