Richelsdorfite is a rare copper-calcium-antimony arsenate mineral that forms as a secondary product in the oxidation zones of copper deposits. It is best identified by its vibrant blue to bluish-green bladed or radial crystal clusters typically found in small vugs.
Is this richelsdorfite?
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 richelsdorfite with a known reference. Richelsdorfite 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. Richelsdorfite leaves a pale blue streak.
- 3Read the lusterHold the specimen under a strong light. Richelsdorfite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: bladed crystals, radial aggregates, crusts.
Often confused with
Richelsdorfite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside richelsdorfite
Minerals reported to co-occur with richelsdorfite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Cu₅Sb(AsO₄)₄(OH)₆·6H₂O
- Mohs hardness
- 2
- Density
- 3.5 g/cm³
- Streak
- Pale Blue
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Bladed Crystals, Radial Aggregates, Crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Copper-bearing Ore Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find richelsdorfite
Classic worldwide localities
- Richelsdorf, Germany
- Cap Garonne, France
- Schwarzwald, Germany
Field-hunting tip
Look in oxidized copper-bearing ore deposits country — that is the host setting where richelsdorfite typically forms. If you start seeing azurite, malachite, baryte in float, you are in the right ground. Field specimens usually show a bladed crystals, radial aggregates, crusts habit, so train your eye for that shape before scanning the outcrop.






