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Shiel Hill
Shiel Hill is a residential suburb of the New Zealand city of Dunedin. It is located at the southeastern edge of the city's urban area, southeast of the city's centre at the western end of the Otago Peninsula, close to the isthmus joining the peninsula to the mainland. As the name suggests, it is situated on the slopes of a hill at the start of the ridge which runs along the spine of the peninsula. The slopes rise to a series of crests generally known collectively as Highcliff, a name also often applied to the last suburban vestiges which remain as Dunedin's urban area becomes the rural land of the peninsula. More accurately, the name is that of a cliff which lies on the Pacific coast of the peninsula east of Shiel Hill. The suburb is almost entirely residential, though there are some retail premises on the suburb's main road, Highcliff Road. These include a small nexus of shops at the southwestern edge of Shiel Hill, at the point where the suburb joins the neighbouring suburb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dunedin City Council
The Dunedin City Council ( mi, Kaunihera ā-Rohe o Ōtepoti) is the local government authority for Dunedin in New Zealand. It is a territorial authority elected to represent the people of Dunedin. Since October 2022, the Mayor of Dunedin is Jules Radich, who succeeded Aaron Hawkins. The council consists of a mayor who is elected at large, and 14 councillors elected at large, one of whom gets chosen as deputy-mayor. The councillors are elected under the Single Transferable Vote Single transferable vote (STV) is a multi-winner electoral system in which voters cast a single vote in the form of a ranked-choice ballot. Voters have the option to rank candidates, and their vote may be transferred according to alternate p ... (STV) system in triennial elections, with the most recent election held on 8 October 2022. 2022–present The current composition of the council is as follows: 2019–2022 During the 2019–2022 term the composition of the Council was as follow: 2016 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2006 New Zealand Census
The New Zealand Census of Population and Dwellings ( mi, Te Tatauranga o ngā Tāngata Huri Noa i Aotearoa me ō rātou Whare Noho) is a national population and housing census conducted by government department Statistics New Zealand every five years. There have been 34 censuses since 1851. In addition to providing detailed information about national demographics, the results of the census play an important part in the calculation of resource allocation to local service providers. The 2018 census took place on Tuesday 6 March 2018. The next census is expected in March 2023. Census date Since 1926, the census has always been held on a Tuesday and since 1966, the census always occurs in March. These are statistically the month and weekday on which New Zealanders are least likely to be travelling. The census forms have to be returned by midnight on census day for them to be valid. Conducting the census Until 2018, census forms were hand-delivered by census workers during the lead ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2013 New Zealand Census
The 2013 New Zealand census was the thirty-third national census. "The National Census Day" used for the census was on Tuesday, 5 March 2013. The population of New Zealand was counted as 4,242,048, – an increase of 214,101 or 5.3% over the 2006 census. The 2013 census forms were the same as the forms developed for the 2011 census which was cancelled due to the February 2011 major earthquake in Christchurch. There were no new topics or questions. New Zealand's next census was conducted in March 2018. Collection methods The results from the post-enumeration survey showed that the 2013 census recorded 97.6 percent of the residents in New Zealand on census night. However, the overall response rate was 92.9 percent, with a non-response rate of 7.1 percent made up of the net undercount and people who were counted in the census but had not received a form. Results Population and dwellings Population counts for New Zealand regions. Note: All figures are for the census usually r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2018 New Zealand Census
Eighteen or 18 may refer to: * 18 (number), the natural number following 17 and preceding 19 * one of the years 18 BC, AD 18, 1918, 2018 Film, television and entertainment * ''18'' (film), a 1993 Taiwanese experimental film based on the short story ''God's Dice'' * ''Eighteen'' (film), a 2005 Canadian dramatic feature film * 18 (British Board of Film Classification), a film rating in the United Kingdom, also used in Ireland by the Irish Film Classification Office * 18 (''Dragon Ball''), a character in the ''Dragon Ball'' franchise * "Eighteen", a 2006 episode of the animated television series ''12 oz. Mouse'' Music Albums * ''18'' (Moby album), 2002 * ''18'' (Nana Kitade album), 2005 * '' 18...'', 2009 debut album by G.E.M. Songs * "18" (5 Seconds of Summer song), from their 2014 eponymous debut album * "18" (One Direction song), from their 2014 studio album ''Four'' * "18", by Anarbor from their 2013 studio album '' Burnout'' * "I'm Eighteen", by Alice Cooper commo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edinburgh
Edinburgh ( ; gd, Dùn Èideann ) is the capital city of Scotland and one of its 32 Council areas of Scotland, council areas. Historically part of the county of Midlothian (interchangeably Edinburghshire before 1921), it is located in Lothian on the southern shore of the Firth of Forth. Edinburgh is Scotland's List of towns and cities in Scotland by population, second-most populous city, after Glasgow, and the List of cities in the United Kingdom, seventh-most populous city in the United Kingdom. Recognised as the capital of Scotland since at least the 15th century, Edinburgh is the seat of the Scottish Government, the Scottish Parliament and the Courts of Scotland, highest courts in Scotland. The city's Holyrood Palace, Palace of Holyroodhouse is the official residence of the Monarchy of the United Kingdom, British monarchy in Scotland. The city has long been a centre of education, particularly in the fields of medicine, Scots law, Scottish law, literature, philosophy, the sc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arthur's Seat
