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Top Attractions in Canterbury

Christchurch

Christchurch is the largest city in the South Island of New Zealand, and the country's third-most populous urban area. It lies one third of the way down the South Island's east coast, just north of Banks Peninsula, which itself, since 2006, lies within the formal limits of Christchurch. The population of Christchurch City at the 5 March 2013 census was 341,469. The city was named by the Canterbury Association, which settled the surrounding province of Canterbury. The name of Christchurch was agreed on at the first meeting of the association on 27 March 1848. It was suggested by John Robert Godley, who had attended Christ Church, Oxford. Some early writers called the town Christ Church, but it was recorded as Christchurch in the minutes of the management committee of the association. Christchurch became a city by Royal Charter on 31 July 1856, making it officially the oldest established city in New Zealand. The river that flows through the centre of the city was named Avon at the request of the pioneering Deans brothers to commemorate the Scottish Avon, which rises in the Ayrshire hills near what was their grandfathers' farm and flows into the Clyde. The usual Māori name for Christchurch is Ōtautahi . This was originally the name of a specific site by the Avon River near present-day Kilmore Street and the Christchurch Central Fire Station. The site was a seasonal dwelling of Ngāi Tahu chief Te Potiki Tautahi, whose main home was Port Levy on Banks Peninsula. The Ōtautahi name was adopted in the 1930s. Prior to that the Ngāi Tahu generally referred to the Christchurch area as Karaitiana, a transliteration of the English word Christian. The city's name is often abbreviated by New Zealanders to Chch. In New Zealand Sign Language, the city's name is the fingerspelled letter C signed twice, with the second to the right of the first, while mouthing "Christchurch".

Lake Pukaki

Lake Pukaki is the largest of three roughly parallel alpine lakes running north-south along the northern edge of the Mackenzie Basin on New Zealands South Island. The others are Lakes Tekapo and Ohau. All three lakes were created when the terminal moraines of receding glaciers blocked their respective valleys, forming moraine-dammed lakes. The glacial feed to the lakes gives them a distinctive blue colour, created by glacial flour, the extremely finely ground rock particles from the glaciers. Lake Pukaki covers an area of 178.7 km², and the surface elevation of the lake normally ranges from 518.2 to 532 metres above sea level. The lake is fed at its northern end by the braided Tasman River, which has its source in the Tasman and Hooker Glaciers, close to Aoraki/Mount Cook. Good views of the mountain, 70 kilometres to the north can be had from the southern shore of the lake. The lake is now part of the Waitaki hydroelectric scheme. The lakes original outflow was at its southern end, into the Pukaki River. The outflow has been dammed, and canals carry water from Lake Pukaki and Lake Ohau through the Ohau A power station to Lake Ruataniwha. Pukaki is also fed by the waters of Lake Tekapo, which are diverted through a canal to a power station on Pukakis eastern shore . The lake has been raised twice to increase storage capacity, submerging Five Pound Note Island, which once appeared on New Zealands five pound note. The current lake has an operating range of 13.8 m, giving it an energy storage capacity of 1,595 GWh. Along with Lake Tekapos 770 GWh storage, it provides over half New Zealands hydroelectricity storage capacity. In September 2012, Environment Canterbury approved a change in conditions of Meridian Energys resource consent controlling the water levels and flows of Lake Pukaki. The change allows Meridian to lower the lake a further five metres from the minimum level of 518m above sea level in the event of an energy crisis.

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