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Waiheke Island AI simulator
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Hub AI
Waiheke Island AI simulator
(@Waiheke Island_simulator)
Waiheke Island
Waiheke Island is the second-largest island (after Great Barrier Island) in the Hauraki Gulf of New Zealand. Its ferry terminal in Matiatia Bay at the western end is 21.5 km (13.4 mi) from the central-city terminal in Auckland.
It is the most populated island in the gulf, with 9,310 permanent residents, and the third most populous island in New Zealand (behind the two main islands). An additional estimated 3,400 people have second homes or holiday homes on the island. It is more densely populated than the North and South Islands. It is the most accessible island in the gulf, with regular passenger and car-ferry services, a helicopter operator based on the island, and other air links.[better source needed]
In November 2015, Lonely Planet rated Waiheke Island the fifth-best region in the world to visit in 2016.
The island is off the coast of the North Island. It is 19.3 km (12.0 mi) in length from west to east, varies in width from 0.64 to 9.65 km (0.40 to 6.00 mi), and has a surface area of 92 km2 (36 sq mi). The coastline is 133.5 km (83.0 mi), including 40 km (25 mi) of beaches. The port of Matiatia at the western end is 17.7 km (11.0 mi) from Auckland and the eastern end is 21.4 km (13.3 mi) from Coromandel. The much smaller Tarahiki Island lies 3 km (1.9 mi) to the east.
The island is very hilly with few flat areas, the highest point being Maunganui at 231 m (758 ft).
Approximately 17,000 years ago during the Last Glacial Maximum when sea levels were over 100 metres lower than present day levels, Waiheke Island was landlocked to the North Island, surrounded by a vast coastal plain where the Hauraki Gulf / Tīkapa Moana exists today. Sea levels began to rise 7,000 years ago, after which Waiheke became an island separated from the rest of New Zealand.
Much of eastern Waiheke island is the remains of a Miocene volcano of the Kiwitahi Group, which erupted approximately 15 million years ago. There are locations of interest to geologists: an argillite outcrop in Ōmiha, and a chert stack at the end of Pohutukawa Point, considered "one of the best exposures of folded chert in Auckland City".
There are many scenic beaches, including:
Waiheke Island
Waiheke Island is the second-largest island (after Great Barrier Island) in the Hauraki Gulf of New Zealand. Its ferry terminal in Matiatia Bay at the western end is 21.5 km (13.4 mi) from the central-city terminal in Auckland.
It is the most populated island in the gulf, with 9,310 permanent residents, and the third most populous island in New Zealand (behind the two main islands). An additional estimated 3,400 people have second homes or holiday homes on the island. It is more densely populated than the North and South Islands. It is the most accessible island in the gulf, with regular passenger and car-ferry services, a helicopter operator based on the island, and other air links.[better source needed]
In November 2015, Lonely Planet rated Waiheke Island the fifth-best region in the world to visit in 2016.
The island is off the coast of the North Island. It is 19.3 km (12.0 mi) in length from west to east, varies in width from 0.64 to 9.65 km (0.40 to 6.00 mi), and has a surface area of 92 km2 (36 sq mi). The coastline is 133.5 km (83.0 mi), including 40 km (25 mi) of beaches. The port of Matiatia at the western end is 17.7 km (11.0 mi) from Auckland and the eastern end is 21.4 km (13.3 mi) from Coromandel. The much smaller Tarahiki Island lies 3 km (1.9 mi) to the east.
The island is very hilly with few flat areas, the highest point being Maunganui at 231 m (758 ft).
Approximately 17,000 years ago during the Last Glacial Maximum when sea levels were over 100 metres lower than present day levels, Waiheke Island was landlocked to the North Island, surrounded by a vast coastal plain where the Hauraki Gulf / Tīkapa Moana exists today. Sea levels began to rise 7,000 years ago, after which Waiheke became an island separated from the rest of New Zealand.
Much of eastern Waiheke island is the remains of a Miocene volcano of the Kiwitahi Group, which erupted approximately 15 million years ago. There are locations of interest to geologists: an argillite outcrop in Ōmiha, and a chert stack at the end of Pohutukawa Point, considered "one of the best exposures of folded chert in Auckland City".
There are many scenic beaches, including:
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