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 — that is 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.






