Hermannroseite is a rare copper phosphate mineral often found as small, vibrant green crusts or fine tabular crystals. It is primarily identified by its distinct color and association with other secondary copper minerals in oxidized zones of ore deposits.
Is this hermannroseite?
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 hermannroseite with a known reference. Hermannroseite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: grassy-green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, radial aggregates, crusts.
Often confused with
Hermannroseite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside hermannroseite
Minerals reported to co-occur with hermannroseite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCu(PO₄)OH
- Mohs hardness
- 4
- Density
- 4.08 g/cm³
- Colors
- Grassy-green
- Streak
- Pale green
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular crystals, radial aggregates, crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral in an oxidize, polymetallic sulfide deposit
Where rockhounds find hermannroseite
Classic worldwide localities
- Tsumeb mine, Tsumeb, Namibia
Field-hunting tip
Where it forms: A secondary mineral in an oxidize, polymetallic sulfide deposit. If you start seeing conichalcite, whitlockite, pseudomalachite in float, you are in the right ground. Typical habit: tabular crystals, radial aggregates, crusts. Train your eye for that shape before scanning the outcrop.





