Clinoungemachite is a rare potassium sodium iron sulfate that forms colorless to pale yellow as minute thick tabular pseudorhombohedral crystals. It was approved as a distinct mineral species in 1938. It was first described from Chuquicamata, Antofagasta, Chile.

Hardness
2.5-3
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent

Is this clinoungemachite?

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 clinoungemachite with a known reference. Clinoungemachite sits at Mohs 2.5-3, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: 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: colorless, white, light yellow.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: as minute thick tabular pseudorhombohedral crystals.

Often confused with

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

Often found alongside clinoungemachite

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

All properties

Chemical formula
K₃Na₈Fe³⁺(SO₄)₆(OH)₂·10H₂O
Mohs hardness
2.5-3
Density
6.8-7.2 g/cm³
Streak
White
Luster
Vitreous
Transparency
Transparent
Crystal system
Monoclinic
Crystal habit
As minute thick tabular pseudorhombohedral crystals
Cleavage
Perfect
Rarity
Rare
Uses
Collector
Host rock
Very rarely formed by the oxidation of pyrite in an arid climate, in veins and cavities in other massive iron sulfates

Where rockhounds find clinoungemachite

Classic worldwide localities

  • Chuquicamata, Antofagasta, Chile

Field-hunting tip

Where it forms: Very rarely formed by the oxidation of pyrite in an arid climate, in veins and cavities in other massive iron sulfates. If you start seeing ungemachite, jarosite, sideronatrite in float, you are in the right ground. Typical habit: as minute thick tabular pseudorhombohedral crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify clinoungemachite?+
Mohs hardness is 2.5-3. Luster: vitreous. The streak is white. Common colors include colorless, white, light yellow.
Where is clinoungemachite found?+
Notable localities include Chuquicamata, Antofagasta, Chile.
What rocks look like clinoungemachite?+
Clinoungemachite is most often confused with Ungemachite, Bottinoite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with clinoungemachite?+
Clinoungemachite commonly co-occurs with Ungemachite, Jarosite, Sideronatrite, Metasideronatrite, Metavoltine, Fibroferrite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does clinoungemachite form in?+
Where it forms: Very rarely formed by the oxidation of pyrite in an arid climate, in veins and cavities in other massive iron sulfates. Working float back to the host body is the standard way to chase a fresh occurrence.
What is clinoungemachite used for?+
Clinoungemachite is used in collector.

Find clinoungemachite on the map

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