Chlorophoenicite is a rare zinc-arsenic mineral best known for its association with the famous Franklin mining district in New Jersey. It typically forms as prismatic to acicular crystals or radial sprays in shades of pink, and it is highly prized by collectors for its distinctive fluorescence under ultraviolet light.
Is this chlorophoenicite?
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 chlorophoenicite with a known reference. Chlorophoenicite sits at Mohs 3.5, 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, silky, pearly on cleavages.
- 4Match the color rangeCompare against the expected color range: grayish green, purplish red.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, radial sprays, fibrous aggregates.
Often confused with
Chlorophoenicite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chlorophoenicite
Minerals reported to co-occur with chlorophoenicite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn₃Zn₂(OH)₆As[O₃(OH)₃]
- Mohs hardness
- 3.5
- Density
- 3.46-3.53 g/cm³
- Colors
- Grayish greenPurplish red
- Streak
- White
- Luster
- Vitreous, silky, pearly on cleavages
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals, radial sprays, fibrous aggregates
- Cleavage
- Good on {100}
- Fluorescence
- Bright white/yellow under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Along secondary cracks through franklinite ores in a metamorphosed stratiform zinc orebody
Where rockhounds find chlorophoenicite
Classic worldwide localities
- Franklin and Sterling Hill, Ogdensburg, Sussex Co., New Jersey, USA
Field-hunting tip
Where it forms: Along secondary cracks through franklinite ores in a metamorphosed stratiform zinc orebody. If you start seeing leucophoenicite, hodgkinsonite, hetaerolite in float, you are in the right ground. Typical habit: prismatic crystals, radial sprays, fibrous aggregates. Train your eye for that shape before scanning the outcrop.








