Tellurite is a rare secondary mineral formed in the oxidized zones of tellurium-rich ore deposits. Collectors typically look for its distinct acicular or radiating crystal clusters that exhibit an adamantine luster, most notably coming from the Moctezuma mine in Mexico.
Is this tellurite?
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 tellurite with a known reference. Tellurite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tellurite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tellurite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: white, yellowish-white, colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular or prismatic crystals, radiating clusters, crusts.
Often confused with
Tellurite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside tellurite
Minerals reported to co-occur with tellurite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- TeO₂
- Mohs hardness
- 2
- Density
- 4.45 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular or Prismatic Crystals, Radiating Clusters, Crusts
- Cleavage
- Perfect On {010}
- Rarity
- Rare
- Uses
- Collector, Reference Material
- Host rock
- Oxidized Zones of Tellurium-bearing Hydrothermal Gold Deposits
- Typical price
- $50-500 depending on specimen size and clarity
Where rockhounds find tellurite
Classic worldwide localities
- Moctezuma, Mexico
- Goldfield, Nevada
- Satu Mare, Romania
Field-hunting tip
Look in oxidized zones of tellurium-bearing hydrothermal gold deposits country — that is the host setting where tellurite typically forms. If you start seeing paratellurite, emmonsite, tlapallite in float, you are in the right ground. Field specimens usually show a acicular or prismatic crystals, radiating clusters, crusts habit, so train your eye for that shape before scanning the outcrop.




