Rusinovite is an extremely rare calcium silicate chloride mineral discovered in the Chegem volcanic caldera in Russia. It typically occurs as small tabular crystals within high-temperature skarn environments associated with carbonate-rich volcanic xenoliths.
Is this rusinovite?
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 rusinovite with a known reference. Rusinovite sits at Mohs 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: white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals.
Often confused with
Rusinovite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside rusinovite
Minerals reported to co-occur with rusinovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₁₀(Si₂O₇)₃Cl₂
- Mohs hardness
- 4-5
- Density
- 2.93 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous to silky
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular crystals
- Cleavage
- Good on (010)
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a thermally altered (sanidinite facies) carbonate-silicate xenolith about 10 m in size enclosed in ignimbrite
Where rockhounds find rusinovite
Classic worldwide localities
- Upper Chegem caldera, near Mt. Lakargi, Kabardino-Balkaria, Northern Caucasus, Russia
Field-hunting tip
Where it forms: In a thermally altered (sanidinite facies) carbonate-silicate xenolith about 10 m in size enclosed in ignimbrite. If you start seeing wadalite, wollastonite, trabzonite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.


