Rappoldite is a rare lead cobalt arsenate, typically red to red-brown. It is a secondary mineral. It was first described from Rappold mine, near Schneeberg, Saxony, Germany.
Is this rappoldite?
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 rappoldite with a known reference. Rappoldite sits at Mohs 4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Rappoldite leaves a light yellow-brown streak.
- 3Read the lusterHold the specimen under a strong light. Rappoldite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: red, red-brown.
- 5Look at form & habitCrystal system: triclinic. Typical habit: drusy aggregates.
Often confused with
Rappoldite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside rappoldite
Minerals reported to co-occur with rappoldite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbCo₂(AsO₄)₂·2H₂O
- Mohs hardness
- 4.5
- Density
- 5.28 g/cm³
- Streak
- Light Yellow-brown
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Drusy Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Metamorphic Rocks
Where rockhounds find rappoldite
Classic worldwide localities
- Rappold, Germany
Field-hunting tip
Look in hydrothermal veins in metamorphic rocks country, the host setting where rappoldite typically forms. If you start seeing arsenopyrite, pharmacolite, picropharmacolite in float, you are in the right ground. Field specimens usually show a drusy aggregates habit, so train your eye for that shape before scanning the outcrop.




