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.
Is this clairite?
5-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 clairite with a known reference. Clairite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Clairite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Clairite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, brownish-yellow.
- 5Look at form & habitCrystal 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⁺₄(SO₄)₆(OH)₂·7H₂O
- Mohs hardness
- 2.5
- Density
- 2.44 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Sulfide Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find clairite
Classic worldwide localities
- Friedrichssegen Mine, Germany
- Kladno, Czech Republic
Field-hunting tip
Look in oxidized sulfide deposits country — that is the host setting where clairite typically forms. If you start seeing jarosite, gypsum, melanterite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.




