Schreyerite is an extremely rare vanadium-titanium oxide mineral typically found as small, black, opaque grains within metamorphic gneisses. It was first described from the Mutuca mine in Kenya and remains a highly sought-after specimen for advanced mineral collectors due to its unique vanadium chemistry.
Is this schreyerite?
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 schreyerite with a known reference. Schreyerite sits at Mohs 6-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Schreyerite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Schreyerite typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: black, brownish-black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, massive, granular aggregates.
Often confused with
Schreyerite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside schreyerite
Minerals reported to co-occur with schreyerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- V₂Ti₃O₉
- Mohs hardness
- 6-7
- Density
- 4.8-4.9 g/cm³
- Colors
- Streak
- Black
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Massive, Granular Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Metamorphic Rocks, Specifically Vanadium-rich Graphite Gneisses
- Typical price
- $50-300+ per specimen
Where rockhounds find schreyerite
Classic worldwide localities
- Kenya
- Russia
- Czech Republic
Field-hunting tip
Look in metamorphic rocks, specifically vanadium-rich graphite gneisses country — that is the host setting where schreyerite typically forms. If you start seeing karelianite, rutile, vesuvianite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular aggregates habit, so train your eye for that shape before scanning the outcrop.





