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 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: pale blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: aggregates, prismatic.
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(PO₄)₂SO₄·5H₂O
- Mohs hardness
- 3.5-4
- Density
- 3.61 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Aggregates, prismatic
- Cleavage
- None observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Late-stage supergene mineral formed as part of a suite of secondary phosphate minerals under low-temperature conditions
Where rockhounds find birchite
Classic worldwide localities
- Block 14 Opencut, Broken Hill, New South Wales, Australia
Field-hunting tip
Where it forms: Late-stage supergene mineral formed as part of a suite of secondary phosphate minerals under low-temperature conditions. If you start seeing hinsdalite-plumbogummite, cerussite, anglesite in float, you are in the right ground. Typical habit: aggregates, prismatic. Train your eye for that shape before scanning the outcrop.







