Dzharkenite is a very rare iron selenide mineral that typically occurs as small, metallic grains within hydrothermal veins. It is visually similar to pyrite but is distinguished by its specific occurrence in selenium-rich environments and its distinct chemical composition.
Is this dzharkenite?
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 dzharkenite with a known reference. Dzharkenite sits at Mohs 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Dzharkenite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Dzharkenite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: gray, blackish-gray.
- 5Look at form & habitCrystal system: cubic. Typical habit: granular.
Often confused with
Dzharkenite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Pyrite is the harder of the two (Mohs 6-6.5 vs. 3.5-4); streak differs, so Dzharkenite leaves black, Pyrite leaves greenish-black to brownish-black.

How to tell apart: Marcasite is the harder of the two (Mohs 6-6.5 vs. 3.5-4); streak differs, so Dzharkenite leaves black, Marcasite leaves greyish-black.
Often found alongside dzharkenite
Minerals reported to co-occur with dzharkenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeSe₂
- Mohs hardness
- 3.5-4
- Density
- 5.35 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Study
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find dzharkenite
Classic worldwide localities
- Dzharken, Kazakhstan
Field-hunting tip
Look in hydrothermal veins country, the host setting where dzharkenite typically forms. If you start seeing clausthalite, tiemannite, pyrite in float, you are in the right ground. Field specimens usually show a granular habit, so train your eye for that shape before scanning the outcrop.


