Achávalite is a rare iron selenide mineral that typically forms as metallic, bronze-colored grains within hydrothermal veins. Collectors most often find it in argentiferous or selenide-bearing mineral deposits where it is usually associated with other rare sulfide and selenide species.
Is this achávalite?
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 achávalite with a known reference. Achávalite 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. Achávalite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Achávalite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: bronze, reddish-brown.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: massive, anhedral grains.
Often confused with
Achávalite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside achávalite
Minerals reported to co-occur with achávalite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeSe
- Mohs hardness
- 3.5-4
- Density
- 6.6 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Massive, Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find achávalite
Classic worldwide localities
- Cacheuta, Argentina
- Krushev Dol, Bulgaria
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where achávalite typically forms. If you start seeing calcite, pyrite, siderite in float, you are in the right ground. Field specimens usually show a massive, anhedral grains habit, so train your eye for that shape before scanning the outcrop.





