Birchite is a very rare secondary cadmium copper sulfate mineral found in oxidized base metal deposits. It typically occurs as tiny, thin tabular crystals associated with lead and copper minerals in arid climates. Due to its scarcity and delicate nature, it is primarily sought after by advanced systematic mineral collectors.
Is this birchite?
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 birchite with a known reference. Birchite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Birchite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Birchite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, subparallel aggregates.
Often confused with
Birchite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside birchite
Minerals reported to co-occur with birchite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cd₂Cu₂(SO₄)(OH)₄
- Mohs hardness
- 3.5
- Density
- 3.16 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Subparallel Aggregates
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Lead-zinc-copper Deposits
- Typical price
- $100-500 thumbnail
Where rockhounds find birchite
Classic worldwide localities
- Red Cloud Mine, Arizona, USA
Field-hunting tip
Look in oxidized hydrothermal lead-zinc-copper deposits country — that is the host setting where birchite typically forms. If you start seeing cerussite, anglesite, wulfenite in float, you are in the right ground. Field specimens usually show a tabular crystals, subparallel aggregates habit, so train your eye for that shape before scanning the outcrop.






