Tomichite is a very rare titanium-vanadium-arsenic mineral found primarily in specific metasomatized ultramafic rocks in Western Australia. It typically occurs as small, dark, platy crystals that resemble ilmenite or hematite, often requiring X-ray diffraction for definitive identification in the field.
Is this tomichite?
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 tomichite with a known reference. Tomichite 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. Tomichite leaves a brown streak.
- 3Read the lusterHold the specimen under a strong light. Tomichite typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: dark brown, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, granular aggregates.
Often confused with
Tomichite vs. its common look-alikes, and how to tell them apart in the field.
How to tell apart: Streak differs, so Tomichite leaves brown, Manaccanite leaves black.

How to tell apart: Streak differs, so Tomichite leaves brown, Iron Ore leaves reddish-brown to black; luster reads submetallic on Tomichite and metallic to submetallic on Iron Ore.
Often found alongside tomichite
Minerals reported to co-occur with tomichite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ti₄V₃AsO₁₃(OH)₆
- Mohs hardness
- 5-6
- Density
- 4.8-5.0 g/cm³
- Colors
- Streak
- Brown
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Granular Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metasomatized Ultramafic Rocks
- Typical price
- $50-300 per small specimen
Where rockhounds find tomichite
Classic worldwide localities
- Mount Tomich, Australia
Field-hunting tip
Look in metasomatized ultramafic rocks country, the host setting where tomichite typically forms. If you start seeing ilmenite, hematite, quartz in float, you are in the right ground. Field specimens usually show a platy crystals, granular aggregates habit, so train your eye for that shape before scanning the outcrop.


