Nolzeite is a rare sodium manganese hydroxide, typically colorless to pale green. It is a late-stage mineral likely formed under alkaline conditions in vugs in altered sodalite syenite. It was first described from Poudrette quarry, La Vallée-du-Richelieu, Montérégie, Québec, Canada.
Is this nolzeite?
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 nolzeite with a known reference. Nolzeite sits at Mohs 4, 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: colorless, pale green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals.
Often confused with
Nolzeite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside nolzeite
Minerals reported to co-occur with nolzeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na(Mn,☐)₂[Si₃(B,Si)O₉(OH)₂](H₂O)₂
- Mohs hardness
- 4
- Density
- 2.79 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A late-stage mineral likely formed underalkaline conditions in vugs in altered sodalite syenite
Where rockhounds find nolzeite
Classic worldwide localities
- Poudrette quarry, La Vallée-du-Richelieu, Montérégie (formerly Rouville County), Québec, Canada
Field-hunting tip
Where it forms: A late-stage mineral likely formed underalkaline conditions in vugs in altered sodalite syenite. If you start seeing aegirine, nepheline, sodalite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.








