Hendricksite is a rare zinc-bearing member of the mica group, typically identified by its dark, bronzy, micaceous platy crystals. It is primarily found within the unique mineral environment of the Sterling Hill mine in New Jersey. Collectors should look for its distinctive pearly luster and perfect basal cleavage characteristic of the mica family.
Is this hendricksite?
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 hendricksite with a known reference. Hendricksite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Hendricksite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Hendricksite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: dark brown, reddish brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy, micaceous.
Often confused with
Hendricksite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside hendricksite
Minerals reported to co-occur with hendricksite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (K,Na)(Zn,Mn,Mg,Fe²⁺)₃(Si₃Al)O₁₀(OH,F)₂
- Mohs hardness
- 2.5-3
- Density
- 3.10-3.15 g/cm³
- Colors
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy, Micaceous
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Zinc Ore Deposits
- Typical price
- $20-150 thumbnail
Where rockhounds find hendricksite
Classic worldwide localities
- Sterling Hill Mine, New Jersey, USA
Field-hunting tip
Look in metamorphic zinc ore deposits country — that is the host setting where hendricksite typically forms. If you start seeing willemite, franklinite, zincite in float, you are in the right ground. Field specimens usually show a platy, micaceous habit, so train your eye for that shape before scanning the outcrop.





