Nikmelnikovite is a rare titanium-rich member of the garnet group, specifically a silicate with iron and titanium. It is typically found in alkaline igneous complexes as dark, sub-metallic to vitreous crystals associated with other titanium-bearing minerals.
Is this nikmelnikovite?
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 nikmelnikovite with a known reference. Nikmelnikovite sits at Mohs 6.5-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Nikmelnikovite leaves a brownish streak.
- 3Read the lusterHold the specimen under a strong light. Nikmelnikovite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark brown, black.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral crystals.
Often confused with
Nikmelnikovite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside nikmelnikovite
Minerals reported to co-occur with nikmelnikovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Fe₂Si₃O₁₂
- Mohs hardness
- 6.5-7
- Density
- 3.8-3.9 g/cm³
- Colors
- Streak
- Brownish
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Alkaline Igneous Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find nikmelnikovite
Classic worldwide localities
- Kola Peninsula, Russia
Field-hunting tip
Look in alkaline igneous rocks country — that is the host setting where nikmelnikovite typically forms. If you start seeing aegirine, nepheline, titanite in float, you are in the right ground. Field specimens usually show a dodecahedral crystals habit, so train your eye for that shape before scanning the outcrop.