Arthur's Seat ( gd, Suidhe Artair, ) is an ancient volcano which is the main peak of the group of hills in Edinburgh, Scotland, which form most of Holyrood Park, described by Robert Louis Stevenson as "a hill for magnitude, a mountain in virtue of its bold design". It is situated just to the east of the city centre, about to the east of Edinburgh Castle. The hill rises above the city to a height of , provides excellent panoramic views of the city and beyond, is relatively easy to climb, and is popular for hillwalking. Though it can be climbed from almost any direction, the easiest and simplest ascent is from the east, where a grassy slope rises above Dunsapie Loch. At a spur of the hill, Salisbury Crags has historically been a rock climbing venue with routes of various degrees of difficulty. Until recently rock climbing was restricted to the South Quarry, but access is currently banned altogether by Historic Environment Scotland. Name It is sometimes said that its name is de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoopers Inlet
Hoopers Inlet is one of two large inlets in the Pacific coast of Otago Peninsula, in the South Island of New Zealand. The origin of the name is a little confused; there was an early settler family called Hooper who lived nearby, but the name appears on charts made prior to their arrival in the area. A. W. Reed has suggested that the name is a corruption of "Cooper's Inlet", named for Daniel Cooper, the ship's captain of the ''Unity'', which operated in the area during the Peninsula's years as a base for sealers.Reed, A.W. (1975) ''Place names of New Zealand.'' Wellington: A.H. & A.W. Reed. p.178 The inlet was on a traditional Māori route for collecting shellfish, which ran from Otakou to what is now St. Clair.Goodall, M., and Griffiths, G. (1980) ''Maori Dunedin.'' Dunedin: Otago Heritage Books. . p.17 The Māori name for the inlet was ''Puke-tu-roto'', meaning either "hills standing around a lake" or "hills standing inland". Like its near neighbour, Papanui Inlet, Hoopers Inle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boulder Beach
Boulder Beach is a rocky beach on the Pacific Ocean, located on the south side of Otago Peninsula, some by road east from central Dunedin, New Zealand. In addition to being relatively difficult to access physically due to the steepness of the surrounding country, it is closed to the public in the summer months (November–February) to protect the yellow-eyed penguins that nest on it. Physical geography Boulder Beach is approximately long, facing almost exactly due south. Near the eastern end a stretch of about is sandy; the remainder is covered in boulders, hence the beach's name. To the west the beach ends with the rise of Highcliff, for which the neighbouring suburb of Dunedin is named; Highcliff becomes Pudneys Cliff further west, and ends at Māori Head, beyond which lie Smaills Beach and Tomahawk Beach. To the east Boulder Beach is truncated by a series of headlands which culminate in Seal Point, followed by Sandfly Bay. Northward the land rises steeply to Highcliff H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pukehiki
Pukehiki is a small locality on the Otago Peninsula, within the city of Dunedin on the South Island of New Zealand. It is located on the ridge which runs along the centre of the peninsula, from Dunedin city centre, at a junction between Highcliff Road, which runs along the peninsula's ridge, and Castlewood Road, which descends to Company Bay on the shore of the Otago Harbour. Pukehiki has one notable structure, its local church. But it is far more well known for the nearby Larnach Castle, which lies to the north on Camp Road, a small road that leads off of Castlewood Road. From Pukehiki, Highcliff Road continues heading east, eventually reaching the coast at Portobello, New Zealand Portobello is a village beside the Otago Harbour halfway along the Otago Peninsula in Dunedin City, New Zealand. It lies at the foot of a small peninsula (Portobello Peninsula) between Portobello Bay and Latham Bay. Like scores of Dunedin fea .... Populated places in Otago Otago Peninsul ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandfly Bay
Sandfly Bay is a sandy bay with large dunes east of central Dunedin, New Zealand. Located on the southern side of Otago Peninsula, between Seal Point and the Gull Rocks on the western side of Sandymount, Sandfly Bay is a Department of Conservation wildlife reserve frequented by trampers. Name The bay is often thought by locals to have been named for a small biting insect known as the sandfly, but this is incorrect. It was named for the sand which, given the windy nature of this coast, flies from the tall dunes surrounding the bay. Physical geography Sandfly Bay is approximately across when measured in a straight line between the headlands. On the western side the cliffs of Seal Point rise directly out of the sea in a near-straight wall about long; beyond Seal Point along the coast lies Boulder Beach. On the eastern side lies a white sand beach, facing south-southwest, crossed by the mouth of Morris Creek flowing in from the north. Towards the eastern end of the bay t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Otago Harbour
Otago Harbour is the natural harbour of Dunedin, New Zealand, consisting of a long, much-indented stretch of generally navigable water separating the Otago Peninsula from the mainland. They join at its southwest end, from the harbour mouth. It is home to Dunedin's two port facilities, Port Chalmers (half way along the harbour) and at Dunedin's wharf (at the harbour's end). The harbour has been of significant economic importance for approximately 700 years, as a sheltered harbour and fishery, then deep water port. Geography The harbour was formed from the drowned remnants of the giant Dunedin Volcano, centred close to what is now Port Chalmers. The remains of this violent origin can be seen in the basalt of the surrounding hills. The last eruptive phase ended some ten million years ago, leaving the prominent peak of Mount Cargill. The ancient and modern channel runs along the western side of the harbour, the eastern side being shallow, with large sandbanks exposed at low tide. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
