Ferroselite is a rare iron selenide mineral typically found in hydrothermal uranium-rich deposits. It is most easily identified by its distinct metallic luster and association with other selenium minerals like clausthalite, often occurring as fine-grained, radiating, or acicular crystals.
Is this ferroselite?
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 ferroselite with a known reference. Ferroselite sits at Mohs 6-6.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: bronze, steel gray, silver white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular, striated, twinning common.
Often confused with
Ferroselite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ferroselite
Minerals reported to co-occur with ferroselite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeSe₂
- Mohs hardness
- 6-6.5
- Density
- 7.20 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular, striated, twinning common
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In red-bed deposits of the Colorado Plateau type, peripheral to pyrite and uranium concentrations (Utah, USA); in U–V ores in sandstone, with coalified wood (Colorado, USA)
Where rockhounds find ferroselite
Classic worldwide localities
- Sandstones of the Powder River basin, Wyoming, USA
- Kermac Sec. 10 mine, McKinley Co., New Mexico, USA
- Mitten #2 mine, Navajo Co., Arizona, USA
- A number of mines in the Uravan district, Montrose Co., Colorado, USA
- Ust’-Uyuk V–Se–U deposit, Tuva, Siberia (type locality), Russia
- Zapadno-Ozernogo Cu–Zn deposit, Southern Ural Mountains, Russia
Field-hunting tip
Where it forms: In red-bed deposits of the Colorado Plateau type, peripheral to pyrite and uranium concentrations (Utah, USA); in U–V ores in sandstone, with coalified wood (Colorado, USA). If you start seeing uraninite, pyrite, marcasite in float, you are in the right ground. Typical habit: acicular, striated, twinning common. Train your eye for that shape before scanning the outcrop.






