Zebra rock is an ornamental clayey siltstone unique to northern Western Australia, found around and in Lake Argyle south of Kununurra. It forms beds 5 to 15 cm thick in the Johnny Cake Member of the early Ediacaran Ranford Formation, banded in diffuse red and grey stripes 4 to 25 mm thick, with the red coming from hematite. How the banding formed is debated: it has been explained as marine clay, groundwater or hydrothermal alteration, and, in a 2020 study, an ancient waterlogged soil. It is widely used in jewelry and sculpture.
Is this zebra rock?
3-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Read the textureLook at a fresh break with a hand lens. Texture: Diffuse red and grey bands 4 to 25 mm thick. Grain size: clayey siltstone.
- 2Pick out the mineralsComposition: Clayey siltstone; red bands colored by hematite. Identify the two or three most abundant grains.
- 3Match the color rangeCompare against the expected color range: red, gray, white.
Often found alongside zebra rock
Minerals reported to co-occur with zebra rock. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Uses
- Jewelry, Decorative
- Host rock
- Johnny Cake Member of the early Ediacaran Ranford Formation
- Texture
- Diffuse red and grey bands 4 to 25 mm thick
- Grain size
- clayey siltstone
- Composition
- Clayey siltstone; red bands colored by hematite
Where rockhounds find zebra rock
Classic worldwide localities
- Lake Argyle, south of Kununurra, Western Australia
Field-hunting tip
Where it forms: Johnny Cake Member of the early Ediacaran Ranford Formation. If you start seeing hematite in float, you are in the right ground.



