Wallkilldellite-(Fe) is a rare arsenate mineral characterized by its reddish-brown platy crystals and radial habits. It is primarily found in the metamorphosed zinc ore deposits of the Sterling Hill Mine, where it occurs as a late-stage secondary mineral. Collectors value it for its limited occurrence and relationship to other rare Franklin-area arsenates.
Is this wallkilldellite-(fe)?
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 wallkilldellite-(fe) with a known reference. Wallkilldellite-(Fe) sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: light brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous on cleavage surfaces; slightly resinous on fracture surfaces.
- 4Match the color rangeCompare against the expected color range: brownish yellow.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: microscopic crystals, spherical.
Often confused with
Wallkilldellite-(Fe) vs. its common look-alikes, and how to tell them apart in the field.
How to tell apart: Streak differs, so Wallkilldellite-(Fe) leaves light brown, Wallkilldellite leaves pale orange.

How to tell apart: Streak differs, so Wallkilldellite-(Fe) leaves light brown, Chlorophoenicite leaves white.
Often found alongside wallkilldellite-(fe)
Minerals reported to co-occur with wallkilldellite-(fe). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂Fe₃(AsO₄)₂(OH)₄·9H₂O
- Mohs hardness
- 2-3
- Density
- 3.0 g/cm³
- Colors
- Streak
- Light brown
- Luster
- Vitreous on cleavage surfaces; slightly resinous on fracture surfaces
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Microscopic crystals, spherical
- Cleavage
- Perfect on {0001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Secondary in the oxidation zone of copper arsenide deposits
Where rockhounds find wallkilldellite-(fe)
Classic worldwide localities
- Roua mine, Alpes-Maritimes, France and the Uriya deposit, Kura mine, Saiki City, Oita Prefecture, Japan
Field-hunting tip
Where it forms: Secondary in the oxidation zone of copper arsenide deposits. If you start seeing cuprite, algodonite, domeykite in float, you are in the right ground. Typical habit: microscopic crystals, spherical. Train your eye for that shape before scanning the outcrop.





