Clairite is a very rare ammonium-bearing sulfate mineral often found in the oxidized zones of coal mine dumps. It typically appears as small, yellowish, pearly tabular crystals and is distinguished from common copiapite by its ammonium content and specific geological setting.

Hardness
2
Mohs
Luster
Pearly
Streak
Yellow
Transparency
Transparent to translucent

Is this clairite?

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 clairite with a known reference. Clairite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: yellow.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: pearly.
  • 4
    Match the color range
    Compare against the expected color range: yellow.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: tabular crystals.

Often confused with

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

Often found alongside clairite

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

All properties

Chemical formula
(NH₄)₂Fe₃(SO₄)₄(OH)₃·3H₂O
Mohs hardness
2
Density
2.31 g/cm³
Colors
Streak
Yellow
Luster
Pearly
Transparency
Transparent to translucent
Crystal system
Triclinic
Crystal habit
Tabular crystals
Cleavage
Perfect on {001}
Rarity
Rare
Uses
Collector
Host rock
A rare secondary mineral formed by alteration of pyrite to ferric sulfate, and reaction, at pH ∼2, with ammonia produced as the result of decay of organic matter (Hyrax excreta)

Where rockhounds find clairite

Classic worldwide localities

  • Lone Creek Fall cave, near Sbri, eastern Transvaal, South Africa (type locality)

Field-hunting tip

Where it forms: A rare secondary mineral formed by alteration of pyrite to ferric sulfate, and reaction, at pH ∼2, with ammonia produced as the result of decay of organic matter (Hyrax excreta). If you start seeing lonecreekite, sabieite, tschermigite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify clairite?+
Mohs hardness is 2. Luster: pearly. The streak is yellow. Common colors include yellow.
Where is clairite found?+
Notable localities include Lone Creek Fall cave, near Sbri, eastern Transvaal, South Africa (type locality).
What rocks look like clairite?+
Clairite is most often confused with Copiapite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with clairite?+
Clairite commonly co-occurs with Lonecreekite, Sabieite, Tschermigite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does clairite form in?+
Where it forms: A rare secondary mineral formed by alteration of pyrite to ferric sulfate, and reaction, at pH ∼2, with ammonia produced as the result of decay of organic matter (Hyrax excreta). Working float back to the host body is the standard way to chase a fresh occurrence.
What is clairite used for?+
Clairite is used in collector.

Find clairite on the map

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