Clinoatacamite is a monoclinic polymorph of the copper oxychloride Cu₂(OH)₃Cl. It is typically found in the oxidized zones of copper deposits, often appearing as distinct green, tabular crystals or crusts that are visually indistinguishable from other members of the atacamite group without laboratory analysis.

Hardness
3
Mohs
Luster
Adamantine to vitreous
Streak
Greenish white
Transparency
Transparent to translucent

Is this clinoatacamite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch clinoatacamite with a known reference. Clinoatacamite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: greenish white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: adamantine to vitreous.
  • 4
    Match the color range
    Compare against the expected color range: green, dark greenish black, greenish blue.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: crystalline.

Often confused with

Clinoatacamite vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside clinoatacamite

Minerals reported to co-occur with clinoatacamite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
Cu₂(OH)₃Cl
Mohs hardness
3
Density
3.71 g/cm³
Colors
GreenDark greenish blackGreenish blue
Streak
Greenish white
Luster
Adamantine to vitreous
Transparency
Transparent to translucent
Crystal system
Monoclinic
Crystal habit
Crystalline
Cleavage
Perfect on {012}
Rarity
Uncommon
Uses
Collector, Scientific research
Host rock
An oxidation product of other copper minerals

Where rockhounds find clinoatacamite

Classic worldwide localities

  • Calumet, Keweenaw Co., Michigan, and Mason Pass, near Yerington, Lyon Co., Nevada, USA
  • Chuquicamata, and in the Sierra Gorda district, southwest of Calama, Antofagasta, Chile
  • Remolinos, Atacama, Chile
  • Wallaces Gully, Mount Painter, and Wallaroo, South Australia
  • Castletown mine, Lochgilphead, Scotland

Field-hunting tip

Where it forms: An oxidation product of other copper minerals. If you start seeing atacamite, paratacamite, gypsum in float, you are in the right ground. Typical habit: crystalline. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify clinoatacamite?+
Mohs hardness is 3. Luster: adamantine to vitreous. The streak is greenish white. Common colors include green, dark greenish black, greenish blue.
Where is clinoatacamite found?+
Notable localities include Calumet, Keweenaw Co., Michigan, and Mason Pass, near Yerington, Lyon Co., Nevada, USA; Chuquicamata, and in the Sierra Gorda district, southwest of Calama, Antofagasta, Chile; Remolinos, Atacama, Chile; Wallaces Gully, Mount Painter, and Wallaroo, South Australia; Castletown mine, Lochgilphead, Scotland.
Is clinoatacamite safe to handle?+
Clinoatacamite contains copper. Contains copper and chlorine. Wash hands after handling to avoid ingestion or skin irritation; keep away from food and children.
What rocks look like clinoatacamite?+
Clinoatacamite is most often confused with Atacamite, Paratacamite, Botallackite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with clinoatacamite?+
Clinoatacamite commonly co-occurs with Atacamite, Paratacamite, Gypsum, Alunite, Zincian paratacamite, Caracolite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does clinoatacamite form in?+
Where it forms: An oxidation product of other copper minerals. Working float back to the host body is the standard way to chase a fresh occurrence.
What is clinoatacamite used for?+
Clinoatacamite is used in collector, scientific research.

Find clinoatacamite on the map

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