Nickellotharmeyerite is a rare arsenic-bearing mineral belonging to the Tsumcorite group. It is typically found as small, vibrant yellow to orange prismatic crystals or crusts in the oxidation zones of ore deposits. Due to its rarity and specific chemical requirements, it is primarily a target for advanced mineral collectors.
Is this nickellotharmeyerite?
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 nickellotharmeyerite with a known reference. Nickellotharmeyerite sits at Mohs 4-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Nickellotharmeyerite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Nickellotharmeyerite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, crusts.
Often confused with
Nickellotharmeyerite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside nickellotharmeyerite
Minerals reported to co-occur with nickellotharmeyerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaNi₂(AsO₄)₂·2H₂O
- Mohs hardness
- 4-5
- Density
- 4.5-5.5 g/cm³
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Crusts
- Cleavage
- Good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Arsenic-rich Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find nickellotharmeyerite
Classic worldwide localities
- Schneeberg, Saxony, Germany
- Tsumeb, Namibia
Field-hunting tip
Look in oxidized hydrothermal arsenic-rich deposits country — that is the host setting where nickellotharmeyerite typically forms. If you start seeing pharmacolite, goethite, scorodite in float, you are in the right ground. Field specimens usually show a prismatic crystals, crusts habit, so train your eye for that shape before scanning the outcrop.




