Otago
Otago is a region of New Zealand located in the southern half of the South Island administered by the Otago Regional Council. It has an area of approximately, making it the country's third largest local government region. Its population was
The name "Otago" is an Anglicisation of "Otakou", the name of the Māori village near the entrance to the harbour. The exact meaning of the term is disputed, with common translations being "isolated village" and "place of red earth", the latter referring to the reddish-ochre clay which is common in the area around Dunedin. "Otago" is also the old name of the European settlement on the Otago Harbour, established by the Weller Brothers in 1831, which lies close to the modern harbourside community of Otakou. The place later became the focus of the Otago Association, an offshoot of the Free Church of Scotland, notable for its adoption of the principle that ordinary people, not the landowner, should choose the ministers.
Major centres include Dunedin, Oamaru, Balclutha, Alexandra, and the major tourist centres Queenstown and Wanaka. Kaitangata in South Otago is a prominent source of coal. The Waitaki and Clutha rivers provide much of the country's hydroelectric power. Vineyards and wineries have been developed in the Central Otago wine region. Some parts of the area originally covered by Otago Province are now administered by either Canterbury Regional Council or Southland Regional Council.
History
The Otago settlement, an outgrowth of the Free Church of Scotland, materialised in March 1848 with the arrival of the first two immigrant ships from Greenock on the Firth of Clyde—the John Wickliffe and the Philip Laing. Captain William Cargill, a veteran of the Peninsular War, was the secular leader: Otago citizens subsequently elected him to the office of provincial Superintendent after the New Zealand provinces were created in 1853. The Otago Province was the whole of New Zealand from the Waitaki River south, including Stewart Island and the sub-Antarctic islands. It included the territory of the later Southland Province and also the much more extensive lands of the modern Southland Region., a historic mining town
Initial settlement was concentrated on the port and city, then expanded, notably to the south-west, where the fertile Taieri Plains offered good farmland. The 1860s saw rapid commercial expansion after Gabriel Read discovered gold at Gabriel's Gully near Lawrence, and the Central Otago goldrush ensued. Veterans of goldfields in California and Australia, plus many other fortune-seekers from Europe, North America and China, poured into the then Province of Otago, eroding its Scottish Presbyterian character. Further gold discoveries at Clyde and on the Arrow River around Arrowtown led to a boom, and Otago became for a period the cultural and economic centre of New Zealand. New Zealand's first daily newspaper, the Otago Daily Times, originally edited by Julius Vogel, dates from this period.
, New Zealand's oldest university
New Zealand's first university, the University of Otago, was founded in 1869 as the provincial university in Dunedin.
The Province of Southland separated from Otago Province and set up its own Provincial Council at Invercargill in 1861. After difficulties ensued, Otago re-absorbed it in 1870. Its territory is included in the southern region of the old Otago Province which is named after it and is now the territory of the Southland region.
The provincial governments were abolished in 1876 when the Abolition of the Provinces Act came into force on 1 November 1876, and were replaced by other forms of local authority, including counties. Two in Otago were named after the Scottish independence heroes Wallace and Bruce. From this time the national limelight gradually shifted northwards.
Geography
Beginning in the west, the geography of Otago consists of high alpine mountains. The highest peak in Otago is Mount Aspiring / Tititea, which is on the Main Divide. From the high mountains the rivers discharge into large glacial lakes. In this part of Otago glacial activity – both recent and very old – dominates the landscape, with large 'U' shaped valleys and rivers which have high sediment loads. River flows also vary dramatically, with large flood flows occurring after heavy rain. Lakes Wakatipu, Wanaka, and Hawea form the sources of the Clutha, the largest river in New Zealand. The Clutha flows generally to the southeast through Otago and discharges near Balclutha. The river has been used for hydroelectric power generation, with large dams at Clyde and Roxburgh. The traditional northern boundary of the region, the Waitaki River, is also heavily utilised for hydroelectricity, though the region's current official boundaries put much of that river's catchment in Canterbury., where Roaring Meg joins the Kawarau River, in central Otago
The country's fourth-longest river, the Taieri, also has both its source and outflow in Otago, rising from rough hill country and following a broad horseshoe-shaped path, north, then east, and finally southeast, before reaching the Pacific Ocean. Along its course it forms two notable geographic features – the broad high valley of the Strath-Taieri in its upper reaches, and the fertile Taieri Plains as it approaches the ocean.
