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  2. Great Ocean Road - Wikipedia

    en.wikipedia.org/wiki/Great_Ocean_Road

    The Great Ocean Road is an Australian National Heritage-listed 240-kilometre (150 mi) ... Great Ocean Road Map An Interactive Map showcasing 150+ attractions, ...

  3. Bay of Islands Coastal Park - Wikipedia

    en.wikipedia.org/wiki/Bay_of_Islands_Coastal_Park

    Bay of Islands Coastal Park is a 32 kilometres (20 miles) long coastal reserve located in Victoria, Australia on the Great Ocean Road between Peterborough and Warrnambool. [1] [2] Lookout areas with parking are provided at the Bay of Martyrs, the Bay of Islands, Three Mile Beach and Childers Cove. [3]

  4. The Twelve Apostles (Victoria) - Wikipedia

    en.wikipedia.org/wiki/The_Twelve_Apostles_(Victoria)

    The Twelve Apostles are a collection of limestone stacks off the shore of Port Campbell National Park, by the Great Ocean Road in Victoria, Australia. The Twelve Apostles are located on the traditional lands of the Eastern Maar peoples. [1] Their proximity to one another has made the site a popular tourist attraction.

  5. The Grotto, Victoria - Wikipedia

    en.wikipedia.org/wiki/The_Grotto,_Victoria

    The Grotto. The Grotto) is a sinkhole geological formation and tourist attraction, found on the Great Ocean Road outside Port Campbell in Victoria, AustraliaWooden steps wind down the cliff face to the bottom, providing visibility of the sea beyond a pool at low tide.

  6. Island Archway - Wikipedia

    en.wikipedia.org/wiki/Island_Archway

    The Island Archway was part of a series of free-standing limestone formations on the Great Ocean Road that includes the Twelve Apostles. As early as January 1990, another rock arch on this coast, the inner arch of the London Bridge, had collapsed. The stability of these cliffs is short-lived in geological terms.

  7. London Bridge (Victoria) - Wikipedia

    en.wikipedia.org/wiki/London_Bridge_(Victoria)

    The arch is a significant tourist attraction along the Great Ocean Road near Port Campbell in Victoria. The stack was formed by a gradual process of erosion, and until 1990 formed a complete double-span natural bridge. The formation in 1961, prior to its collapse in 1990

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