Drysdallite is a rare molybdenum selenide mineral that looks very similar to molybdenite but typically occurs in distinct selenium-rich environments. It is characterized by its soft, flexible, and sectile nature, often forming platy or foliated aggregates that can be easily mistaken for graphite or molybdenite without chemical analysis.
Is this drysdallite?
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 drysdallite with a known reference. Drysdallite sits at Mohs 1-1.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: brownish black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: grayish black.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: foliated, platy, lamellar aggregates.
Often confused with
Drysdallite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside drysdallite
Minerals reported to co-occur with drysdallite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MoSe₂
- Mohs hardness
- 1-1.5
- Density
- 6.25 g/cm³
- Colors
- Streak
- Brownish black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Foliated, platy, lamellar aggregates
- Cleavage
- {0001}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxidation zone of a uranium deposit in a talc schist
Where rockhounds find drysdallite
Classic worldwide localities
- Kapijimpanga uranium deposit, 16 km southeast of Solwezi, Northwestern Province, Zambia (type locality)
Field-hunting tip
Where it forms: In the oxidation zone of a uranium deposit in a talc schist. If you start seeing uraninite, apatite, masuyite in float, you are in the right ground. Typical habit: foliated, platy, lamellar aggregates. Train your eye for that shape before scanning the outcrop.





