Katerinopoulosite is an extremely rare ammonium-iron sulfate mineral found primarily in the historic mine dumps of the Lavrion District in Greece. It typically forms as delicate, white, acicular crystal sprays or coatings associated with other secondary sulfate minerals in oxidized hydrothermal deposits.
Is this katerinopoulosite?
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 katerinopoulosite with a known reference. Katerinopoulosite sits at Mohs 2.5, 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: colorless, pale blue, or pale green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular to fibrous aggregates.
Often confused with
Katerinopoulosite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside katerinopoulosite
Minerals reported to co-occur with katerinopoulosite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (NH₄)₂Zn(SO₄)₂·6H₂O
- Mohs hardness
- 2.5
- Density
- 1.97 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular to fibrous aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral formed in the oxidation zone of a sphalerite-rich deposit situated in the contact zone between calcite marble and mica schist
Where rockhounds find katerinopoulosite
Classic worldwide localities
- Esperanza mine, Lavrion District, Attikí Prefecture, Greece
Field-hunting tip
Where it forms: A secondary mineral formed in the oxidation zone of a sphalerite-rich deposit situated in the contact zone between calcite marble and mica schist. If you start seeing chalcanthite, nickelboussingaultite, ammoniojarosite in float, you are in the right ground. Typical habit: acicular to fibrous aggregates. Train your eye for that shape before scanning the outcrop.







