Nelenite is a rare manganese silicate mineral primarily known from the unique zinc mines of Franklin and Sterling Hill. It typically appears as yellowish-brown tabular crystals or foliated masses often associated with willemite and franklinite.
Is this nelenite?
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 nelenite with a known reference. Nelenite sits at Mohs ~5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: light brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous on cleavages, resinous and duller on fractures.
- 4Match the color rangeCompare against the expected color range: brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: crystalline, massive.
Often confused with
Nelenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside nelenite
Minerals reported to co-occur with nelenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn₁₆As₃Si₁₂O₃₆(OH)₁₇
- Mohs hardness
- ~5
- Density
- 3.46 g/cm³
- Colors
- Streak
- Light brown
- Luster
- Vitreous on cleavages, resinous and duller on fractures
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Crystalline, massive
- Cleavage
- {0001}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a metamorphosed stratiform zinc deposit, within pegmatitic textured masses, and as calcite-cemented fragments in a breccia probably derived from the pegmatitic material
Where rockhounds find nelenite
Classic worldwide localities
- Franklin, Sussex Co., New Jersey, USA
Field-hunting tip
Where it forms: In a metamorphosed stratiform zinc deposit, within pegmatitic textured masses, and as calcite-cemented fragments in a breccia probably derived from the pegmatitic material. If you start seeing actinolite, calcite, willemite in float, you are in the right ground. Typical habit: crystalline, massive. Train your eye for that shape before scanning the outcrop.






