Koktaite is a rare sulfate mineral that typically forms as white to colorless efflorescences or small, thin tabular crystals in self-burning coal mine waste heaps. It is chemically related to syngenite but contains ammonium as a major cation, making it a distinct phase often found in ephemeral environments. Due to its solubility, it is best kept in a dry environment and protected from high humidity.
Is this koktaite?
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 koktaite with a known reference. Koktaite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Koktaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Koktaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, crusts, efflorescences.
Often confused with
Koktaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside koktaite
Minerals reported to co-occur with koktaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (NH₄)₂Ca(SO₄)₂·H₂O
- Mohs hardness
- 2
- Density
- 1.74 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Crusts, Efflorescences
- Cleavage
- Distinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Burning Coal Mine Dumps, Guano Deposits
- Typical price
- $20-100 per specimen
Where rockhounds find koktaite
Classic worldwide localities
- Koktavskoe coal mine, Czech Republic
- various guano deposits
- burning coal waste heaps
Field-hunting tip
Look in burning coal mine dumps, guano deposits country — that is the host setting where koktaite typically forms. If you start seeing gypsum, syngenite, arcanite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts, efflorescences habit, so train your eye for that shape before scanning the outcrop.



