Within the gully-eroded areas of the Copley–Leigh Creek commons, ephemeral clay pinnacles are preserved. Their butte-like form may result from chenopod roots stabilising sections of the eroding margins.



Within the gully-eroded areas of the Copley–Leigh Creek commons, ephemeral clay pinnacles are preserved. Their butte-like form may result from chenopod roots stabilising sections of the eroding margins.



On the western side of the Blinman diapir in Parachilna Gorge, the ‘Badlands’ are created by rapid erosion of soft rocks.

