Beudantite is a secondary mineral found in the oxidation zones of lead-bearing ore deposits. It typically forms small, sharp rhombohedral or pseudo-cubic crystals, often appearing in rich brown to yellow crusts or coatings on other host minerals.
Is this beudantite?
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 beudantite with a known reference. Beudantite sits at Mohs 3.5-4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Beudantite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Beudantite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, yellow, green, black.
- 5Look at form & habitCrystal system: trigonal. Typical habit: rhombohedral crystals, pseudocubic, tabular.
Often confused with
Beudantite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside beudantite
Minerals reported to co-occur with beudantite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbFe₃(AsO₄)(SO₄)(OH)₆
- Mohs hardness
- 3.5-4.5
- Density
- 4.1-4.3 g/cm³
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Rhombohedral Crystals, Pseudocubic, Tabular
- Cleavage
- Distinct On {0001}
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Oxidized Zones of Base Metal Hydrothermal Deposits
- Typical price
- $20-150 thumbnail specimens
Where rockhounds find beudantite
Classic worldwide localities
- Grube Stahlberg, Germany
- Tsumeb Mine, Namibia
- Broken Hill, Australia
- Black Pine Mine, USA
Field-hunting tip
Look in oxidized zones of base metal hydrothermal deposits country, the host setting where beudantite typically forms. If you start seeing mimetite, pyromorphite, anglesite in float, you are in the right ground. Field specimens usually show a rhombohedral crystals, pseudocubic, tabular habit, so train your eye for that shape before scanning the outcrop.







