Omarama Clay Cliffs Cliff

The Omarama Clay Cliffs are an erosional landform near the township of Omarama in Otago on New Zealand’s South Island. The site is composed of steep pinnacles and ridges that rise to roughly 30 metres in places.

The cliffs form a narrow band of sculpted earth with sharp gullies and spires; a short, unsealed access track leads from a roadside car park to viewing areas. The formations are visually striking at close range and popular with photographers and short-walk visitors.

They were created by the erosion of soft sedimentary deposits, shaped over time by rain and wind. The features remain active and continue to change slowly as erosion progresses.

Located near the small service town of Omarama, the cliffs sit within the broader Mackenzie/Otago landscape of tussock country and dry river terraces in the South Island.

• Height and access: Formations reach about 30 metres in height and are best viewed from the marked car park and short walking track.

From the town of Omarama (on State Highway 8), follow signs for the Clay Cliffs viewing area-it’s about a 10-15 minute drive north of the township. There is a sealed pull-off and a short walking track from the car park to the viewing platform; the site is visible from the parking area but short trails allow closer views. Gravel roads around the site can be rough; two-wheel-drive cars are generally fine in good weather.

• Go at sunrise for the clearest light and to avoid the midday winds that can kick up dust and make the cliffs hazy for photos.
• Wear sturdy shoes-footing on the clay slope is loose and a fall can be slippery.
• Respect private farm fences: some viewing points are on farmland; use the official car park off State Highway 8 to avoid trespass.