Bukovite is a rare thallium copper selenide mineral typically found as small, opaque grains within hydrothermal selenide ore deposits. Collectors primarily find it in association with other selenide minerals in specific localities such as the type-locality at the Bukov mine in the Czech Republic.
Is this bukovite?
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 bukovite with a known reference. Bukovite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Bukovite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Bukovite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: dark gray, white.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: anhedral to subhedral grains and massive.
Often confused with
Bukovite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside bukovite
Minerals reported to co-occur with bukovite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Tl₂Cu₃Se₄
- Mohs hardness
- 2.5-3
- Density
- 7.3 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Anhedral to Subhedral Grains and Massive
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Selenide Deposits
- Typical price
- $50-300 per specimen depending on size and rarity
Where rockhounds find bukovite
Classic worldwide localities
- Bukov mine, Czech Republic
- Skrikerum, Sweden
- Taimyr Peninsula, Russia
Field-hunting tip
Look in hydrothermal selenide deposits country — that is the host setting where bukovite typically forms. If you start seeing clausthalite, umangite, berzelianite in float, you are in the right ground. Field specimens usually show a anhedral to subhedral grains and massive habit, so train your eye for that shape before scanning the outcrop.