Travelling east from the mountains, the Central Otago drylands predominate. These are Canterbury-Otago tussock grasslands dominated by the block mountains, upthrust schist mountains. In contrast to Canterbury, where the Northwest winds blow across the plains without interruption, in Otago the block mountains impede and dilute the effects of the Nor'wester.
The main Central Otago centres, such as Alexandra and Cromwell, are found in the intermontane basins between the block mountains. The schist bedrock influence extends to the eastern part of Otago, where remnant volcanics mark its edge. The remains of the most spectacular of these are the Miocene volcanics centred on Otago Harbour. Elsewhere, basalt outcrops can be found along the coast and at other sites.
Comparatively similar terrain exists in the high plateau land of the Maniototo Plain, which lies to the east of Central Otago, close to the upper reaches of the Taieri River. This area is sparsely populated, but of historical note for its importance during the Central Otago Gold Rush of the 1860s. The townships of Ranfurly and Naseby lie in this area.
In the southeastern corner of Otago lies The Catlins, an area of rough hill country which geologically forms part of the Murihiku terrane, an accretion which extends inland through the Hokonui Hills in the Southland region. This itself forms part of a larger system known as the Southland Syncline, which links to similar formations in Nelson and even in New Caledonia, away. The Catlins ranges are strike ridges composed of Triassic and Jurassic sandstones, mudstones and other related sedimentary rocks, often with a high incidence of feldspar. Fossils of the late and middle Triassic Warepan and Kaihikuan stages are found in the area.
Climate
Weather conditions vary enormously across Otago, but can be broken into two broad types: the coastal climate of the coastal regions and the more continental climate of the interior.Coastal regions of Otago are subject to the alternating warm and dry/cool and wet weather patterns common to the interannual Southern oscillation. The Southern Hemisphere storm track produces an irregular short cycle of weather which repeats roughly every week, with three or four days of fine weather followed by three or four days of cooler, damp conditions. Drier conditions are often the result of the northwesterly föhn wind, which dries as it crosses the Southern Alps. Wetter air is the result of approaching low-pressure systems which sweep fronts over the country from the southwest. A common variant in this pattern is the centring of a stationary low-pressure zone to the southeast of the country, resulting in long-lasting cool, wet conditions. These have been responsible for several notable historical floods, such as the "hundred year floods" of October 1878 and October 1978.
Typically, winters are cool and wet in the extreme south areas and snow can fall and settle to sea level in winter, especially in the hills and plains of South Otago. More Central and Northern Coastal areas winter is sunnier and drier. Summers, by contrast, tend to be warm and dry, with temperatures often reaching the high 20s and low 30s Celsius.
In Central Otago cold frosty winters are succeeded by hot dry summers. Central Otago's climate is the closest approximation to a continental climate anywhere in New Zealand. This climate is part of the reason why Central Otago vineyards are successful in this region. This inland region is one of the driest regions in the country, sheltered from prevailing rain-bearing weather conditions by the high mountains to the west and hills of the south. Summers can be hot, with temperatures often approaching or exceeding 30 degrees Celsius; winters, by contrast, are often bitterly cold – the township of Ranfurly in Central Otago holds the New Zealand record for lowest temperature with a reading of −25.6 °C on 18 July 1903.
