Markcooperite is an extremely rare lead-uranium silicate mineral discovered in the Musonoi Mine. It typically forms small, yellow, translucent tabular crystals often found associated with other uranium-bearing secondary minerals in oxidation zones.
Is this markcooperite?
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 markcooperite with a known reference. Markcooperite sits at Mohs 3-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Markcooperite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Markcooperite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, aggregates.
Often confused with
Markcooperite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside markcooperite
Minerals reported to co-occur with markcooperite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₂SiUO₈
- Mohs hardness
- 3-4
- Density
- 8.8-9.0 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Aggregates
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Uranium Deposits
- Typical price
- $200-1000+ for rare micro specimens
Where rockhounds find markcooperite
Classic worldwide localities
- Musonoi Mine, Democratic Republic of the Congo
Field-hunting tip
Look in oxidized zones of uranium deposits country, the host setting where markcooperite typically forms. If you start seeing soddyite, kasolite, curite in float, you are in the right ground. Field specimens usually show a tabular crystals, aggregates habit, so train your eye for that shape before scanning the outcrop.



