Zincospiroffite is a rare tellurite mineral discovered in the oxidized zones of tellurium-bearing deposits. It typically forms small, clear, tabular crystals and is predominantly found associated with other tellurium minerals in the Moctezuma mine region of Mexico.
Is this zincospiroffite?
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 zincospiroffite with a known reference. Zincospiroffite 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. Zincospiroffite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Zincospiroffite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic to tabular crystals.
Often confused with
Zincospiroffite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside zincospiroffite
Minerals reported to co-occur with zincospiroffite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn₂Te₃O₈
- Mohs hardness
- 3.5-4
- Density
- 5.73 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic to Tabular Crystals
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Tellurium-rich Hydrothermal Deposits
- Typical price
- $50-300 per micro-mount or thumbnail
Where rockhounds find zincospiroffite
Classic worldwide localities
- Moctezuma mine, Sonora, Mexico
Field-hunting tip
Look in tellurium-rich hydrothermal deposits country — that is the host setting where zincospiroffite typically forms. If you start seeing tellurium, spiroffite, quartz in float, you are in the right ground. Field specimens usually show a prismatic to tabular crystals habit, so train your eye for that shape before scanning the outcrop.



