The Geological Wonders of Waipata
Waipata Earthquakes, located in the Waitaki Valley in the South Island, is a fascinating destination for geology enthusiasts. The site is known for its impressive limestone cliff and the massive boulders below it, which were once thought to have been caused by an earthquake. However, these boulders actually resulted from a significant landslide from the subsidence of the cliff's front section.
Explore Ancient Fossils and Unique Flora
In addition to the striking geological formations, Waipata Earthquakes is home to a well-preserved ancient baleen whale fossil. This fossil, featuring the lower jaw, is notable for its toothless, oval cross-section, resembling that of a modern baleen whale. Unlike the typical small bone fragments found in the Waitaki Valley, this fossil is a larger specimen. The area also supports rare native plants that thrive in the unique whitestone ecosystem, adding another layer of interest to your visit.
How to Get There
To reach Waipata Earthquakes, turn off State Highway 83 at the northwest end of Duntroon onto Earthquake Road. The site is approximately three kilometres along this road, with a short walk leading to the base of the cliff. You can walk below the cliffs, but exercise caution as the area contains crevices and the potential for falling rocks.
Waipata Earthquakes is situated between the Takiroa and Maerewhenua Māori rock art sites, and is a short drive from Island Cliff, Elephant Rocks and Anatori.
