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 — 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 — 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 — that is 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.


