Erikapohlite is a rare copper-zinc arsenate mineral primarily found in the Tsumeb mine in Namibia. It typically occurs as small, deep blue platy crystals or crusts associated with other secondary arsenate minerals in oxidized ore zones.
Is this erikapohlite?
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 erikapohlite with a known reference. Erikapohlite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale blue.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: deep blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts.
Often confused with
Erikapohlite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside erikapohlite
Minerals reported to co-occur with erikapohlite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (□₀.₅Cu₀.₅)CuCaZn₂(AsO₄)₃·H₂O
- Mohs hardness
- 3-4
- Density
- 4.55 g/cm³
- Colors
- Streak
- Pale blue
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, crusts
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral formed by weathering tennantite-rich veins in the oxidized zone of a dolostone-hosted, hydrothermal polymetallic deposit
Where rockhounds find erikapohlite
Classic worldwide localities
- Tsumeb Mine, Namibia
Field-hunting tip
Where it forms: A secondary mineral formed by weathering tennantite-rich veins in the oxidized zone of a dolostone-hosted, hydrothermal polymetallic deposit. If you start seeing lammerite, conichalcite, quartz in float, you are in the right ground. Typical habit: platy crystals, crusts. Train your eye for that shape before scanning the outcrop.




