Conichalcite is a vibrant green secondary mineral often found as attractive botryoidal or crust-like coatings on rock surfaces. It forms in the oxidized zones of copper-arsenic deposits and is frequently collected for its bright coloration and pleasing globular habits.
Is this conichalcite?
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 conichalcite with a known reference. Conichalcite 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. Conichalcite leaves a light green streak.
- 3Read the lusterHold the specimen under a strong light. Conichalcite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, yellow-green, emerald-green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: botryoidal, druzy, massive, or crusts.
Often confused with
Conichalcite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Conichalcite leaves light green, Austinite leaves white.

How to tell apart: Conichalcite is noticeably harder (Mohs 4.5 vs. 3); streak differs, so Conichalcite leaves light green, Olivenite leaves olive-green; luster reads vitreous on Conichalcite and adamantine on Olivenite.

Often found alongside conichalcite
Minerals reported to co-occur with conichalcite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCu(AsO₄)(OH)
- Mohs hardness
- 4.5
- Density
- 4.1-4.3 g/cm³
- Streak
- Light Green
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Botryoidal, Druzy, Massive, Or Crusts
- Cleavage
- None
- Rarity
- Common
- Uses
- Collector, Mineral Specimen
- Host rock
- Oxidized Zones of Arsenic-rich Hydrothermal Copper Deposits
- Typical price
- $10-100 per specimen depending on quality and matrix
Where rockhounds find conichalcite
Classic worldwide localities
- Gold Hill, Utah, USA
- Mapimi, Durango, Mexico
- Tsumeb, Namibia
- Bisbee, Arizona, USA
- Chile
Field-hunting tip
Look in oxidized zones of arsenic-rich hydrothermal copper deposits country, the host setting where conichalcite typically forms. If you start seeing malachite, limonite, adamine in float, you are in the right ground. Field specimens usually show a botryoidal, druzy, massive, or crusts habit, so train your eye for that shape before scanning the outcrop.


