Minehillite is a rare phyllosilicate mineral uniquely associated with the zinc deposits of the Franklin Mining District. It is most easily identified by its bright blue fluorescence under ultraviolet light and its characteristic micaceous, platy crystal structure.
Is this minehillite?
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 minehillite with a known reference. Minehillite sits at Mohs ~4, 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: pearly on cleavage, vitreous on fractures.
- 4Match the color rangeCompare against the expected color range: white, colorless, gray white, grayish black.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: platy.
Often confused with
Minehillite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside minehillite
Minerals reported to co-occur with minehillite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (K,Na)₂Ca₂₈Zn₅Al₄Si₄₀O₁₁₂(OH)₁₆
- Mohs hardness
- ~4
- Density
- 2.93 g/cm³
- Streak
- White
- Luster
- Pearly on cleavage, vitreous on fractures
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Platy
- Cleavage
- {0001}, perfect
- Fluorescence
- Dull violet under SW and LW UV
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- A secondary low-temperature hydrothermal mineral formed by replacement of associated minerals in a metamorphosed stratiform zinc deposit
Where rockhounds find minehillite
Classic worldwide localities
- Franklin, Sussex Co., New Jersey, USA
Field-hunting tip
Where it forms: A secondary low-temperature hydrothermal mineral formed by replacement of associated minerals in a metamorphosed stratiform zinc deposit. If you start seeing microcline, wollastonite, grossular in float, you are in the right ground. Typical habit: platy. Train your eye for that shape before scanning the outcrop.







