Coloradoite is a rare mercury telluride mineral often found in association with gold and silver deposits. It typically appears as massive, dark grey metallic grains that lack visible cleavage, and it is most famous for its occurrences in tellurium-rich epithermal vein systems.
Is this coloradoite?
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 coloradoite with a known reference. Coloradoite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Coloradoite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Coloradoite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: dark gray, black.
- 5Look at form & habitCrystal system: cubic. Typical habit: massive, granular, or rarely as tetrahedral crystals.
Often confused with
Coloradoite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside coloradoite
Minerals reported to co-occur with coloradoite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- HgTe
- Mohs hardness
- 2.5
- Density
- 8.1-8.2 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Massive, Granular, Or Rarely as Tetrahedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- Epithermal Gold-telluride Veins
- Typical price
- $50-500 depending on specimen size and association
Where rockhounds find coloradoite
Classic worldwide localities
- Boulder County, Colorado, USA
- Kalgoorlie, Western Australia
- Nagyág, Romania
- Taimyr Peninsula, Russia
Field-hunting tip
Look in epithermal gold-telluride veins country — that is the host setting where coloradoite typically forms. If you start seeing gold, tellurium, pyrite in float, you are in the right ground. Field specimens usually show a massive, granular, or rarely as tetrahedral crystals habit, so train your eye for that shape before scanning the outcrop.







