Gordaite is a rare secondary mineral typically found as delicate, pearly-white to pale-blue tabular crystals or micaceous aggregates. It is most notable for forming in the oxidation zones of zinc-rich base metal deposits, where it is often associated with other rare secondary copper and zinc species.
Is this gordaite?
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 gordaite with a known reference. Gordaite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Gordaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Gordaite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale blue, pale green.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, rosette-like aggregates, micaceous flakes.
Often confused with
Gordaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside gordaite
Minerals reported to co-occur with gordaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaZn₄(SO₄)(OH)₆·6H₂O
- Mohs hardness
- 2
- Density
- 3.31 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Rosette-like Aggregates, Micaceous Flakes
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Ore Deposits
- Typical price
- $20-150 for micro-mounts and small cabinet specimens
Where rockhounds find gordaite
Classic worldwide localities
- Sierra Gorda, Chile
- Broken Hill, Australia
- Tsumeb, Namibia
Field-hunting tip
Look in oxidized hydrothermal ore deposits country, the host setting where gordaite typically forms. If you start seeing parnauite, cuprite, jarosite in float, you are in the right ground. Field specimens usually show a tabular crystals, rosette-like aggregates, micaceous flakes habit, so train your eye for that shape before scanning the outcrop.






