Rheniite is a exceptionally rare rhenium sulfide mineral that primarily occurs in high-temperature volcanic fumaroles. It typically forms thin, metallic, platy crystals that closely resemble molybdenite, but it is unique for being the only mineral where rhenium is an essential constituent. Most specimens are sourced from the Kudryavy Volcano in the Kuril Islands, where it was first discovered.
Is this rheniite?
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 rheniite with a known reference. Rheniite 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. Rheniite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Rheniite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black, gray.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: platy crystals, scales, or massive aggregates.
Often confused with
Rheniite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside rheniite
Minerals reported to co-occur with rheniite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ReS₂
- Mohs hardness
- 1.5-2
- Density
- 7.5 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Platy Crystals, Scales, Or Massive Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- Fumarole Deposits
- Typical price
- $100-500+ per specimen
Where rockhounds find rheniite
Classic worldwide localities
- Kudryavy Volcano, Iturup Island, Kuril Islands, Russia
Field-hunting tip
Look in fumarole deposits country — that is the host setting where rheniite typically forms. If you start seeing molybdenite, pyrite, sulfur in float, you are in the right ground. Field specimens usually show a platy crystals, scales, or massive aggregates habit, so train your eye for that shape before scanning the outcrop.




