Magnesiochlorophoenicite is a very rare member of the chlorophoenicite group typically found in the famous zinc mines of Franklin, New Jersey. It is most easily identified by its distinctive pink, radiating acicular crystal sprays associated with willemite and franklinite. Due to its arsenic content, collectors should handle specimens with care and ensure proper labeling.
Is this magnesiochlorophoenicite?
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 magnesiochlorophoenicite with a known reference. Magnesiochlorophoenicite sits at Mohs 3-3.5, 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 to pearly.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous to acicular radiating clusters.
Often confused with
Magnesiochlorophoenicite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside magnesiochlorophoenicite
Minerals reported to co-occur with magnesiochlorophoenicite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₃Zn₂(OH)₆As[O₃(OH)₃]
- Mohs hardness
- 3-3.5
- Density
- 3.37 g/cm³
- Streak
- White
- Luster
- Vitreous to pearly
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous to acicular radiating clusters
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- metamorphic zinc ore deposits
Where rockhounds find magnesiochlorophoenicite
Classic worldwide localities
- Franklin, New Jersey, USA
- Sterling Hill, New Jersey, USA
Field-hunting tip
Where it forms: metamorphic zinc ore deposits. If you start seeing willemite, zincite, franklinite in float, you are in the right ground. Typical habit: fibrous to acicular radiating clusters. Train your eye for that shape before scanning the outcrop.






