Shibkovite is a rare potassium calcium zinc oxide that forms white to colorless equant grains. It occurs in coarse-grained microcline-quartz rocks in glacial moraine. It was first described from the moraine of the Dara-i-Pioz glacier, northern Tajikistan.
Is this shibkovite?
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 shibkovite with a known reference. Shibkovite sits at Mohs 5.5-6, 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: white, colorless.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: microscopic crystals.
Often confused with
Shibkovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside shibkovite
Minerals reported to co-occur with shibkovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂Ca₂(Zn₃Si₁₂)O₃₀
- Mohs hardness
- 5.5-6
- Density
- 2.89 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In coarse-grained microcline-quartz rocks in glacial moraine
Where rockhounds find shibkovite
Classic worldwide localities
- Dara-i-Pioz glacier, Garmsky District, northern Tajikistan (type locality)
Field-hunting tip
Where it forms: In coarse-grained microcline-quartz rocks in glacial moraine. If you start seeing reedmergnerite, aegirine, polylithionite in float, you are in the right ground. Typical habit: microscopic crystals. Train your eye for that shape before scanning the outcrop.








