Kaliochalcite is a rare, secondary sulfate mineral found in the oxidation zones of copper deposits. It typically forms as vibrant yellow-green or emerald-green crystalline crusts or small, distinct tabular crystals often mistaken for more common copper sulfates.

Hardness
4
Mohs
Luster
Vitreous
Streak
Pale green to white
Transparency
Transparent to translucent

Is this kaliochalcite?

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 kaliochalcite with a known reference. Kaliochalcite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: pale green to white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: bright grass-green.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: tabular crystals, drusy coatings, micro-crystalline crusts.

Often confused with

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

Often found alongside kaliochalcite

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

All properties

Chemical formula
KCu₂(SO₄)₂[(OH)(H₂O)]
Mohs hardness
4
Density
3.49 g/cm³
Colors
Bright grass-green
Streak
Pale green to white
Luster
Vitreous
Transparency
Transparent to translucent
Crystal system
Monoclinic
Crystal habit
Tabular crystals, drusy coatings, micro-crystalline crusts
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
Through the reaction of high-temperature, sublimate K-Cu-sulfates and atmospheric water vapor at temperatures <100-150 °C, in volcanic fumaroles

Where rockhounds find kaliochalcite

Classic worldwide localities

  • Yadovitaya and Arsenatnaya fumaroles, Second scoria cone, Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia

Field-hunting tip

Where it forms: Through the reaction of high-temperature, sublimate K-Cu-sulfates and atmospheric water vapor at temperatures <100-150 °C, in volcanic fumaroles. If you start seeing hematite, tenorite, langbeinite in float, you are in the right ground. Typical habit: tabular crystals, drusy coatings, micro-crystalline crusts. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify kaliochalcite?+
Mohs hardness is 4. Luster: vitreous. The streak is pale green to white. Common colors include bright grass-green.
Where is kaliochalcite found?+
Notable localities include Yadovitaya and Arsenatnaya fumaroles, Second scoria cone, Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia.
Is kaliochalcite safe to handle?+
Kaliochalcite contains copper. Contains copper; wash hands thoroughly after handling and avoid inhaling dust during preparation or cleaning.
What rocks look like kaliochalcite?+
Kaliochalcite is most often confused with Brochantite, Antlerite, Langite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with kaliochalcite?+
Kaliochalcite commonly co-occurs with Hematite, Tenorite, Langbeinite, Aphthitalite, Steklite, Lammerite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does kaliochalcite form in?+
Where it forms: Through the reaction of high-temperature, sublimate K-Cu-sulfates and atmospheric water vapor at temperatures <100-150 °C, in volcanic fumaroles. Working float back to the host body is the standard way to chase a fresh occurrence.
What is kaliochalcite used for?+
Kaliochalcite is used in collector.

Find kaliochalcite on the map

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