Native selenium is a rare elemental mineral often found as needle-like crystals or powdery encrustations in hydrothermal deposits. It is known for its distinct metallic grey to reddish-grey appearance and is chemically sensitive, requiring careful storage to prevent degradation.
Is this selenium?
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 selenium with a known reference. Selenium sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: red.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: gray, purple gray, reddish.
- 5Look at form & habitCrystal system: trigonal. Typical habit: crystalline, disseminated, granular.
Often confused with
Selenium vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside selenium
Minerals reported to co-occur with selenium. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Se
- Mohs hardness
- 2
- Density
- 4.80 g/cm³
- Streak
- Red
- Luster
- Metallic
- Transparency
- Opaque, transparent in very thin fragments
- Crystal system
- Trigonal
- Crystal habit
- Crystalline, disseminated, granular
- Cleavage
- Good on {0112}
- Rarity
- Rare
- Uses
- Collector, Industrial
- Host rock
- Formed at relatively low temperatures by sublimation of fumarolic vapors, and from oxidation of selenium-bearing organic compounds in sandstone U–V deposits; from burning coal and pyritic ores
Where rockhounds find selenium
2 mapped spotsClassic worldwide localities
- United Verde mine, Jerome, Yavapai Co., Arizona, USA
- Colorado Plateau, as in the Peanut mine, Bull Canyon, Uravan district, Montrose Co., Colorado, and the Parco No. 23 mine, Thompsons district, Grand Co., Utah, USA
- Road Hog No. 1A mine, Black Hills, Fall River Co., South Dakota, USA
- Mopung Hills, Churchill Co., and the Gold Quarry mine, near Carlin, Eureka Co., Nevada, USA
- Moctezuma (Bambolla) mine, 12 km south of Moctezuma, Sonora, Mexico
- Pacajake mine, Hiaco, 24 km east-northeast of Colquechaca, Potosí, Bolivia
Field-hunting tip
Where it forms: Formed at relatively low temperatures by sublimation of fumarolic vapors, and from oxidation of selenium-bearing organic compounds in sandstone U–V deposits; from burning coal and pyritic ores. If you start seeing pyrite, ferroselite, zippeite in float, you are in the right ground. Typical habit: crystalline, disseminated, granular. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah. Start trip planning there.







