Edwardsite is a rare copper cadmium sulfate that forms pale blue tabular to bladed crystals. It is a secondary mineral in the oxidized portion of a Ag-Pb-Zn metal deposit. It is associated with niedermayrite and christelite. It was first described from Block 14 Opencut, Broken Hill, New South Wales, Australia.
Is this edwardsite?
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 edwardsite with a known reference. Edwardsite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Edwardsite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Edwardsite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pale blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular to bladed crystals.
Often confused with
Edwardsite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside edwardsite
Minerals reported to co-occur with edwardsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃Cd₂(SO₄)₂(OH)₆·4H₂O
- Mohs hardness
- 3-3.5
- Density
- 3.53 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular to Bladed Crystals
- Cleavage
- Excellent On {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
Where rockhounds find edwardsite
Classic worldwide localities
- Block 14 Opencut, New South Wales, Australia
Field-hunting tip
Look in hydrothermal veins country, the host setting where edwardsite typically forms. If you start seeing monazite, cerite in float, you are in the right ground. Field specimens usually show a tabular to bladed crystals habit, so train your eye for that shape before scanning the outcrop.

