Kolicite is an extremely rare manganese zinc silicate-arsenate mineral known almost exclusively from the Franklin-Sterling Hill mining district. It is prized by fluorescent mineral collectors for its vivid orange-red reaction under shortwave ultraviolet light.
Is this kolicite?
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 kolicite with a known reference. Kolicite sits at Mohs ~4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: light orange.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: yellow orange.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: anhedral grains, massive.
Often confused with
Kolicite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Willemite is the harder of the two (Mohs 5.5 vs. ~4.5); streak differs, so Kolicite leaves light orange, Willemite leaves white.

How to tell apart: Streak differs, so Kolicite leaves light orange, Hodgkinsonite leaves white.
Often found alongside kolicite
Minerals reported to co-occur with kolicite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn₄Mn₇(AsO₄)₂(SiO₄)₂(OH)₈
- Mohs hardness
- ~4.5
- Density
- 4.17 g/cm³
- Colors
- Streak
- Light orange
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Anhedral grains, massive
- Cleavage
- None
- Fluorescence
- Bright orange-red under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Incrusting willemite-franklinite ore from metamorphosed stratiform zinc orebodies
Where rockhounds find kolicite
Classic worldwide localities
- Sterling Hill, Ogdensburg, and at Franklin, Sussex Co., New Jersey, USA
Field-hunting tip
Where it forms: Incrusting willemite-franklinite ore from metamorphosed stratiform zinc orebodies. If you start seeing willemite, franklinite, sonolite in float, you are in the right ground. Typical habit: anhedral grains, massive. Train your eye for that shape before scanning the outcrop.




