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, 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.





