Pararaisaite is an extremely rare copper tellurite mineral discovered in the Moctezuma mine of Mexico. It typically forms attractive blue to green bladed or radial crystal clusters that are highly sought after by mineral collectors specializing in rare tellurium species.
Is this pararaisaite?
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 pararaisaite with a known reference. Pararaisaite sits at Mohs 2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: bladed crystals, radial aggregates.
Often confused with
Pararaisaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pararaisaite
Minerals reported to co-occur with pararaisaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- [Mg(H₂O)₆]CuTeO₄(OH)₂
- Mohs hardness
- 2.5
- Density
- 2.85 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Bladed crystals, radial aggregates
- Cleavage
- Perfect on {001}, good on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An oxidation-zone mineral in a hydrothermal polymetallic Au-Ag-Cu-Pb vein deposit in contact-metamorphosed dolomite
Where rockhounds find pararaisaite
Classic worldwide localities
- North Star mine, Mammoth, Tintic district, Juab County, Utah, USA
Field-hunting tip
Where it forms: An oxidation-zone mineral in a hydrothermal polymetallic Au-Ag-Cu-Pb vein deposit in contact-metamorphosed dolomite. If you start seeing barite, goldfieldite, malachite in float, you are in the right ground. Typical habit: bladed crystals, radial aggregates. Train your eye for that shape before scanning the outcrop.






