Paratellurite is the tetragonal polymorph of tellurium dioxide, typically found as tiny, transparent, adamantine prismatic crystals in the oxidation zones of tellurium-rich ore deposits. It is highly valued by mineral collectors for its rarity and its distinct association with other secondary tellurium minerals.
Is this paratellurite?
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 paratellurite with a known reference. Paratellurite 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. Paratellurite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Paratellurite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellowish-white.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: prismatic crystals, acicular, granular.
Often confused with
Paratellurite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside paratellurite
Minerals reported to co-occur with paratellurite. 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
- 5.99 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Prismatic Crystals, Acicular, Granular
- Cleavage
- Perfect On {110}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Tellurium-bearing Hydrothermal Gold-telluride Deposits
- Typical price
- $50-300 for small thumbnail specimens
Where rockhounds find paratellurite
Classic worldwide localities
- Moctezuma, Mexico
- Goldfield, Nevada, USA
- Kawazu mine, Japan
Field-hunting tip
Look in oxidized zones of tellurium-bearing hydrothermal gold-telluride deposits country — that is the host setting where paratellurite typically forms. If you start seeing tellurite, tellurium, emmonsite in float, you are in the right ground. Field specimens usually show a prismatic crystals, acicular, granular habit, so train your eye for that shape before scanning the outcrop.