Population
The population of Otago is, which is approximately percent of New Zealand's total population of million. About percent of the population resides in the Dunedin urban area—the region's main city and the country's sixth largest urban area. For historical and geographical reasons, Dunedin is usually regarded as one of New Zealand's four main centres. Unlike other southern centres, Dunedin's population has not declined since the 1970s, largely due to the presence of the University of Otago – and especially its medical school – which attracts students from all over New Zealand and overseas.Other significant urban centres in Otago with populations over 1,000 include: Queenstown, Oamaru, Wanaka, Port Chalmers, Cromwell, Alexandra, Balclutha, Milton and Mosgiel. Between 1996 and 2006, the population of the Queenstown Lakes District grew by 60% due to the region's booming tourism industry.
| Urban area | Population since the 2013 census, and an increase of 31,383 people since the 2006 census. There were 85,665 households. There were 110,970 males and 114,219 females, giving a sex ratio of 0.97 males per female. Of the total population, 37,275 people were aged up to 15 years, 51,702 were 15 to 29, 99,123 were 30 to 64, and 37,086 were 65 or older. Figures may not add up to the total due to rounding. Ethnicities were 86.9% European/Pākehā, 8.7% Māori, 2.7% Pacific peoples, 7.1% Asian, and 3.1% other ethnicities. People may identify with more than one ethnicity. The percentage of people born overseas was 21.7, compared with 27.1% nationally. Although some people objected to giving their religion, 55.8% had no religion, 33.4% were Christian, and 4.6% had other religions. Of those at least 15 years old, 42,816 people had a bachelor or higher degree, and 31,122 people had no formal qualifications. The median income was $30,000. The employment status of those at least 15 was that 92,418 people were employed full-time, 30,396 were part-time, and 6,048 were unemployed. The majority of the population of European lineage is of Scottish stock—the descendants of early Scottish settlers from the early 19th century. Other well-represented European groups include those of English, Irish, and Dutch descent. A large proportion of the Māori population are from the Ngāi Tahu iwi or tribe. Other significant ethnic minorities include Asians, Pacific Islanders, Africans, Latin Americans and Middle Easterners. Otago's early waves of settlement, especially during and immediately after the gold rush of the 1860s, included a substantial minority of southern Chinese settlers, and a smaller but also prominent number of people from Lebanon. The region's Jewish population also experienced a small influx at this time. The early and middle years of the twentieth century saw smaller influxes of immigrants from several mainland European countries, most notably the Netherlands. In line with the region's Scottish heritage, Presbyterianism is the largest Christian denomination with 17.1 percent affiliating, while Catholicism is the second-largest denomination with 11.5 percent affiliating. PoliticsLocal governmentThe seat of the Otago Regional Council is in Dunedin. The Council is chaired by Marian Hobbs of the Labour Party as of 2019.There are five territorial authorities in Otago:
One list MP is based in Dunedin – Michael Woodhouse of the National Party. One-time Labour Party Deputy Leader David Parker is a former MP for the Otago electorate and currently a list MP. Under the Māori seats system, Otago is also part of the large Te Tai Tonga electorate, which covers the entire South Island and surrounding islands, and is currently held by Labour Party MP Rino Tirikatene. Ngāi Tahu governanceThree of the 18 Ngāi Tahu Rūnanga are based in the Otago Region. All of which are centred at coastal marae, Ōtākou, Moeraki and Puketeraki at Karitane. There is also the Arai Te Uru Marae in Dunedin.EconomyThe subnational gross domestic product of Otago was estimated at NZ$13.58 billion in the year to March 2019, 4.5% of New Zealand's national GDP. The regional GDP per capita was estimated at $57,974 in the same period. In the year to March 2018, primary industries contributed $1.25 billion to the regional GDP, goods-producing industries contributed $2.38 billion, service industries contributed $8.05 billion, and taxes and duties contributed $1.10 billion.Otago has a mixed economy. Dunedin is home to manufacturing, publishing and technology-based industries. Rural economies have been reinvigorated in the 1990s and 2000s: in Clutha district, farms have been converted from sheep to more lucrative dairying. Vineyard planting and production remained modest until the middle of the 1990s when the New Zealand wine industry began to expand rapidly. The Central Otago wine region produces award-winning wines made from varieties such as the Pinot noir, Chardonnay, Sauvignon blanc, Merlot and Riesling grapes. It has an increasing reputation as New Zealand's leading Pinot noir region. |