Švenekite is a very rare calcium arsenate mineral that typically forms as delicate, colorless tabular crystals or thin crusts in weathered arsenic-rich deposits. It is named after the mineralogist Karel Švenek and is primarily found in old mining districts where oxidation of primary arsenic minerals has occurred.
Is this švenekite?
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 švenekite with a known reference. Švenekite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Švenekite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Švenekite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, crusts.
Often confused with
Švenekite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside švenekite
Minerals reported to co-occur with švenekite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca(H₂AsO₄)₂
- Mohs hardness
- 2
- Density
- 3.5 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Crusts
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Arsenic-rich Mineral Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find švenekite
Classic worldwide localities
- Jáchymov, Czech Republic
- Wittichen, Germany
Field-hunting tip
Look in hydrothermal veins in arsenic-rich mineral deposits country — that is the host setting where švenekite typically forms. If you start seeing pharmacolite, pitticite, arsenolite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts habit, so train your eye for that shape before scanning the outcrop.




