Tyrrellite is a very rare copper-iron-cobalt selenide mineral that typically forms as small, steel-grey metallic grains. It is most famous for its occurrences in selenide-rich hydrothermal mineral assemblages, often found alongside clausthalite.
Is this tyrrellite?
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 tyrrellite with a known reference. Tyrrellite 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. Tyrrellite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Tyrrellite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: gray, steel gray.
- 5Look at form & habitCrystal system: cubic. Typical habit: granular, massive, anhedral to subhedral crystals.
Often confused with
Tyrrellite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside tyrrellite
Minerals reported to co-occur with tyrrellite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Cu,Fe,Co)₃Se₄
- Mohs hardness
- 3.5-4
- Density
- 5.6 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Granular, Massive, Anhedral to Subhedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins, Selenide-bearing Deposits
- Typical price
- $50-300 for small microspecimens
Where rockhounds find tyrrellite
Classic worldwide localities
- Hope's Nose, Torquay, England
- Skrikerum, Sweden
- Krunkelbach valley, Germany
Field-hunting tip
Look in hydrothermal veins, selenide-bearing deposits country — that is the host setting where tyrrellite typically forms. If you start seeing clausthalite, gold, hematite in float, you are in the right ground. Field specimens usually show a granular, massive, anhedral to subhedral crystals habit, so train your eye for that shape before scanning the outcrop.






