Franklin Mountains, New Zealand
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Franklin Mountains, New Zealand
The Franklin Mountains of New Zealand are a group of peaks in the southwestern area of the South Island, located between Bligh Sound and Lake Te Anau, within 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 i .... References Mountain ranges of Fiordland Southern Alps {{Fiordland-geo-stub ...
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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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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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Bligh Sound
Bligh may refer to: Surname * Anna Bligh (born 1960), Australian politician * George Miller Bligh (1780–1834), British naval officer, son of Richard Rodney Bligh * Jasmine Bligh (1913–1991), British television presenter * Richard Bligh (1780–1838), British barrister * Richard Rodney Bligh (1737–1821), British naval officer * Thomas Bligh (1685–1775), British army general * Thomas Bligh (1654–1710), (1654–1710) Irish politician * William Bligh (1754–1817), British naval officer whose command of the HMS ''Bounty'' was challenged by 1789 mutiny Members of the family of the Earl of Darnley, an English aristocratic family associated with cricket in Kent: * John Bligh, 1st Earl of Darnley (1687–1728), son of Thomas Bligh (1654–1710) * Edward Bligh, 2nd Earl of Darnley (1715–1747), peer * John Bligh, 3rd Earl of Darnley (1719–1781), parliamentarian * John Bligh, 4th Earl of Darnley (1767–1831), peer and cricketer * General Edward Bligh (1769–1840), soldier, p ...
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Lake Te Anau
Lake Te Anau is in the southwestern corner of the South Island of New Zealand. The lake covers an area of , making it the second-largest lake by surface area in New Zealand (after Lake Taupō) and the largest in the South Island. It is the largest lake in Australasia by fresh water volume. The main body of the lake runs north-south, and is 65 km in length. Three large fiords form arms to the lake on its western flank: North Fiord, Middle Fiord and South Fiord. These are the only inland fiords that New Zealand has, the other 14 are out on the coast. Several small islands lie in the entrance to Middle Fiord, which forks partway along its length into northwest and southwest arms. The surface of the lake is at an altitude of 210 m. It has a maximum depth of 417 m, so much of its bed lies below sea level, with the deepest part of the lake being 226 metres below sea level. Several rivers feed the lake, of which the most important is the Eglinton River, which joins the lake from ...
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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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Mountain Ranges Of Fiordland
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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