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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, crusts.
Often confused with
Švenekite vs. its common look-alikes, and how to tell them apart in the field.
All properties
- Chemical formula
- Ca(H₂AsO₄)₂
- Mohs hardness
- ~2
- Density
- 3.16 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals, crusts
- Cleavage
- Very good on {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral coating granite near a polymetallic hydrothermal vein
Where rockhounds find švenekite
Classic worldwide localities
- Jáchymov, Czech Republic
- Wittichen, Germany
Field-hunting tip
Where it forms: A secondary mineral coating granite near a polymetallic hydrothermal vein. If you start seeing none given in float, you are in the right ground. Typical habit: tabular crystals, crusts. Train your eye for that shape before scanning the outcrop.

