Tondiite is a rare copper magnesium chloride hydroxide mineral found in the oxidation zones of copper-bearing deposits. It typically forms as small, dark green platy crystals or granular masses that can easily be mistaken for other members of the atacamite group.
Is this tondiite?
4-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 tondiite with a known reference. Tondiite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: emerald green, bright green.
- 4Look at form & habitCrystal system: trigonal. Typical habit: platy crystals, granular aggregates.
Often confused with
Tondiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tondiite
Minerals reported to co-occur with tondiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃Mg(OH)₆Cl₂
- Mohs hardness
- 3-3.5
- Density
- 3.503 g/cm³
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Platy crystals, granular aggregates
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral in vesicles in phonolitic tephrite (Vesuvius); a secondary oxidation product of chalcocite, bornite and chalcopyrite in an environment rich in Cl in andesitic porphyric lavas and lava tuff (Chile)
Where rockhounds find tondiite
Classic worldwide localities
- Vesuvius volcano, Italy, and from the Santo Domingo Cu Mine, Caleta Vitor district, Arica Province, Chile
Field-hunting tip
Where it forms: A secondary mineral in vesicles in phonolitic tephrite (Vesuvius); a secondary oxidation product of chalcocite, bornite and chalcopyrite in an environment rich in Cl in andesitic porphyric lavas and lava tuff (Chile). If you start seeing leucite, sodalite, nepheline in float, you are in the right ground. Typical habit: platy crystals, granular aggregates. Train your eye for that shape before scanning the outcrop.









