Fowlerite is a zinc-rich variety of the mineral rhodonite found primarily in the zinc mines of Franklin, New Jersey. It is highly valued by collectors for its distinct pink color and its association with the unique fluorescent mineral assemblage of the region.
Is this fowlerite?
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 fowlerite with a known reference. Fowlerite sits at Mohs 5.5-6.5, 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: pink, reddish-pink, brownish-pink.
- 5Look at form & habitCrystal system: triclinic. Typical habit: massive, granular, tabular crystals.
Often confused with
Fowlerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside fowlerite
Minerals reported to co-occur with fowlerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mn,Zn)SiO₃
- Mohs hardness
- 5.5-6.5
- Density
- 3.5-3.7 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Massive, granular, tabular crystals
- Cleavage
- Perfect in two directions
- Rarity
- Rare
- Uses
- Collector, Lapidary
- Host rock
- metamorphosed zinc ore deposits
Where rockhounds find fowlerite
Classic worldwide localities
- Franklin, New Jersey
- Sterling Hill, New Jersey
Field-hunting tip
Where it forms: metamorphosed zinc ore deposits. If you start seeing willemite, franklinite, zincite in float, you are in the right ground. Typical habit: massive, granular, tabular crystals. Train your eye for that shape before scanning the outcrop.







