Sederholmite is a rare nickel selenide that typically occurs as tiny, metallic, hexagonal plates or grains within hydrothermal veins. It is most often identified by its association with other rare selenium-bearing minerals in complex ore deposits. Collectors primarily seek it as an obscure end-member in mineralogical suites.
Is this sederholmite?
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 sederholmite with a known reference. Sederholmite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Sederholmite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Sederholmite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: bronze, pale brass-yellow.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: hexagonal plates, granular, massive.
Often confused with
Sederholmite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside sederholmite
Minerals reported to co-occur with sederholmite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- β-NiSe
- Mohs hardness
- 3-3.5
- Density
- 5.65 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Hexagonal Plates, Granular, Massive
- Cleavage
- Distinct On Basal Plane
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Selenide Veins
- Typical price
- $50-300 per specimen
Where rockhounds find sederholmite
Classic worldwide localities
- Uran mine, Czech Republic
- Trogtal quarry, Germany
- Clausthal-Zellerfeld, Germany
Field-hunting tip
Look in hydrothermal selenide veins country, the host setting where sederholmite typically forms. If you start seeing clausthalite, tiemannite, berzelianite in float, you are in the right ground. Field specimens usually show a hexagonal plates, granular, massive habit, so train your eye for that shape before scanning the outcrop.






