Mendozavilite-NaCu is an extremely rare secondary molybdate mineral typically found as earthy crusts or powdery coatings in oxidized ore deposits. It is best identified by its association with other molybdenum minerals in arid environments, though positive identification usually requires powder X-ray diffraction analysis.
Is this mendozavilite-nacu?
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 mendozavilite-nacu with a known reference. Mendozavilite-NaCu 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: colorless to very pale green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to subadamantine.
- 4Match the color rangeCompare against the expected color range: lime green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: powdery, earthy, granular aggregates.
Often confused with
Mendozavilite-NaCu vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside mendozavilite-nacu
Minerals reported to co-occur with mendozavilite-nacu. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- [Na₂(H₂O)₁₅Cu(H₂O)₆][Mo₈P₂Fe₃O₃₄(OH)₃]
- Mohs hardness
- ~2.5
- Density
- 2.824 g/cm³
- Colors
- Lime green
- Streak
- Colorless to very pale green
- Luster
- Vitreous to subadamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Powdery, earthy, granular aggregates
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxidized zone of porphyry copper deposit as thin vein fillings and well-formed crystals in cavities
Where rockhounds find mendozavilite-nacu
Classic worldwide localities
- Lomas Bayas mine, 93 km east northeast of Antofagasta, Antofagasta Province, Chile
Field-hunting tip
Where it forms: In the oxidized zone of porphyry copper deposit as thin vein fillings and well-formed crystals in cavities. If you start seeing quartz, feruvite, muscovite in float, you are in the right ground. Typical habit: powdery, earthy, granular aggregates. Train your eye for that shape before scanning the outcrop.







