Aldridgeite is a rare secondary zinc copper sulfate mineral often found as small, delicate, pale blue crystalline crusts in oxidized mine workings. It is primarily known from the Broken Hill ore body and requires careful handling due to its solubility and fragile nature. It is typically sought after by advanced systematic mineral collectors who specialize in rare sulfates.
Is this aldridgeite?
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 aldridgeite with a known reference. Aldridgeite sits at Mohs ~3, 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: pale blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts.
Often confused with
Aldridgeite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Aldridgeite leaves pale blue, Goslarite leaves white.

How to tell apart: Aldridgeite is noticeably harder (Mohs ~3 vs. 2); streak differs, so Aldridgeite leaves pale blue, Melanterite leaves white.
Often found alongside aldridgeite
Minerals reported to co-occur with aldridgeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CdCu₄(SO₄)₂(OH)₆(H₂O)₃
- Mohs hardness
- ~3
- Density
- 3.25 g/cm³
- Colors
- Streak
- Pale blue
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, crusts
- Cleavage
- Perfect on {100} (by analogy to serpierite)
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Secondary mineral in the oxidation zone of a galena, Cd-bearing sphalerite, and chalcopyrite deposit
Where rockhounds find aldridgeite
Classic worldwide localities
- Kintore and Block 14 open cuts, Broken Hill, New South Wales, Australia
Field-hunting tip
Where it forms: Secondary mineral in the oxidation zone of a galena, Cd-bearing sphalerite, and chalcopyrite deposit. If you start seeing neidermayrite, pyromorphite in float, you are in the right ground. Typical habit: platy crystals, crusts. Train your eye for that shape before scanning the outcrop.

