Fuettererite is a rare lead-copper tellurite mineral discovered in the oxidized zones of Mexican ore deposits. It typically forms as delicate, pale green to yellow-green tabular crystals and is highly prized by advanced mineral collectors for its chemical complexity and scarcity.
Is this fuettererite?
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 fuettererite with a known reference. Fuettererite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale bluish green.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: bluish green.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, subparallel aggregates.
Often confused with
Fuettererite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Emmonsite is the harder of the two (Mohs ~5 vs. 2-3); luster reads adamantine on Fuettererite and vitreous on Emmonsite.

How to tell apart: Luster reads adamantine on Fuettererite and pearly to dull on Quetzalcoatlite.
Often found alongside fuettererite
Minerals reported to co-occur with fuettererite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₃Cu₆TeO₆(OH)₇Cl₅
- Mohs hardness
- 2-3
- Density
- 5.552 g/cm³
- Colors
- Streak
- Pale bluish green
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Tabular crystals, subparallel aggregates
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary phase formed by partial oxidation of tellurides, chalcopyrite and galena in quartz veins
Where rockhounds find fuettererite
Classic worldwide localities
- NE2 vein and the Bird Nest drift, Otto Mountain, near Baker, California, USA
Field-hunting tip
Where it forms: A secondary phase formed by partial oxidation of tellurides, chalcopyrite and galena in quartz veins. If you start seeing br-rich chlorargyrite, iodargyrite, telluroperite in float, you are in the right ground. Typical habit: tabular crystals, subparallel aggregates. Train your eye for that shape before scanning the outcrop.





