Mcconnellite is a rare copper chromium oxide mineral that occurs as small, dark, metallic tabular crystals in oxidized zones of copper deposits. It is structurally related to the delafossite group and is primarily a curiosity for advanced mineralogists and systematic collectors. Specimens are typically microscopic to thumbnail-sized and are found in very limited localities worldwide.
Is this mcconnellite?
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 mcconnellite with a known reference. Mcconnellite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Mcconnellite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Mcconnellite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: dark gray, black.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals.
Often confused with
Mcconnellite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside mcconnellite
Minerals reported to co-occur with mcconnellite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuCrO₂
- Mohs hardness
- 3
- Density
- 8.8 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Copper Deposits
- Typical price
- $50-300 per specimen depending on size and provenance
Where rockhounds find mcconnellite
Classic worldwide localities
- Mohave County, Arizona, USA
- Sierra Nevada, California, USA
Field-hunting tip
Look in oxidized copper deposits country, the host setting where mcconnellite typically forms. If you start seeing delafossite, chrysocolla, quartz in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.



