Cuprokalininite is a rare copper-chromium sulfide belonging to the spinel group. It typically appears as opaque, metallic black octahedral crystals found in association with hydrothermal sulfide ore bodies.
Is this cuprokalininite?
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 cuprokalininite with a known reference. Cuprokalininite sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Cuprokalininite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Cuprokalininite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: cubic. Typical habit: octahedral crystals, massive.
Often confused with
Cuprokalininite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside cuprokalininite
Minerals reported to co-occur with cuprokalininite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuCr₂S₄
- Mohs hardness
- 5-6
- Density
- 4.9-5.1 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Octahedral Crystals, Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Sulfide Deposits
- Typical price
- $50-300 per specimen depending on size and provenance
Where rockhounds find cuprokalininite
Classic worldwide localities
- Kalinina deposit, Russia
Field-hunting tip
Look in hydrothermal sulfide deposits country — that is the host setting where cuprokalininite typically forms. If you start seeing galena, pyrite, chalcopyrite in float, you are in the right ground. Field specimens usually show a octahedral crystals, massive habit, so train your eye for that shape before scanning the outcrop.





