Khanneshite is a rare carbonate mineral discovered in the Khanneshin carbonatite complex of Afghanistan. It typically forms as prismatic to acicular crystals and is primarily sought after by advanced mineral collectors specializing in rare carbonatite species.
Is this khanneshite?
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 khanneshite with a known reference. Khanneshite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: light yellow.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals.
Often confused with
Khanneshite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside khanneshite
Minerals reported to co-occur with khanneshite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ca)₃(Ba,Sr,Ce,Ca)₃(CO₃)₅
- Mohs hardness
- 3-4
- Density
- 3.8-3.9 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic crystals
- Cleavage
- One, parallel elongation, indistinct; and a transverse parting
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Disseminated in hydrothermally-altered fine-grained carbonatite (Khanneshin complex, Afghanistan); in a drillcore in a carbonatite veinlet from a differentiated alkalic massif (Khibiny massif, Kola Peninsula, Russia)
Where rockhounds find khanneshite
Classic worldwide localities
- Khanneshin carbonatite complex, Afghanistan
- Tuliylukht Bay, Khibiny massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: Disseminated in hydrothermally-altered fine-grained carbonatite (Khanneshin complex, Afghanistan); in a drillcore in a carbonatite veinlet from a differentiated alkalic massif (Khibiny massif, Kola Peninsula, Russia). If you start seeing dolomite, calkinsite-, carbocernaite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.






