Ramsbeckite is a rare copper-zinc sulfate mineral typically found as small, bright green tabular crystals or crusts. It primarily forms in the oxidized zones of base metal deposits, often associated with other secondary copper minerals.
Is this ramsbeckite?
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 ramsbeckite with a known reference. Ramsbeckite 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. Ramsbeckite leaves a light green streak.
- 3Read the lusterHold the specimen under a strong light. Ramsbeckite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: bright green, dark green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, radiating aggregates, crusts.
Often confused with
Ramsbeckite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside ramsbeckite
Minerals reported to co-occur with ramsbeckite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Cu,Zn)₁₅(SO₄)₄(OH)₂₂·6H₂O
- Mohs hardness
- 3
- Density
- 3.51 g/cm³
- Colors
- Streak
- Light Green
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Radiating Aggregates, Crusts
- Cleavage
- Perfect On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Copper-zinc Sulfide Deposits
- Typical price
- $20-200 depending on specimen size and quality
Where rockhounds find ramsbeckite
Classic worldwide localities
- Ramsbeck, Germany
- Laurion, Greece
- Broken Hill, Australia
- Tsumeb, Namibia
Field-hunting tip
Look in oxidized zones of copper-zinc sulfide deposits country — that is the host setting where ramsbeckite typically forms. If you start seeing sphalerite, galena, linarite in float, you are in the right ground. Field specimens usually show a tabular crystals, radiating aggregates, crusts habit, so train your eye for that shape before scanning the outcrop.








