Ekaterinite is a rare calcium borate halide mineral found primarily in the Korshunovskoye iron deposit in Siberia. It typically forms small, clear, tetragonal prismatic crystals in cavities within iron ore deposits.
Is this ekaterinite?
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 ekaterinite with a known reference. Ekaterinite sits at Mohs 1-1.5, 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: pearly.
- 4Match the color rangeCompare against the expected color range: pearl white, pink.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals.
Often confused with
Ekaterinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ekaterinite
Minerals reported to co-occur with ekaterinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂B₄O₇Cl₂·2H₂O
- Mohs hardness
- 1-1.5
- Density
- 2.440 g/cm³
- Colors
- Streak
- White
- Luster
- Pearly
- Transparency
- Transparent to translucent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic crystals
- Cleavage
- On {0001}, distinct, foliated
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In calcite and calcite–anhydrite veins associated with a mineralized skarn
Where rockhounds find ekaterinite
Classic worldwide localities
- From drill cores in the Korshunovskoye ironboron skarn deposit, Irkutsk district, Siberia, Russia (type locality)
Field-hunting tip
Where it forms: In calcite and calcite–anhydrite veins associated with a mineralized skarn. If you start seeing halite, calcite, szaibélyite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.







