Norfolk Island located on terrain feature Norfolk Island
Norfolk Island (, locally ; Norfuk: Norf'k Ailen) is an  external territory of Australia located in the Pacific Ocean between New Zealand and New Caledonia, 1,412 kilometres (877 mi) directly east of Australia's Evans Head and about 900 kilometres (560 mi) from Lord Howe Island. Together with the neighbouring Phillip Island and Nepean Island, the three islands collectively form the Territory of Norfolk Island. At the 2021 census, it had 2,188 inhabitants living on a total area of about 35 km2 (14 sq mi). Its capital is Kingston.Geography
The Territory of Norfolk Island is located in the South Pacific Ocean, east of the Australian mainland. Norfolk Island itself is the main island of the island group that the territory encompasses and is located at 29°02′S 167°57′E. It has an area of 34.6 square kilometres (13.4 sq mi), with no large-scale internal bodies of water and 32 km (20 mi) of coastline. Norfolk was formed from several volcanic eruptions between 3.1 and 2.3 million years ago.
The island's highest point is Mount Bates reaching 319 metres (1,047 feet) above sea level, located in the northwest quadrant of the island. The majority of the terrain is suitable for farming and other agricultural uses. Phillip Island, the second largest island of the territory, is located at 29°07′S 167°57′E, seven kilometres (4.3 miles) south of the main island.
The coastline of Norfolk Island consists, to varying degrees, of cliff faces. A downward slope exists towards Slaughter Bay and Emily Bay, the site of the original colonial settlement of Kingston. There are no safe harbour facilities on Norfolk Island, with loading jetties existing at Kingston and Cascade Bay. All goods not domestically produced are brought in by ship, usually to Cascade Bay. Emily Bay, protected from the Pacific Ocean by a small coral reef, is the only safe area for recreational swimming, although surfing waves can be found at Anson and Ball Bays.
The climate is subtropical and mild, with little seasonal differentiation. The island is the eroded remnant of a basaltic volcano active around 2.3 to 3 million years ago, with inland areas now consisting mainly of rolling plains. It forms the highest point on the Norfolk Ridge, part of the submerged continent Zealandia.
The area surrounding Mount Bates is preserved as the Norfolk Island National Park. The park, covering around 10% of the land of the island, contains remnants of the forests which originally covered the island, including stands of subtropical rainforest.