- Department of Conservation - Mackenzie Basin tramping tracks
|This article about a river in Canterbury, New Zealand is a stub. You can help Wikipedia by expanding it.|
|This article about a river in Canterbury, New Zealand is a stub. You can help Wikipedia by expanding it.|
The South Island officially named Te Waipounamu, is the larger of the two major islands of New Zealand in surface area. It is bordered to the north by Cook Strait, to the west by the Tasman Sea, to the south and east by the Pacific Ocean; the South Island covers 150,437 square kilometres. It has a temperate climate, it has a 32 percent larger landmass than the North Island, as a result is nicknamed the "mainland" of New Zealand by South Island residents, but only 23 percent of New Zealand's 4.9 million inhabitants live there. In the early stages of European settlement of the country, the South Island had the majority of the European population and wealth due to the 1860s gold rushes; the North Island population overtook the South in the early 20th century, with 56 percent of the population living in the North in 1911, the drift north of people and businesses continued throughout the century. In the 19th century, some maps named the South Island as Middle Island or New Munster, the name South Island or New Leinster was used for today's Stewart Island/Rakiura.
In 1907 the Minister for Lands gave instructions to the Land and Survey Department that the name Middle Island was not to be used in future. "South Island will be adhered to in all cases". Although the island had been known as the South Island for many years, in 2009 the New Zealand Geographic Board found that, along with the North Island, the South Island had no official name. After a public consultation, the board named the island South Island or Te Waipounamu in October 2013. Said to mean "the Water of Greenstone", this name evolved from Te Wāhi Pounamu "the Place Of Greenstone"; the island is known as Te Waka a Māui which means "Māui's Canoe". In some Māori legends, the South Island existed first, as the boat of Maui, while the North Island was the fish that he caught. In prose, the two main islands of New Zealand are called the North Island and the South Island, with the definite article, it is normal to use the preposition in rather than on, for example "Christchurch is in the South Island", "my mother lives in the South Island".
Maps, headings and adjectival expressions use South Island without "the". Charcoal drawings can be found on limestone rock shelters in the centre of the South Island, with over 500 sites stretching from Kaikoura to North Otago; the drawings are estimated to be between 500 and 800 years old, portray animals and fantastic creatures stylised reptiles. Some of the birds pictured are long extinct, including Haast's eagles, they were drawn by early Māori, but by the time Europeans arrived, local Māori did not know the origins of the drawings. Early inhabitants of the South Island were the Waitaha, they were absorbed via marriage and conquest by the Kāti Māmoe in the 16th century. Kāti Māmoe were in turn absorbed via marriage and conquest by the Kāi Tahu who migrated south in the 17th century. While today there is no distinct Kāti Māmoe organisation, many Kāi Tahu have Kāti Māmoe links in their whakapapa and in the far south of the island. Around the same time a group of Māori migrated to Rekohu, where, in adapting to the local climate and the availability of resources, they evolved into a separate people known as the Moriori with its own distinct language — related to the parent culture and language in mainland New Zealand.
One notable feature of the Moriori culture, an emphasis on pacifism, proved disadvantageous when Māori warriors arrived in the 1830s aboard a chartered European ship. In the early 18th century, Kāi Tahu, a Māori tribe who originated on the east coast of the North Island, began migrating to the northern part of the South Island. There they and Kāti Māmoe fought Ngāi Rangitāne in the Wairau Valley. Ngāti Māmoe ceded the east coast regions north of the Clarence River to Kāi Tahu. Kāi Tahu continued conquering Kaikoura. By the 1730s, Kāi Tahu had settled including Banks Peninsula. From there they spread further south and into the West Coast. In 1827-1828 Ngāti Toa under the leadership of Te Rauparaha attacked Kāi Tahu at Kaikoura. Ngāti Toa visited Kaiapoi, ostensibly to trade; when they attacked their hosts, the well-prepared Kāi Tahu killed all the leading Ngāti Toa chiefs except Te Rauparaha. Te Rauparaha returned to his Kapiti Island stronghold. In November 1830 Te Rauparaha persuaded Captain John Stewart of the brig Elizabeth to carry him and his warriors in secret to Akaroa, where by subterfuge they captured the leading Kāi Tahu chief, Te Maiharanui, his wife and daughter.
