Great ocean road australia

The Great Ocean Road is a 243 km coastal highway in southwestern Australia, renowned for its limestone cliffs and the Twelve Apostles.

About this subject

The Great Ocean Road is located in the state of Victoria, Australia, stretching 243 kilometers between the towns of Torquay and Allansford. Built between 1919 and 1932 by returned soldiers from World War I, the road serves as a living war memorial, honoring those who served. It is considered the world's largest war memorial. The highway winds along dramatic cliffs, offering spectacular views of the Southern Ocean. One of the most iconic attractions is the Twelve Apostles, limestone rock formations rising from the sea, the result of continuous erosion over millennia. Originally formed by the fragmentation of the coastline, these limestone stacks are a classic example of coastal geomorphology. Unfortunately, the number of apostles is diminishing due to natural erosion; as of 2023, only seven remain. Other notable points include Loch Ard Gorge, site of a historic shipwreck in 1878, and London Arch (formerly London Bridge), which partially collapsed in 1990, temporarily stranding two tourists. The region also encompasses Port Campbell National Park, preserving native flora and fauna, including koalas and kangaroos. The Great Ocean Road attracts about 6 million visitors per year, making it one of Australia's most iconic tourist destinations. The road is a landmark of engineering and tourism, uniquely combining natural and human history.

Frequently Asked Questions

What is the total length of the Great Ocean Road?

The Great Ocean Road is 243 kilometers long, connecting Torquay to Allansford on the southwestern coast of Victoria, Australia.

Why is the Great Ocean Road considered a war memorial?

The road was built by returned soldiers from World War I as a living memorial, officially dedicated to those who served and died in the conflict.

How many of the Twelve Apostles are still standing?

Currently only seven apostles remain, as natural erosion continues to topple the limestone stacks. The most recent collapse occurred in 2005.