Graeserite is an exceptionally rare arsenic-iron-titanium oxide mineral known primarily from the Binntal region of Switzerland. It typically appears as tiny, black, tabular crystals embedded within mineral-rich pockets of metamorphic dolomitic marble. Due to its scarcity and complex chemistry, it is a highly sought-after prize for advanced mineralogists and systematic collectors.
Is this graeserite?
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 graeserite with a known reference. Graeserite sits at Mohs 5.5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Graeserite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Graeserite typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals.
Often confused with
Graeserite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside graeserite
Minerals reported to co-occur with graeserite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₄Ti₃As₄O₁₉
- Mohs hardness
- 5.5-6
- Density
- 4.95 g/cm³
- Colors
- Streak
- Black
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Dolomitic Marble in Hydrothermal Veins
- Typical price
- $200-1000+ for micro-specimens
Where rockhounds find graeserite
Classic worldwide localities
- Binntal, Valais, Switzerland
Field-hunting tip
Look in dolomitic marble in hydrothermal veins country — that is the host setting where graeserite typically forms. If you start seeing lengenbachite, realgar, sartorite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.





