Niksergievite is a rare phyllosilicate mineral belonging to the clintonite group, typically found as small, pearly-lustered lamellar crystals or scaly masses. It is primarily known from the Khaidarkan mercury-antimony deposit in Kyrgyzstan where it forms as a rare alteration product. Collectors should look for its characteristic mica-like habit and association with fluorite in hydrothermal vein environments.
Is this niksergievite?
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 niksergievite with a known reference. Niksergievite sits at Mohs 3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Niksergievite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Niksergievite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: lamellar crystals, scaly aggregates.
Often confused with
Niksergievite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside niksergievite
Minerals reported to co-occur with niksergievite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (□,Ca,Na)₂(Al,Mg,Fe)₃(Al,Si)₄O₁₀(OH)₂
- Mohs hardness
- 3.5
- Density
- 3.08 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Lamellar Crystals, Scaly Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Vein Deposits in Sedimentary Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find niksergievite
Classic worldwide localities
- Khaidarkan, Kyrgyzstan
Field-hunting tip
Look in hydrothermal vein deposits in sedimentary rocks country, the host setting where niksergievite typically forms. If you start seeing fluorite, quartz, calcite in float, you are in the right ground. Field specimens usually show a lamellar crystals, scaly aggregates habit, so train your eye for that shape before scanning the outcrop.







