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  1. Geography. The islands lie within 29° to 31.5° south latitude and 178° to 179° west longitude, 800–1,000 km (500–620 mi) northeast of New Zealand's North Island, and a similar distance southwest of Tonga. The total area of the islands is 33.6 km 2 (12.97 sq mi).

  2. Kermadec Islands, volcanic island group in the South Pacific Ocean, 600 mi (1,000 km) northeast of Auckland, New Zealand; they are a dependency of New Zealand. They include Raoul (Sunday), Macauley, and Curtis islands and l’Esperance Rock and have a total land area of 13 sq mi (34 sq km).

    • The Editors of Encyclopaedia Britannica
  3. Kermadec Islands. Located in the Northland region. View saved (0) The Kermadec Islands Nature Reserve and Marine Reserve, located about 1,000 km northeast of New Zealand, is the most remote area managed by DOC and can only be visited with a special permit. View boundaries on MarineMate app.

  4. The Kermadec Islands are a group of small volcanic islands, 800–1,000 kilometres north-east of the North Island. A nature reserve, they are uninhabited, except for a Department of Conservation field station on Raoul Island, the main island. Geology and climate

  5. Kermadec Islands map. The Kermadec Islands are the tiny emergent part of a chain of submarine volcanoes that define the Kermadec ridge. In political terms the Kermadecs are important for New Zealand as they define the northern extent of both the Exclusive Economic Zone (EEZ) and the Extended Continental Shelf (ECS).

  6. Facts and practical information. The Kermadec Islands, located in the Northern Islands region of New Zealand, are a remote and pristine group of volcanic islands that offer a unique and unparalleled natural experience.

  7. The Kermadec Islands are nature reserves protected under the 1977 Reserves Act. The Act requires all visitors landing on the island to obtain and comply with an entry permit. Entry permits are only issued for Raoul island, and stipulate what places visitors can access and when. Raoul Island is an active volcanic site.

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