Hodgkinsonite is a rare silicate mineral primarily known from the unique zinc ore deposits of the Franklin Mining District. It is highly sought after by fluorescent mineral collectors due to its vivid orange-red reaction under shortwave UV light. Collectors should look for transparent pink to reddish prisms often associated with other rare zinc-manganese minerals.
Is this hodgkinsonite?
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 hodgkinsonite with a known reference. Hodgkinsonite 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: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: light pink, orange, reddish brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular, radial.
Often confused with
Hodgkinsonite vs. its common look-alikes, and how to tell them apart in the field.


How to tell apart: Luster reads vitreous on Hodgkinsonite and brilliant, glassy; pearly on {010} on Clinohedrite.

How to tell apart: Luster reads vitreous on Hodgkinsonite and dull to slightly greasy on Esperite.
Often found alongside hodgkinsonite
Minerals reported to co-occur with hodgkinsonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn₂Mn²⁺(SiO₄)(OH)₂
- Mohs hardness
- <5
- Density
- 4.06-4.08 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular, radial
- Cleavage
- Perfect on {001}
- Fluorescence
- Red under LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As seams in massive willemite-franklinite granular ore in a metamorphosed stratiform zinc deposit (Franklin, New Jersey, USA)
Where rockhounds find hodgkinsonite
Classic worldwide localities
- Franklin and Sterling Hill, Ogdensburg, Sussex Co., New Jersey, USA
Field-hunting tip
Where it forms: As seams in massive willemite-franklinite granular ore in a metamorphosed stratiform zinc deposit (Franklin, New Jersey, USA). If you start seeing barite, willemite, franklinite in float, you are in the right ground. Typical habit: acicular, radial. Train your eye for that shape before scanning the outcrop.





