Dussertite is a rare barium-iron arsenate mineral that typically forms as small, tabular, hexagonal crystals or distinct crusts in oxidized mineral deposits. Collectors usually find it as a secondary mineral in the weathered zones of arsenic-rich ore bodies, often associated with other iron-bearing sulfates and arsenates.
Is this dussertite?
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 dussertite with a known reference. Dussertite sits at Mohs 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Dussertite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Dussertite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-green, brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, crusts, botryoidal.
Often confused with
Dussertite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside dussertite
Minerals reported to co-occur with dussertite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaFe₃(AsO₄)(OH)₆
- Mohs hardness
- 3.5-4
- Density
- 4.2 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Crusts, Botryoidal
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Ore Deposits
- Typical price
- $20-150 for micro-mounts and thumbnails
Where rockhounds find dussertite
Classic worldwide localities
- Dussert mine, Algeria
- Laurion, Greece
- Ojuela Mine, Mexico
- Tsumeb, Namibia
Field-hunting tip
Look in oxidized hydrothermal ore deposits country, the host setting where dussertite typically forms. If you start seeing goethite, hematite, jarosite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts, botryoidal habit, so train your eye for that shape before scanning the outcrop.





