Ktenasite is a rare secondary copper-zinc sulfate mineral typically found as vibrant blue to blue-green platy crystals or thin crusts. It is most famous from the ancient mining district of Laurion, Greece, where it forms in the oxidation zones of ore bodies alongside other copper-zinc minerals.
Is this ktenasite?
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 ktenasite with a known reference. Ktenasite 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. Ktenasite leaves a pale blue streak.
- 3Read the lusterHold the specimen under a strong light. Ktenasite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: bright blue, blue-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts, radial aggregates.
Often confused with
Ktenasite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ktenasite
Minerals reported to co-occur with ktenasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Cu,Zn)₅(SO₄)₂(OH)₆·6H₂O
- Mohs hardness
- 2
- Density
- 3.17 g/cm³
- Colors
- Streak
- Pale Blue
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Crusts, Radial Aggregates
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Copper-zinc Deposits
- Typical price
- $20-150 for micro-mounts and small specimens
Where rockhounds find ktenasite
Classic worldwide localities
- Kamariza mines, Laurion, Greece
- Broken Hill, New South Wales, Australia
- Kallmünz, Bavaria, Germany
- Tsumeb, Namibia
Field-hunting tip
Look in oxidized zones of copper-zinc deposits country — that is the host setting where ktenasite typically forms. If you start seeing smithsonite, hemimorphite, brochantite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, radial aggregates habit, so train your eye for that shape before scanning the outcrop.






