Ferropseudobrookite is an iron-titanium oxide mineral typically found in volcanic rocks as small, well-formed prismatic crystals. It is distinguished from other iron-titanium oxides by its orthorhombic structure and its tendency to occur within basaltic or rhyolitic cavities. Collectors primarily source these from classic volcanic regions in Europe and Mexico.
Is this ferropseudobrookite?
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 ferropseudobrookite with a known reference. Ferropseudobrookite sits at Mohs 6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ferropseudobrookite leaves a brown streak.
- 3Read the lusterHold the specimen under a strong light. Ferropseudobrookite typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: black, brownish-black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic to tabular crystals.
Often confused with
Ferropseudobrookite vs. its common look-alikes — and how to tell them apart in the field.
How to tell apart: Streak differs — Ferropseudobrookite leaves brown, Manaccanite leaves black.

How to tell apart: Streak differs — Ferropseudobrookite leaves brown, Iron Ore leaves reddish-brown to black; luster reads submetallic on Ferropseudobrookite and metallic to submetallic on Iron Ore.

How to tell apart: Streak differs — Ferropseudobrookite leaves brown, Pseudobrookite leaves white; luster reads submetallic on Ferropseudobrookite and adamantine on Pseudobrookite.
Often found alongside ferropseudobrookite
Minerals reported to co-occur with ferropseudobrookite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₂TiO₅
- Mohs hardness
- 6
- Density
- 4.3-4.4 g/cm³
- Colors
- Streak
- Brown
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic to Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Volcanic Rocks, Particularly Rhyolites and Basaltic Scoria
- Typical price
- $20-150 for micro-mounts or thumbnail specimens
Where rockhounds find ferropseudobrookite
Classic worldwide localities
- Eifel Mountains, Germany
- Puy-de-Dôme, France
- Mexico
- Italy
Field-hunting tip
Look in volcanic rocks, particularly rhyolites and basaltic scoria country — that is the host setting where ferropseudobrookite typically forms. If you start seeing fayalite, magnetite, sanidine in float, you are in the right ground. Field specimens usually show a prismatic to tabular crystals habit, so train your eye for that shape before scanning the outcrop.




