Molybdofornacite is a rare secondary mineral found in the oxidation zones of lead-bearing ore deposits. It typically appears as bright yellow to greenish-yellow tabular crystals or thin crusts, often associated with other rare arsenates and chromates at world-class localities like Tsumeb.
Is this molybdofornacite?
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 molybdofornacite with a known reference. Molybdofornacite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Molybdofornacite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Molybdofornacite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, greenish-yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, crusts, acicular aggregates.
Often confused with
Molybdofornacite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside molybdofornacite
Minerals reported to co-occur with molybdofornacite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂Cu(CrO₄)(AsO₄)(OH)
- Mohs hardness
- 3
- Density
- 6.08 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Crusts, Acicular Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Zones in Polymetallic Deposits
- Typical price
- $50-500 depending on specimen quality
Where rockhounds find molybdofornacite
Classic worldwide localities
- Tsumeb Mine, Namibia
- Callenberg, Saxony, Germany
Field-hunting tip
Look in oxidized hydrothermal zones in polymetallic deposits country, the host setting where molybdofornacite typically forms. If you start seeing cerussite, duftite, mimetite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts, acicular aggregates habit, so train your eye for that shape before scanning the outcrop.






