Crednerite is a rare copper manganese oxide mineral typically found in oxidized zones of copper deposits. It often occurs as dark, metallic, platy or foliated aggregates and is best identified by its association with other manganese and copper minerals.
Is this crednerite?
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 crednerite with a known reference. Crednerite 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. Crednerite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Crednerite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, foliated to lamellar masses.
Often confused with
Crednerite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside crednerite
Minerals reported to co-occur with crednerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuMnO₂
- Mohs hardness
- 4.5
- Density
- 5.03 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Foliated to Lamellar Masses
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Manganese-copper Deposits
- Typical price
- $20-150 for small specimens
Where rockhounds find crednerite
Classic worldwide localities
- Friedrichroda, Thuringia, Germany
- Bisbee, Arizona, USA
- Kalahari Manganese Field, South Africa
Field-hunting tip
Look in oxidized hydrothermal manganese-copper deposits country — that is the host setting where crednerite typically forms. If you start seeing tenorite, hausmannite, pyrolusite in float, you are in the right ground. Field specimens usually show a platy crystals, foliated to lamellar masses habit, so train your eye for that shape before scanning the outcrop.




