Skippenite is a rare bismuth selenide telluride that typically occurs as metallic, lead-gray foliated or platy masses. It is primarily found in hydrothermal vein systems and is often associated with native gold and other telluride minerals. Due to its extreme rarity and soft nature, it is highly prized by advanced mineral collectors specializing in bismuth species.
Is this skippenite?
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 skippenite with a known reference. Skippenite sits at Mohs 1.5-2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Skippenite leaves a lead-gray streak.
- 3Read the lusterHold the specimen under a strong light. Skippenite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray, silver-white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: platy crystals, foliated masses, lamellar aggregates.
Often confused with
Skippenite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside skippenite
Minerals reported to co-occur with skippenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Bi₂Se₂Te
- Mohs hardness
- 1.5-2
- Density
- 7.6-7.8 g/cm³
- Colors
- Streak
- Lead-gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Platy Crystals, Foliated Masses, Lamellar Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Gold-bearing Quartz Veins
- Typical price
- $50-300 per specimen
Where rockhounds find skippenite
Classic worldwide localities
- Skippen Creek, British Columbia, Canada
- various hydrothermal vein deposits
Field-hunting tip
Look in hydrothermal gold-bearing quartz veins country — that is the host setting where skippenite typically forms. If you start seeing quartz, pyrite, calcite in float, you are in the right ground. Field specimens usually show a platy crystals, foliated masses, lamellar aggregates habit, so train your eye for that shape before scanning the outcrop.






