Awarua Point
Awarua Point is located on the southwestern coast of New Zealand's South Island, at the northern end of Big Bay, north of Milford Sound, and north of the mouth of the Hollyford River. Traditionally, Awarua Point is regarded as the end of Fiordland Fiordland is a geographical region of New Zealand in the south-western corner of the South Island, comprising the westernmost third of Southland. Most of Fiordland is dominated by the steep sides of the snow-capped Southern Alps, deep lake ... and the start of the West Coast region, although the boundary of Fiordland National Park is located farther south at the northern end of Martins Bay. The New Zealand Ministry for Culture and Heritage gives a translation of "two streams" for ''Awarua''. See also * Awarua Plains References Headlands of the West Coast, New Zealand Westland District {{WestCoastNZ-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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. ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Big Bay (Southland)
Big Bay, also known as Awarua Bay, is a deep indentation in the southwestern coast of New Zealand's South Island, 40 kilometres north of Milford Sound and immediately to the north of Martins Bay. The bay is eight kilometres in width, and extends eight kilometres into the South Island, making an almost square indentation in the island's coastline. Its northern end is Awarua Point. Immediately beyond Long Reef, the rocky point at the southern end, is the mouth of the Hollyford River and Martins Bay. Big Bay has a sandy beach named Three Mile Beach. The Awarua River enters the bay at the northern end of the beach. The mouth of the Awarua River is the western end of the boundary between the West Coast Regional Council area and the Southland Regional Council area. It was formerly the boundary between Canterbury Province and Otago Province from when they were created in 1853. Three Mile Beach, the Awarua River and Waiuna Lagoon are within the boundary of Southland region. Awarua Point ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Milford Sound
Milford Sound / Piopiotahi is a fiord in the south west of New Zealand's South Island within Fiordland National Park, Piopiotahi (Milford Sound) Marine Reserve, and the Te Wahipounamu World Heritage site. It has been judged the world's top travel destination in an international survey (the ''2008 Travelers' Choice Destinations Awards'' by TripAdvisor) and is acclaimed as New Zealand's most famous tourist destination."Real Journeys rapt with Kiwi Must-Do's" ''Scoop'', 13 February 2007. had previously called it the eighth Wonder of ...
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Hollyford River
The Hollyford River / Whakatipu Kā Tuka is in the southwest of the South Island of New Zealand. It runs for through Fiordland, its sources being close to the Homer Tunnel and in Gertrude Valley in the southern Darran Mountains. At first, the river flows southeast and east, coming as close as 1km to the east-west divide of the South Island, before continuing north through the glacier-formed Hollyford Valley. Near the end, the river passes through Lake McKerrow before reaching Martins Bay on the coast of the Tasman Sea north of Milford Sound. The Hollyford Track follows the river's course. Part of the river's course is traditionally regarded as the boundary between the Southland Southland may refer to: Places Canada * Dunbar–Southlands, Vancouver, British Columbia New Zealand * Southland Region, a region of New Zealand * Southland County, a former New Zealand county * Southland District, part of the wider Southland Re ... and Otago regions, however, current maps ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Fiordland
Fiordland is a geographical region of New Zealand in the south-western corner of the South Island, comprising the westernmost third of Southland. Most of Fiordland is dominated by the steep sides of the snow-capped Southern Alps, deep lakes, and its steep, glacier-carved and now ocean-flooded western valleys. The name "Fiordland" comes from a variant spelling of the Scandinavian word for this type of steep valley, "fjord". The area of Fiordland is dominated by, and very roughly coterminous with, Fiordland National Park, New Zealand's largest National Park. Due to the often steep terrain and high amount of rainfall supporting dense vegetation, the interior of the Fiordland region is largely inaccessible. As a result, Fiordland was never subjected to notable logging operations, and even attempts at whaling, seal hunting, and mining were on a small scale and short-lived, partly also because of the challenging weather. Today, Fiordland contains by far the greatest extent of u ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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West Coast, New Zealand
The West Coast ( mi, Te Tai Poutini, lit=The Coast of Poutini, the Taniwha) is a regions of New Zealand, region of New Zealand on the west coast of the South Island that is administered by the West Coast Regional Council, and is known co-officially as Te Tai Poutini. It comprises the Territorial authorities of New Zealand, territorial authorities of Buller District, Grey District and Westland District. The principal towns are Westport, New Zealand, Westport, Greymouth and Hokitika. The region, one of the more remote areas of the country, is also the most sparsely populated. With a population of just 32,000 people, Te Tai Poutini is the least populous region in New Zealand, and it is the only region where the population is declining. The region has a rich and important history. The land itself is ancient, stretching back to the Carboniferous period; this is evident by the amount of carboniferous materials naturally found there, especially coal. First settled by Ngāi Tahu, Kāi T ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Ministry For Culture And Heritage
The Ministry for Culture and Heritage (MCH; ) is the department of the New Zealand Government responsible for supporting the arts, culture, built heritage, sport and recreation, and broadcasting sectors in New Zealand and advising government on such. History The Ministry of Cultural Affairs had been created in 1991; prior to this, the Department of Internal Affairs (DIA) had provided oversight and support for arts and culture functions. MCH was founded in 1999 with the merger of the former Ministry of Cultural Affairs and the history and heritage functions of the DIA, as well as some functions from the Department of Conservation and Ministry of Commerce. The purpose of the merger of functions and departments was to create a coherent, non-fragmented overview of the cultural and heritage sector, rather than spreading services and functions across several departments. Minister for Cultural Affairs Marie Hasler oversaw the transition of functions into the new agency. Opposition La ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Awarua Plains
The Awarua Plain is a large area of wetland to the east of Bluff, New Zealand. Covering an area of around 600 km², the plain stretches for 35 kilometres along the coast of Foveaux Strait. This stretch of coast includes the peninsula of Tiwai Point, Awarua Bay, the Waituna Lagoon, and Toetoes Bay. The Mataura River is the major river responsible for the presence of the Awarua Plain; along with the Ōreti River, it is a remnant of the rivers from the Ice Ages that formed the Southland Plains (Murihiku). In addition, several small streams enter Foveaux Strait along this stretch of coast, mainly via Awarua Bay and Waituna Lagoon. The New Zealand Ministry for Culture and Heritage gives a translation of "two streams" for ''Awarua''. Demographics The Awarua Plains statistical area covers within Southland District. It had an estimated population of as of with a population density of people per km2. Awarua Plains had a population of 1,020 at the 2018 New Zealand census, a ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Headlands Of The West Coast, New Zealand
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |