Otago

Otago is a region of New Zealand in the south of the South Island administered by the Otago Regional Council. It has an area of approximately 32,000 square kilometres (12,000 sq mi), making it the country's third largest local government region. Its population was 219,200 in the June 2016.

The name "Otago" is an old Māori southern dialect word (the North Island dialect equivalent is "Otakou"), introduced to the south by Europeans in the 1840s. 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 high-minded adoption of the principle that ordinary people, not the landowner, should choose the ministers.

Major centres include Dunedin (the principal city), Oamaru (made famous by Janet Frame), 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. Some parts of the area originally covered by Otago Province are now administered by either Canterbury Regional Council or Southland Regional Council.

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.

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 1852. 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. 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 round 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 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 (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.

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 (offset by the Alpine Fault) and even in New Caledonia, 3,500 km (2,200 mi) 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.

Population

The population of Otago is 219,200, which is approximately 4.7 percent of New Zealand’s total population of 4.7 million. About 54.1 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 due to the presence of the University of Otago 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, 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 areas in Otago Urban area Population
(June 2016) % of region Dunedin 118,500 54.1% Queenstown 14,300 6.5% Oamaru 13,850 6.3% Wanaka 7,850 3.6% Alexandra 5,300 2.4% Cromwell 4,670 2.1% Balclutha 4,010 1.8% Arrowtown 2,830 1.3% Milton 1,940 0.9% Waikouaiti 1,150 0.5%

1. ^ Includes Mosgiel and Port Chalmers.

Approximately 80% of the region’s population is of European lineage with the majority being 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. Maori comprise approximately 7% of the population with a large proportion being 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 (Guangdong) 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.

Around 46.2 percent of Otago's population affiliate with Christianity and 3.2 percent affiliate with non-Christian religions, while 48.3 percent are irreligious. 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