Quetzalcoatlite is an extremely rare copper-zinc tellurite mineral discovered in Mexico. It typically occurs as small, delicate hexagonal plates or crusts within the oxidized zones of tellurium-rich ore deposits.
Is this quetzalcoatlite?
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 quetzalcoatlite with a known reference. Quetzalcoatlite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale blue, almost white.
- 3Read the lusterHold the specimen under a strong light. Luster: pearly to dull.
- 4Match the color rangeCompare against the expected color range: blue.
- 5Look at form & habitCrystal system: trigonal. Typical habit: hexagonal plates.
Often confused with
Quetzalcoatlite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside quetzalcoatlite
Minerals reported to co-occur with quetzalcoatlite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃Zn₆Te₂O₁₂(OH)₆·(Ag,Pb,□)Cl
- Mohs hardness
- 3
- Density
- 6.05 g/cm³
- Colors
- Streak
- Pale blue, almost white
- Luster
- Pearly to dull
- Transparency
- Semitransparent
- Crystal system
- Trigonal
- Crystal habit
- Hexagonal plates
- Cleavage
- On {1010}, fair
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare mineral in the oxidized zone of tellurium-bearing hydrothermal ore deposits
Where rockhounds find quetzalcoatlite
Classic worldwide localities
- Old Guard mine, Tombstone, Cochise Co., Arizona, USA
- Blue Bell claims, San Bernardino Co., California, USA
- Centennial Eureka mine, Tintic district, Juab Co., Utah, USA
- Oriental (Bambollita) mine, northeast of the Moctezuma mine, Moctezuma, Sonora, Mexico
Field-hunting tip
Where it forms: A rare mineral in the oxidized zone of tellurium-bearing hydrothermal ore deposits. If you start seeing hessite, galena, bornite in float, you are in the right ground. Typical habit: hexagonal plates. Train your eye for that shape before scanning the outcrop.







