Kasatkinite is an extremely rare barium-calcium borosilicate mineral found in alkaline igneous complexes. It typically presents as colorless to white platy crystals or radiating sprays within quartz-rich matrices.
Is this kasatkinite?
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 kasatkinite with a known reference. Kasatkinite sits at Mohs 4-4.5, 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 to silky.
- 4Match the color rangeCompare against the expected color range: colorless, snow-white aggregates.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, radiating aggregates.
Often confused with
Kasatkinite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Stillwellite-(Ce) is the harder of the two (Mohs ~6.5 vs. 4-4.5); luster reads vitreous to silky on Kasatkinite and resinous on Stillwellite-(Ce).

How to tell apart: Barylite is the harder of the two (Mohs 7 vs. 4-4.5).
Often found alongside kasatkinite
Minerals reported to co-occur with kasatkinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ba₂Ca₈B₅Si₈O₃₂(OH)₃·6H₂O
- Mohs hardness
- 4-4.5
- Density
- 2.95 g/cm³
- Colors
- ColorlessSnow-white aggregates
- Streak
- White
- Luster
- Vitreous to silky
- Transparency
- Translucent to nearly opaque
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, radiating aggregates
- Cleavage
- None observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Of hydrothermal origin in cavities in rhodingite
Where rockhounds find kasatkinite
Classic worldwide localities
- Bazhenovskoe chrysotile-asbestos deposit (eastern part of the open pit Yuzhnyi), near Asbest, Middle Urals, Russia
Field-hunting tip
Where it forms: Of hydrothermal origin in cavities in rhodingite. If you start seeing prehnite, pectolite, calcite in float, you are in the right ground. Typical habit: platy crystals, radiating aggregates. Train your eye for that shape before scanning the outcrop.






