Hancockite is a rare lead-bearing member of the epidote group typically found in the famous zinc-manganese orebodies of Franklin and Sterling Hill. Collectors look for its distinctive deep reddish-brown tabular crystals that often display a subtle, vitreous luster.
Is this hancockite?
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 hancockite with a known reference. Hancockite sits at Mohs 6-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: grayish white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: crystals yellowish brown, yellow-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic to tabular crystals.
Often confused with
Hancockite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside hancockite
Minerals reported to co-occur with hancockite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaPbFeAl₂(Si₂O₇)(SiO₄)O(OH)
- Mohs hardness
- 6-7
- Density
- 4.03 g/cm³
- Colors
- Crystals yellowish brownYellow-green
- Streak
- Grayish white
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic to tabular crystals
- Cleavage
- {001}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a metamorphosed stratiform zinc deposit (Franklin, New Jersey, USA); in a metamorphosed manganese-iron orebody in skarns enclosed in dolomitic marble (Jakobsberg, Sweden)
Where rockhounds find hancockite
Classic worldwide localities
- Franklin, Sussex Co., New Jersey, USA
- Jakobsberg, Värmland, Sweden
Field-hunting tip
Where it forms: In a metamorphosed stratiform zinc deposit (Franklin, New Jersey, USA); in a metamorphosed manganese-iron orebody in skarns enclosed in dolomitic marble (Jakobsberg, Sweden). If you start seeing andradite, franklinite, manganaxinite in float, you are in the right ground. Typical habit: prismatic to tabular crystals. Train your eye for that shape before scanning the outcrop.








