Scottyite is an extremely rare barium copper silicate mineral primarily known from the Wedderburn meteorite. It typically occurs as small platy crystals within the metallic matrix of iron meteorites, formed under specific meteoritic conditions.
Is this scottyite?
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 scottyite with a known reference. Scottyite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Scottyite leaves a brown streak.
- 3Read the lusterHold the specimen under a strong light. Scottyite typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: dark brown, black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals.
Often confused with
Scottyite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside scottyite
Minerals reported to co-occur with scottyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaCuSi₂O₆
- Mohs hardness
- 3-4
- Density
- 4.15 g/cm³
- Colors
- Streak
- Brown
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Iron Meteorites
- Typical price
- very high (research/museum grade only)
Where rockhounds find scottyite
Classic worldwide localities
- Wedderburn meteorite
- Victoria, Australia
Field-hunting tip
Look in iron meteorites country — that is the host setting where scottyite typically forms. If you start seeing kamacite, taenite, schreibersite in float, you are in the right ground. Field specimens usually show a platy crystals habit, so train your eye for that shape before scanning the outcrop.




