Catherine Island (New Zealand)
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Catherine Island (New Zealand)
Catherine Island is an island in the Gold Arm of Taiporoporo / Charles Sound in the South Island of New Zealand New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island count .... References Uninhabited islands of New Zealand Islands of Fiordland Fiordland National Park {{Fiordland-geo-stub ...
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Fiordland National Park
Fiordland National Park occupies the southwest corner of the South Island of New Zealand. It is by far the largest of the 13 national parks in New Zealand, with an area of , and a major part of the Te Wahipounamu World Heritage Site. The park is administered by the Department of Conservation. of Fiordland were set aside as a national reserve in 1904, following suggestions by then-future Prime Minister Thomas Mackenzie and Southland Commissioner of Crown Lands, John Hay, that the region should be declared a national park. The area had already become a destination for trampers, following the opening up of the Milford Track from Lake Te Anau to Milford Sound in 1889 by New Zealand explorers Quintin McKinnon and Donald Sutherland, which received significant publicity from a 1908 article in the London Spectator describing it as the "Finest Walk in the World". The Fiordland "public reserve" was created as a park administered by the Department of Lands and Survey - in practical t ...
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Regions Of New Zealand
New Zealand is divided into sixteen regions () for local government in New Zealand, local government purposes. Eleven are administered by regional councils (the top tier of local government), and five are administered by Unitary authority#New Zealand, unitary authorities, which are territorial authorities of New Zealand, territorial authorities (the second tier of local government) that also perform the functions of regional councils. The Chatham Islands#Government, Chatham Islands Council is not a region but is similar to a unitary authority, authorised under its own legislation. Current regions History and statutory basis The regional councils are listed in Part 1 of Schedule 2 of the Local Government Act 2002 (New Zealand), Local Government Act 2002, along with reference to the ''New Zealand Gazette, Gazette'' notices that established them in 1989. The Act requires regional councils to promote sustainable developmentthe social, economic, environmental and cultural well-bei ...
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Southland Region
Southland ( mi, Murihiku) is New Zealand's southernmost region. It consists mainly of the southwestern portion of the South Island and Stewart Island/Rakiura. It includes Southland District, Gore District and the city of Invercargill. The region covers over 3.1 million hectares and spans over 3,400 km of coast. History The earliest inhabitants of Murihiku (meaning "the last joint of the tail") were Māori of the Waitaha iwi, followed later by Kāti Māmoe and Kāi Tahu. Waitaha sailed on the Uruao waka, whose captain Rakaihautū named sites and carved out lakes throughout the area. The Takitimu Mountains were formed by the overturned Kāi Tahu waka Tākitimu. Descendants created networks of customary food gathering sites, travelling seasonally as needed, to support permanent and semi-permanent settlements in coastal and inland regions. In later years, the coastline was a scene of early extended contact between Māori and Europeans, in this case sealers, whalers ...
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Taiporoporo / Charles Sound
Taiporoporo / Charles Sound is a fiord of the South Island of New Zealand. It is one of the fiords that form the coast of Fiordland. Geography Extending south from Milford Sound / Piopiotahi, Taiporoporo / Charles Sound is the sixth fiord in Fiordland, on the southwest coast of New Zealand's South Island, situated between Taitetimu / Caswell Sound to the north and Hinenui / Nancy Sound to the south. At a length of just under , it is the second shortest standalone fiord in Fiordland (after Te Rā / Dagg Sound). Despite this, Taiporoporo has the deepest sill depth of the northern fiords, with a depth of before deepening to a maximum depth of in the main basin of the fiord. The main body of the fiord extends in a southeasterly direction from the outer Fiordland coast, before splitting into two arms of similar length in its upper reaches: the Emelius Arm (to the north) and the Gold Arm (to the south). The latter of these is protected by the Kahukura (Gold Arm) Marine Reserve. O ...
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South Island
The South Island, also officially named , is the larger of the two major islands of New Zealand in surface area, the other being the smaller but more populous North Island. It is bordered to the north by Cook Strait, to the west by the Tasman Sea, and to the south and east by the Pacific Ocean. The South Island covers , making it the world's 12th-largest island. At low altitude, it has an oceanic climate. The South Island is shaped by the Southern Alps which run along it from north to south. They include New Zealand's highest peak, Aoraki / Mount Cook at . The high Kaikōura Ranges lie to the northeast. The east side of the island is home to the Canterbury Plains while the West Coast is famous for its rough coastlines such as Fiordland, a very high proportion of native bush and national parks, and the Fox and Franz Josef Glaciers. The main centres are Christchurch and Dunedin. The economy relies on agriculture and fishing, tourism, and general manufacturing and services. ...
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New Zealand
New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island country by area, covering . New Zealand is about east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The country's varied topography and sharp mountain peaks, including the Southern Alps, owe much to tectonic uplift and volcanic eruptions. New Zealand's capital city is Wellington, and its most populous city is Auckland. The islands of New Zealand were the last large habitable land to be settled by humans. Between about 1280 and 1350, Polynesians began to settle in the islands and then developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. In 1840, representatives of the United Kingdom and Māori chiefs ...
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Uninhabited Islands Of New Zealand
The list of uninhabited regions includes a number of places around the globe. The list changes year over year as human beings migrate into formerly uninhabited regions, or migrate out of formerly inhabited regions. List As a group, the list of uninhabited places are called the "nonecumene". This is a special geography term which means the uninhabited area of the world. * Virtually all of the Ocean *Virtually all of Antarctica *Most of The Arctic *Most of Greenland *Most of The Sahara * Antipodes Islands * Ashmore and Cartier Islands * Bajo Nuevo Bank * Baker Island * Ball's Pyramid * Balleny Islands * Big Major Cay * Bouvet Island * Much of the interior of Brazil * Caroline Island * Clipperton Island * The semi-arid regions and deserts of Australia * Devon Island * Much of Eastern Oregon * Elephant Island * Elobey Chico * Ernst Thälmann Island * Much of Fiordland, New Zealand * Goa Island * Gough Island * Hans Island * Harmil * Hashima Island * Hatutu * Heard Island a ...
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Islands Of Fiordland
An island or isle is a piece of subcontinental land completely surrounded by water. Very small islands such as emergent land features on atolls can be called islets, skerries, cays or keys. An island in a river or a lake island may be called an eyot or ait, and a small island off the coast may be called a holm. Sedimentary islands in the Ganges Delta are called chars. A grouping of geographically or geologically related islands, such as the Philippines, is referred to as an archipelago. There are two main types of islands in the sea: continental islands and oceanic islands. There are also artificial islands (man-made islands). There are about 900,000 official islands in the world. This number consists of all the officially-reported islands of each country. The total number of islands in the world is unknown. There may be hundreds of thousands of tiny islands that are unknown and uncounted. The number of sea islands in the world is estimated to be more than 200,000. The t ...
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