Samfowlerite is a very rare silicate mineral found exclusively in the unique metamorphic environment of Franklin, New Jersey. It typically occurs as small, pale pink to colorless tabular crystals or granular masses associated with other zinc-rich minerals.
Is this samfowlerite?
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 samfowlerite with a known reference. Samfowlerite sits at Mohs <3, 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: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: crystalline.
Often confused with
Samfowlerite 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. <3).

How to tell apart: Clinohedrite is the harder of the two (Mohs 5.5 vs. <3); luster reads vitreous on Samfowlerite and brilliant, glassy; pearly on {010} on Clinohedrite.
Often found alongside samfowlerite
Minerals reported to co-occur with samfowlerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₁₄Mn₃Zn₂Be₂Be₆Si₁₄O₅₂(OH)₆
- Mohs hardness
- <3
- Density
- 3.28 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Crystalline
- Cleavage
- None
- Fluorescence
- Weak red under SW and LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In vugs in granular willemite-franklinite-andradite ore from a metamorphosed stratiform Zn{Mn deposit
Where rockhounds find samfowlerite
Classic worldwide localities
- Franklin, Sussex Co., New Jersey, USA
Field-hunting tip
Where it forms: In vugs in granular willemite-franklinite-andradite ore from a metamorphosed stratiform Zn{Mn deposit. If you start seeing andradite-grossular, cahnite, clinochlore in float, you are in the right ground. Typical habit: crystalline. Train your eye for that shape before scanning the outcrop.






