The name "Otago" is the local southern Māori dialect pronunciation of "Ōtākou", the name of the Māori village near the entrance to Otago Harbour.[6][7] 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 harbour, established by the Weller Brothers in 1831, which lies close to Otakou. The upper harbour 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.
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.
Initial settlement was concentrated on the port and city, then expanded, notably to the south-west, where the fertile Taieri Plains offered good farmland.[9] The 1860s saw rapid commercial expansion after Gabriel Read discovered gold at Gabriel's Gully near Lawrence, and the Central Otago goldrush ensued.[10]
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.[11]
New Zealand's first university, the University of Otago, was founded in 1869 as the provincial university in Dunedin.[12]
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,[13] 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
Autumn 2004 in OtagoAerial photo of Beaumont area in Otago, looking southwest. State Highway 8 runs from left to right across the photo (only visible in the right half), and crosses the Clutha River just below centre.Mount Aspiring / Tititea is New Zealand's highest mountain outside the Aoraki / Mount Cook region.
Beginning in the west, the geography of Otago consists of high alpine mountains. The highest peak in Otago (and highest outside the Aoraki / Mount Cook area) is Mount Aspiring / Tititea,[14] 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, Wānaka, and Hāwea form the sources of the Clutha / Matau-au, the largest river (by discharge) 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.
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,[14] 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 (offset by the Alpine Fault) and even in New Caledonia, 3,500 km (2,200 mi) away.[15]
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.[16]
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 northwesterlyföhn 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.[17]
Population
A map showing population density in the Otago Region at the 2006 census.
Otago Region covers 31,186.16 km2 (12,041.04 sq mi).[18] The population is 254,600 as of June 2023,[1][1] which is approximately 4.9 percent of New Zealand's total population of 5.2 million. The population density is 8.2 people per km2. About 41.7 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.[19]
Otago Region had a population of 225,186 at the 2018 New Zealand census, an increase of 22,716 people (11.2%) since the 2013 census, and an increase of 31,383 people (16.2%) since the 2006 census. There were 85,665 households, comprising 110,970 males and 114,219 females, giving a sex ratio of 0.97 males per female. The median age was 38.2 years (compared with 37.4 years nationally), with 37,275 people (16.6%) aged under 15 years, 51,702 (23.0%) aged 15 to 29, 99,123 (44.0%) aged 30 to 64, and 37,086 (16.5%) aged 65 or older.
Ethnicities were 86.9% European/Pākehā, 8.7% Māori, 2.7% Pasifika, 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 chose not to answer the census's question about religious affiliation, 55.8% had no religion, 33.4% were Christian, 0.2% had Māori religious beliefs, 0.8% were Hindu, 0.7% were Muslim, 0.7% were Buddhist and 2.1% had other religions.
Of those at least 15 years old, 42,816 (22.8%) people had a bachelor's or higher degree, and 31,122 (16.6%) people had no formal qualifications. The median income was $30,000, compared with $31,800 nationally. 26,988 people (14.4%) earned over $70,000 compared to 17.2% nationally. The employment status of those at least 15 was that 92,418 (49.2%) people were employed full-time, 30,396 (16.2%) were part-time, and 6,048 (3.2%) were unemployed.[21]
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 Tahuiwi or tribe. Other significant ethnic minorities include Asians, Pacific Islanders, Africans, Latin Americans and Middle Easterners.[24] Otago's early waves of settlement, especially during and immediately after the gold rush of the 1860s, included a substantial minority of southern (Guangdong) Chinese settlers, and a smaller but also prominent number of people from Lebanon.[25] 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.[26]
Otago is represented by four parliamentaryelectorates. Dunedin and nearby towns are represented by the Dunedin electorate, held by Rachel Brooking, and the Taieri electorate, occupied by Ingrid Leary. Both MPs are members of the Labour Party, and Dunedin has traditionally been a Labour stronghold. Since 2008 the rest of Otago has been divided between the large rural electorates of Waitaki, which also includes some of the neighbouring Canterbury Region, and Clutha-Southland, which also includes most of the rural part of the neighbouring Southland Region. The Waitaki electorate has traditionally been a National Party stronghold and is currently held by Miles Anderson. The Southland electorate, also a National Party stronghold, is currently represented by Joseph Mooney. The earlier Otago electorate existed from 1978 to 2008, when it was split and merged into Waitaki and Clutha-Southland.
Two list MPs are based in Dunedin – Michael Woodhouse of the National Party and Rachel Brooking of the Labour 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 electorates 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 Te Pati Maori Party MP Takuta Ferris.
Ngāi Tahu governance
Three of the 18 Ngāi TahuRūnanga (councils) are based in the Otago Region. Each one is centred on a coastal marae, namely Ōtākou, Moeraki and Puketeraki at Karitane.[27] There is also the Arai Te Uru Marae in Dunedin.[28]
Economy
The subnational gross domestic product (GDP) of Otago was estimated at NZ$14.18 billion[29] in the year to March 2020, 4.38% of New Zealand's national GDP. The regional GDP per capita was estimated at $58,353 in the same period. In the year to March 2018, primary industries contributed $1.25 billion (9.8%) to the regional GDP, goods-producing industries contributed $2.38 billion (18.6%), service industries contributed $8.05 billion (63.0%), and taxes and duties contributed $1.10 billion (8.6%).[30]
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 wine 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.[31]
Education
Otago has numerous rural primary schools, several small town primary and secondary schools, and some larger schools in Dunedin. Most are state schools which do not charge tuition, except for international students.[32][33] Some are state integrated schools, former private schools with a special character based on a religious or philosophical belief that has been integrated into the state system, but still charge "attendance dues" to cover the building and maintenance of school buildings. These schools are not owned by the government, but otherwise they like state schools cannot charge fees for tuition of domestic students but may request a donation. As Dunedin was founded by Presbyterian Scottish settlers there are a Presbyterian girls' and boys' school in the city. Unlike other major cities in New Zealand, Dunedin does not have any private intermediate or high schools, as all remaining private intermediate and high schools have been integrated into the state system.
^Jones, Daniel (2003) [1917], Peter Roach; James Hartmann; Jane Setter (eds.), English Pronouncing Dictionary, Cambridge: Cambridge University Press, ISBN3-12-539683-2
^Peter Entwisle, Behold the Moon: The European Occupation of the Dunedin District 1770–1848, Dunedin, NZ: Port Daniel Press, 1998 (ISBN0-473-05591-0), appendix 1 pp.136–139.
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