After destroying Te Maiharanui's village they killed them. John Stewart, though arrested and sent to trial in Sydney as an accomplice to murder escaped conviction. In the summer of 1831–32 Te Rauparaha attacked the Kaiapoi pā. Kaiapoi was engaged in a three-month siege by Te Rauparaha, during which his men sapped the pā, they attacked Kāi Tahu on Banks Peninsula and took the pā at Onawe. In 1832-33 Kāi Tahu retaliated under the leadership of Tūhawaiki and others, attacking Ngāti Toa at Lake Grassmere. Kāi Tahu prevailed, killed many Ngāti Toa, although Te Rauparaha again escaped. Fighting continued with Kāi Tahu maintaining the upper hand. Ngāti Toa never again made a major incursion into Kāi Tahu territory. By 1839 Kāi Tahu and Ngāti Toa established peace and Te Rauparaha released the Kāi Tahu captives he held. Formal marriages between the leading families in the two tribes sealed the peace; the first Europeans known to reach the South Island were the crew o
Canterbury is a region of New Zealand, located in the central-eastern South Island. The region covers an area of 44,508 square kilometres, is home to a population of 624,000; the region in its current form was established in 1989 during nationwide local government reforms. The Kaikoura District joined the region in 1992 following the abolition of the Nelson-Marlborough Regional Council. Christchurch, the South Island's largest city and the country's third-largest urban area, is the seat of the region and home to 65 percent of the region's population. Other major towns and cities include Timaru, Ashburton and Rolleston. In 1848, Edward Gibbon Wakefield, a Briton, John Robert Godley, an Anglo-Irish aristocrat, founded the Canterbury Association to establish an Anglican colony in the South Island; the colony was based upon theories developed by Wakefield while in prison for eloping with a woman not-of-age. Due to ties to the University of Oxford, the Canterbury Association succeeded in raising sufficient funds and recruiting middle-class and upper-class settlers.
In April 1850, a preliminary group led by Godley landed at Port Cooper—modern-day Lyttelton Harbour—and established a port and shops in preparation for the main body of settlers. In December 1850, the first wave of 750 settlers arrived at Lyttelton in a fleet of four ships. Following 1850, the province's economy developed with the introduction of sheep farming; the Canterbury region's tussock plains in particular were suitable for extensive sheep farming. Since they were valued by settlers for their meat and wool, there were over half a million sheep in the region by the early 1850s. By the 1860s, this figure had risen to three million. During this period, the architect Benjamin Mountfort designed many civic and ecclesiastical buildings in the Gothic Revival style; the Canterbury Province was formed in 1853 following the passing of the New Zealand Constitution Act 1852. It was formed from part of New Munster Province and covered the middle part of the South Island, stretching from the east coast to the west coast.
The province was abolished, along with other provinces of New Zealand, when the Abolition of the Provinces Act came into force on 1 Nov 1876. The modern Canterbury Region has different boundaries in the north, where it includes some districts from the old Nelson Province; the area administered by the Canterbury Regional Council consists of all the river catchments on the east coast of the South Island from that of the Clarence River, north of Kaikoura, to that of the Waitaki River, in South Canterbury. It is New Zealand's largest region by area, with an area of 45,346 km2. Canterbury was traditionally bounded in the north by the Conway River, to the west by the Southern Alps, to the south by the Waitaki River; the area is divided into North Canterbury, Mid Canterbury, South Canterbury and Christchurch City. Canterbury is home to 624,000 people according to Statistics New Zealand's June 2018, 13 percent of New Zealand's population, it the second most populous region in New Zealand. The median age of Canterbury's population is two years above the New Zealand median.
Around 15.5 percent of the population is aged 65 or over while 18.7 percent is aged under 15. There are 97.5 males for every hundred females in Canterbury. At the 2013 Census of Population and Dwellings, 86.9 percent of Cantabrians identified as of European ethnicity, 8.1 percent as Māori, 6.9 percent as Asian, 2.5 percent as Pacific Peoples, 0.8 percent as Middle Eastern/Latin American/African, 2.0 percent as another ethnicity. Just under 20 percent of Canterbury's population was born overseas, compared to 25 percent for New Zealand as a whole; the British Isles remains the largest region of origin, accounting for 36.5 percent of the overseas-born population in Canterbury. Around a quarter of Canterbury's overseas-born population at the 2013 Census had been living in New Zealand for less than five years, 11 percent had been living in New Zealand for less than two years. Around 49.7 percent of Cantabrians affiliate with Christianity and 3.3 percent affiliate with non-Christian religions, while 44.5 percent are irreligious.
Anglicanism is the largest Christian denomination in Canterbury with 14.8 percent affiliating, while Catholicism is the second-largest with 12.7 percent affiliating. The Canterbury region's economy is diversified into agriculture, fishing, forestry and energy resources such as coal and hydroelectricity, its agriculture sector is diversified into dairy farming, sheep farming and horticulture viticulture. The strength of the region's agricultural economy is displayed every November at the Canterbury A&P Show; the show coincides with Cup Week. During the interwar period, agricultural productivity was boosted by the introduction of mechanization and the improvement of seed stocks. Canterbury is New Zealand's main producer of cereal crops such as wheat and oats; as of 2002, the region produced 60.7% of the nation's supply of wheat, 51.1% of its barley stocks and 43.7% of its supply of oats. The region's viticulture industry was established by French settlers in Akaroa. Since wine-growing is concentrated into two regions: Waipara and Burnham.
