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 — that is 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.



