Moeraki Boulders - Nature’s Marvel on the New Zealand Coastline
Discover the Moeraki Boulders, New Zealand’s natural marvel on the South Island. These spherical stones are scattered along Koekohe Beach, providing a unique and mystical coastal experience.
Top Attractions at the Moeraki Boulders
The Boulders Themselves
The Moeraki Boulders are naturally occurring, spherical stones that sit along Koekohe Beach. These boulders, formed millions of years ago, are a result of calcite build-up around a core, making them a unique geological phenomenon.
Koekohe Beach
The boulders rest on Koekohe Beach, offering a stunning coastal walk that provides panoramic views of the Pacific Ocean. It’s an ideal stop for photographers and nature enthusiasts alike.
Myths and Legends
In Māori mythology, the Moeraki Boulders are believed to be the remains of food baskets and gourds that washed ashore from the wreck of the Araiteuru canoe, which is a significant part of Māori legend.
Self-Drive Tours Featuring the Moeraki Boulders
Include a visit to the Moeraki Boulders in your South Island road trip itinerary.
Here are some tours that pass through or near this location
12 Day Ultimate Southern Adventure
Discover Wanaka’s scenic beauty along with other South Island highlights such as Milford Sound and Franz Josef Glacier on this ultimate 12-day journey.
11 Day Scenic South Island
Wanaka is a key stop on this 11-day scenic journey that explores the best of the South Island, from lakes to mountain vistas.
Best Time to Visit the Moeraki Boulders
Weather and Seasonal Events
The best time to visit the Moeraki Boulders is during low tide, as many of the boulders are submerged when the tide is high. Plan your visit accordingly to get up close to these geological wonders.
Moeraki Boulders Facts - Did You Know?
The Moeraki Boulders are as large as 2 metres in diameter, with some of the smaller ones measuring just 0.5 metres across.
The spherical boulders were formed over 60 million years ago through a natural process called concretion, which happens when minerals harden around a central core.
These boulders are an internationally protected landmark due to their unique formation and cultural significance.