Lake Ohau is a glacial lake in the Mackenzie Basin of New Zealand's South Island. It is fed by the Hopkins and Dobson rivers, which have their headwaters in the Southern Alps, has its outflow in the Ohau River, which itself feeds into the Waitaki River hydroelectric project. Ohau is the smallest of three parallel lakes running north-south along the northern edge of the Mackenzie Basin, it covers 60 km². The Ohau ski field is located close to the western shore of the lake, as is its service town, Lake Ohau Alpine Village; the lake forms part of the traditional boundary between Otago and Canterbury regions, Otago's northernmost point being the headwaters of the Hopkins River. The lake lies in the northwestern part of the Waitaki District within the southern part of the Canterbury region. Lake Ohau is on the route of the Alps to Ocean Cycle Trail, constructed in the years after approval in 2010; the trail runs along the Lake up to Lake Ohau Lodge, climbs up the Tarnbrae Track before a flowing descent to Quailburn Road.
Media related to Lake Ohau at Wikimedia Commons Ski Ohau Pictures of Ohau
New Zealand is a sovereign island country in the southwestern Pacific Ocean. The country geographically comprises two main landmasses—the North Island, the South Island —and around 600 smaller islands. New Zealand is situated some 2,000 kilometres east of Australia across the Tasman Sea and 1,000 kilometres south of the Pacific island areas of New Caledonia and Tonga; because of its remoteness, it was one of the last lands to be settled by humans. During its long period of isolation, New Zealand developed a distinct biodiversity of animal and plant life; the country's varied topography and its sharp mountain peaks, such as the Southern Alps, owe much to the tectonic uplift of land and volcanic eruptions. New Zealand's capital city is Wellington. Sometime between 1250 and 1300, Polynesians settled in the islands that were named New Zealand and developed a distinctive Māori culture. In 1642, Dutch explorer Abel Tasman became the first European to sight New Zealand. In 1840, representatives of the United Kingdom and Māori chiefs signed the Treaty of Waitangi, which declared British sovereignty over the islands.
In 1841, New Zealand became a colony within the British Empire and in 1907 it became a dominion. Today, the majority of New Zealand's population of 4.9 million is of European descent. Reflecting this, New Zealand's culture is derived from Māori and early British settlers, with recent broadening arising from increased immigration; the official languages are English, Māori, NZ Sign Language, with English being dominant. A developed country, New Zealand ranks in international comparisons of national performance, such as quality of life, education, protection of civil liberties, economic freedom. New Zealand underwent major economic changes during the 1980s, which transformed it from a protectionist to a liberalised free-trade economy; the service sector dominates the national economy, followed by the industrial sector, agriculture. Nationally, legislative authority is vested in an elected, unicameral Parliament, while executive political power is exercised by the Cabinet, led by the prime minister Jacinda Ardern.
Queen Elizabeth II is the country's monarch and is represented by a governor-general Dame Patsy Reddy. In addition, New Zealand is organised into 11 regional councils and 67 territorial authorities for local government purposes; the Realm of New Zealand includes Tokelau. New Zealand is a member of the United Nations, Commonwealth of Nations, ANZUS, Organisation for Economic Co-operation and Development, ASEAN Plus Six, Asia-Pacific Economic Cooperation, the Pacific Community and the Pacific Islands Forum. Dutch explorer Abel Tasman sighted New Zealand in 1642 and named it Staten Land "in honour of the States General", he wrote, "it is possible that this land joins to the Staten Land but it is uncertain", referring to a landmass of the same name at the southern tip of South America, discovered by Jacob Le Maire in 1616. In 1645, Dutch cartographers renamed the land Nova Zeelandia after the Dutch province of Zeeland. British explorer James Cook subsequently anglicised the name to New Zealand. Aotearoa is the current Māori name for New Zealand.
It is unknown whether Māori had a name for the whole country before the arrival of Europeans, with Aotearoa referring to just the North Island. Māori had several traditional names for the two main islands, including Te Ika-a-Māui for the North Island and Te Waipounamu or Te Waka o Aoraki for the South Island. Early European maps labelled the islands North and South. In 1830, maps began to use North and South to distinguish the two largest islands and by 1907 this was the accepted norm; the New Zealand Geographic Board discovered in 2009 that the names of the North Island and South Island had never been formalised, names and alternative names were formalised in 2013. This set the names as North Island or Te Ika-a-Māui, South Island or Te Waipounamu. For each island, either its English or Māori name can be used. New Zealand was one of the last major landmasses settled by humans. Radiocarbon dating, evidence of deforestation and mitochondrial DNA variability within Māori populations suggest New Zealand was first settled by Eastern Polynesians between 1250 and 1300, concluding a long series of voyages through the southern Pacific islands.
