Graemite is a rare copper tellurite mineral typically found as small, bright green bladed crystals or radial clusters. It is almost exclusively associated with the type locality in the Tombstone District of Arizona, where it forms in the oxidation zones of telluride-bearing mineral deposits.
Is this graemite?
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 graemite with a known reference. Graemite 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. Streak: pale blue-green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: green, blue green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: bladed crystals, radial aggregates.
Often confused with
Graemite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside graemite
Minerals reported to co-occur with graemite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuTeO₃·H₂O
- Mohs hardness
- 3-3.5
- Density
- 4.13 g/cm³
- Colors
- Streak
- Pale blue-green
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Bladed crystals, radial aggregates
- Cleavage
- On {010}, good; on {100}, a parting
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare dehydration product of teineite, as pseudomorphs and incrustations
Where rockhounds find graemite
Classic worldwide localities
- Cole shaft and in the Shattuck mine, Bisbee, Warren district, Cochise Co., and in the Dome Rock Mountains, La Paz Co, Arizona, USA
Field-hunting tip
Where it forms: A rare dehydration product of teineite, as pseudomorphs and incrustations. If you start seeing teineite, malachite, cuprite in float, you are in the right ground. Typical habit: bladed crystals, radial aggregates. Train your eye for that shape before scanning the outcrop.






