The Antipodes Islands seen from the north
Position relative to New Zealand and other outlying islands
|Location||860 kilometres (534 mi) southeast of Stewart Island/Rakiura|
|Major islands||Antipodes Island, Bollons Island|
|Area||22 km2 (8.5 sq mi)|
|Highest elevation||366 m (1,201 ft)|
|Highest point||Mount Galloway|
|Population||0 (as of 2006)|
The Antipodes Islands (from Greek αντίποδες - antipodes) are inhospitable volcanic islands to the south of—and territorially part of—New Zealand. They lie 860 kilometres (534 mi) to the southeast of Stewart Island/Rakiura.
Ecologically, the islands are part of the Antipodes Subantarctic Islands tundra ecoregion. The islands are inscribed on the UNESCO World Heritage List, together with other sub-Antarctic New Zealand islands. The island group is a nature reserve and there is no general public access.
The island group was originally called the "Penantipodes" meaning "next to the antipodes", because it lies near to the antipodes of London. Over time the name has been shortened to "Antipodes" leaving some to suppose its European discoverers had not realised its global location. This misapprehension persists. In fact, the island's antipodes are situated on the territory of the French village Gatteville-le-Phare, near Cherbourg.
The volcanic Antipodes Islands lie 860 kilometres southwest of Stewart Island/Rakiura. They consist of a main island (Antipodes Island), area 20 km2 (7.7 sq mi), surrounded by a series of small offshore islands and rocks. These islands include Bollons Island, at 2 km2 (0.77 sq mi) the second largest in the group, 1200 metres to the northeast of the main island's North Cape, and the nearby smaller Archway Island; Leeward Island, situated just off the centre of the main island's east coast (to which it is connected by a rocky bar at low tide); the two Windward Islands, situated 800 metres apart, the easternmost of which is 600 metres to the immediate north of Cave Point, the main island's westernmost point; and the tiny Orde Lees Islet, located close to the main island's northwestern shore. Numerous small islets and stacks further surround the coast of the main island.
The islands are steep, and cliffs and rocky reefs line the majority of the coasts. The highest point, in the north of the main island, is Mount Galloway, at 366 m (1,201 ft), which also forms part of the group's most recently active volcano. Mount Waterhouse, to Galloway's southwest, also reaches over 360 metres. Several other heights on the main island reach above 200 metres, as does the highest point of Bollons Island. A ridge of peaks, the Reliance Ridge, runs along the main island's south cast. Several small streams run from the slopes of the main island's peaks, with the largest of these being the Dougall Stream, which runs northeast from the eastern slopes of Mount Waterhouse to reach the east coast not far from its closest point to Leeward Island. The Ringdove Stream runs east along the northern flanks of the Reliance Ridge to reach the large, rocky Ringdove Bay in the southeast of the main island. A further prominent stream runs southwest from the northwestern slopes of Mount Waterhouse to reach Stack Bay to the south of the Cave Point Peninsula, and a fourth runs north from the slopes of Mount Galloway, reaching the sea to the west of North Cape, close to Reef Point.
There is no archaeological evidence of human visitation prior to European discovery of the islands. Descriptions of a shard of early Polynesian pottery having been discovered 2 ft 6 in below the surface on the main island in 1886, and housed in the collections of the Museum of New Zealand Te Papa Tongarewa, are unsubstantiated. The Museum has not been able to locate such a shard in its collection, and the original reference to the object in the Museum's collection documentation indicates no reference to Polynesian influences.
|This section does not cite any references or sources. (May 2013)|
The island group was first charted in 1800 by Captain Henry Waterhouse of the British ship HMS Reliance. In 1803 Waterhouse's brother-in-law George Bass applied to Governor Philip Gidley King of New South Wales for a fishing monopoly from a line bisecting southern New Zealand from Dusky Sound to the Otago Harbour to cover all the lands and seas to the south, including the Antipodes Islands, probably because he knew the latter were home to large populations of fur seals. Bass sailed from Sydney to the south that year and was never heard of again but his information led to a sealing boom at the islands in 1805 to 1807.
At one time eighty men were present; there was a battle between American and British-led gangs and a single cargo of more than 80,000 skins—one of the greatest ever shipped from Australasia—was on-sold in Canton for one pound sterling a skin, a multi-million dollar return in modern terms. Prominent Sydney merchants such as Simeon Lord, Henry Kable and James Underwood were engaged in the trade as well as the Americans Daniel Whitney and Owen Folger Smith. William W. Stewart, who claimed to have charted Stewart Island, and probably William Tucker who started the retail trade in preserved Maori heads, were present during the boom. After 1807, sealing was occasional and cargoes small, no doubt because the animals had been all but exterminated.
A much later attempt to establish cattle on the islands was short-lived (as were the cattle). When the ship Spirit of the Dawn (with a crew of 16) foundered off the main island's coast in 1893, the eleven surviving crew spent nearly three months living as castaways on the island, living on raw muttonbirds, mussels and roots for 87 days before gaining the attention of the government steamer Hinemoa by a flag made from their sail.
A well-supplied castaway depot was available on the other end of the island, but the survivors' weak condition and the island's mountainous terrain prevented them from searching for depots. The depot was found and used by the crew of the President Felix Faure wrecked in Anchorage bay in 1908. The last wreck at the Antipodes was the yacht Totorore with the loss of two lives, Gerry Clark and Roger Sale, in June 1999.
Flora and fauna
The flora of the islands has been recorded in detail, and includes megaherbs. The islands are also home to numerous bird species including the endemic Antipodes Snipe and Antipodes Island Parakeet, as well as several albatrosses, petrels and penguins, including half of the world population of Erect-crested Penguins. Antipodes Island has introduced house mice.
Important Bird Area
The Antipodes group has been identified as an Important Bird Area (IBA) by BirdLife International because of its significance as a breeding site for several species of seabirds. The seabirds are Southern Rockhopper and Erect-crested Penguins, Antipodean, Black-browed, Light-mantled and White-capped Albatrosses, and Northern Giant, Grey and White-chinned Petrels.
As with many other islands, introduced rodents have caused problems by preying on the indigenous wildlife. A "Million Dollar Mouse" campaign was launched in 2012 to raise funds for an eradication programme.
- Composite Antarctic Gazetteer
- List of Antarctic and sub-Antarctic islands
- List of islands of New Zealand
- New Zealand sub-antarctic islands
- Territorial claims in Antarctica
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