Over the centuries that followed, these settlers developed a distinct culture now known as Māori. The population was divided into iwi and hapū who would sometimes cooperate, sometimes compete and sometimes fight against each other. At some point a group of Māori migrated to Rēkohu, now known as the Chatham Islands, where they developed their distinct Moriori culture; the Moriori population was all but wiped out between 1835 and 1862 because of Taranaki Māori invasion and enslavement in the 1830s, although European diseases contributed. In 1862 only 101 survived, the last known full-blooded Moriori died in 1933; the first Europeans known to have reached New Zeala
The Hopkins River is in the central South Island of New Zealand. It flows south for 40 kilometres from the Southern Alps into the northern end of Lake Ohau in the Mackenzie Country, its headwaters, on the southern slopes of Mount Hopkins, form the northernmost point of Otago, the river's braided valley is part of the border between Otago and Canterbury. The river's main tributary is the Dobson River
A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position. A common choice of coordinates is latitude and elevation. To specify a location on a plane requires a map projection; the invention of a geographic coordinate system is credited to Eratosthenes of Cyrene, who composed his now-lost Geography at the Library of Alexandria in the 3rd century BC. A century Hipparchus of Nicaea improved on this system by determining latitude from stellar measurements rather than solar altitude and determining longitude by timings of lunar eclipses, rather than dead reckoning. In the 1st or 2nd century, Marinus of Tyre compiled an extensive gazetteer and mathematically-plotted world map using coordinates measured east from a prime meridian at the westernmost known land, designated the Fortunate Isles, off the coast of western Africa around the Canary or Cape Verde Islands, measured north or south of the island of Rhodes off Asia Minor.
Ptolemy credited him with the full adoption of longitude and latitude, rather than measuring latitude in terms of the length of the midsummer day. Ptolemy's 2nd-century Geography used the same prime meridian but measured latitude from the Equator instead. After their work was translated into Arabic in the 9th century, Al-Khwārizmī's Book of the Description of the Earth corrected Marinus' and Ptolemy's errors regarding the length of the Mediterranean Sea, causing medieval Arabic cartography to use a prime meridian around 10° east of Ptolemy's line. Mathematical cartography resumed in Europe following Maximus Planudes' recovery of Ptolemy's text a little before 1300. In 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, England as the zero-reference line; the Dominican Republic voted against the motion, while Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911.
In order to be unambiguous about the direction of "vertical" and the "horizontal" surface above which they are measuring, map-makers choose a reference ellipsoid with a given origin and orientation that best fits their need for the area they are mapping. They choose the most appropriate mapping of the spherical coordinate system onto that ellipsoid, called a terrestrial reference system or geodetic datum. Datums may be global, meaning that they represent the whole Earth, or they may be local, meaning that they represent an ellipsoid best-fit to only a portion of the Earth. Points on the Earth's surface move relative to each other due to continental plate motion and diurnal Earth tidal movement caused by the Moon and the Sun; this daily movement can be as much as a metre. Continental movement can be up to 10 m in a century. A weather system high-pressure area can cause a sinking of 5 mm. Scandinavia is rising by 1 cm a year as a result of the melting of the ice sheets of the last ice age, but neighbouring Scotland is rising by only 0.2 cm.
These changes are insignificant if a local datum is used, but are statistically significant if a global datum is used. Examples of global datums include World Geodetic System, the default datum used for the Global Positioning System, the International Terrestrial Reference Frame, used for estimating continental drift and crustal deformation; the distance to Earth's center can be used both for deep positions and for positions in space. Local datums chosen by a national cartographical organisation include the North American Datum, the European ED50, the British OSGB36. Given a location, the datum provides the latitude ϕ and longitude λ. In the United Kingdom there are three common latitude and height systems in use. WGS 84 differs at Greenwich from the one used on published maps OSGB36 by 112 m; the military system ED50, used by NATO, differs from about 120 m to 180 m. The latitude and longitude on a map made against a local datum may not be the same as one obtained from a GPS receiver. Coordinates from the mapping system can sometimes be changed into another datum using a simple translation.
For example, to convert from ETRF89 to the Irish Grid add 49 metres to the east, subtract 23.4 metres from the north. More one datum is changed into any other datum using a process called Helmert transformations; this involves converting the spherical coordinates into Cartesian coordinates and applying a seven parameter transformation, converting back. In popular GIS software, data projected in latitude/longitude is represented as a Geographic Coordinate System. For example, data in latitude/longitude if the datum is the North American Datum of 1983 is denoted by'GCS North American 1983'; the "latitude" of a point on Earth's surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the Equator and to each other; the North Pole is 90° N. The 0° parallel of latitude is designated the Equator, the fun