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Saddle Hill, New Zealand
Saddle Hill is a prominent landmark overlooking the northeastern end of the Taieri Plains in Otago, New Zealand. Within the limits of Dunedin city, it is located 18 kilometres to the west of the city centre, between Mosgiel and Green Island, New Zealand, Green Island, and is clearly visible from many of the city's southern hill suburbs. A lookout on the northern slopes of the hill commands a good view across the plains, with Lake Waihola visible 25 kilometres to the west in clear weather. The hill has two peaks: the eastern is the higher, rising to 473 metres; the western peak – Jaffrays Hill – rises to 431 metres. Of largely volcanic origin, the hill is part of the extinct Dunedin Volcano complex, with a base of Cretaceous breccia overlaid with Miocene igneous rocks, these in turn overlaid with Cenozoic sediments. Erosion has revealed a volcanic plug on the western peak, giving the hill its distinct breast-like shape. The hill was – along with Cape Saunders on the Otago ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Green Island, New Zealand
Green Island is a suburb of Dunedin, New Zealand. Not an actual island, this former borough takes its name from the Green Island bush, uncleared native forest extending from the valley where the community is centred over the hills towards the coast. The name of the nearby offshore island — Green Island (Okaihe) — was used to identify the bush and, thus, also lent its name to the mainland suburb. Green Island suburb Under the 1989 local government reforms, the city of Dunedin and its surrounding region was grouped into a territorial authority called Dunedin City. Under this system, Green Island is officially an outer suburb within this territorial authority. Green Island is on State Highway 1, about west-southwest of the Octagon, Dunedin's city centre. Along with neighbouring Abbotsford, it is the westernmost suburb within Dunedin City's main urban area. Green Island's main economy is based on light and small scale heavy industry. Prior to 1950 Green Island, and neighbou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cenozoic
The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants, a cooling and drying climate, and the current configuration of continents. It is the latest of three geological eras since complex life evolved, preceded by the Mesozoic and Paleozoic. It started with the Cretaceous–Paleogene extinction event, when many species, including the non-avian dinosaurs, became extinct in an event attributed by most experts to the impact of a large asteroid or other celestial body, the Chicxulub impactor. The Cenozoic is also known as the Age of Mammals because the terrestrial animals that dominated both hemispheres were mammalsthe eutherians (placentals) in the northern hemisphere and the metatherians (marsupials, now mainly restricted to Australia) in the southern hemisphere. The extinction of many groups allowed mammals and birds to greatly diversify so that l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Dunedin
Dunedin ( ; mi, Ōtepoti) is the second-largest city in the South Island of New Zealand (after Christchurch), and the principal city of the Otago region. Its name comes from , the Scottish Gaelic name for Edinburgh, the capital of Scotland. The city has a rich Scottish, Chinese and Māori heritage. With an estimated population of as of , Dunedin is both New Zealand's seventh-most populous metro and urban area. For historic, cultural and geographic reasons the city has long been considered one of New Zealand's four main centres. The urban area of Dunedin lies on the central-eastern coast of Otago, surrounding the head of Otago Harbour, and the harbour and hills around Dunedin are the remnants of an extinct volcano. The city suburbs extend out into the surrounding valleys and hills, onto the isthmus of the Otago Peninsula, and along the shores of the Otago Harbour and the Pacific Ocean. Archaeological evidence points to lengthy occupation of the area by Māori prior to the ar ... [...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] |
Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neville Peat
Neville Douglas Peat (born 1947) is a New Zealand author and photographer, based at Broad Bay on the Otago Peninsula. He specialises in topics about natural history, notably that of southern New Zealand and New Zealand's subantarctic islands. He has written over 40 titles since the late 1970s and has been writing full-time since 1986. In 1994, Peat was named Dunedin Citizen of the Year for his series of photographic books on the city and his establishment of the Dunedin Environmental Business Network, and in 1996 won the Montana New Zealand Book Awards for his book ''Wild Dunedin''. He has been a Councillor on the Otago Regional Council since 1998, and was its Deputy Chairperson from 2004 to 2007. In 2004, Peat was behind moves to create an official flag for Otago. This culminated in a competition run through the auspices of the '' Otago Daily Times'' newspaper and Otago Polytechnic School of Art towards the end of that year. In 2007, Peat was awarded the Creative New Zea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taniwha
In Māori mythology, taniwha () are large supernatural beings that live in deep pools in rivers, dark caves, or in the sea, especially in places with dangerous currents or deceptive breakers (giant waves). They may be considered highly respected kaitiaki (protective guardians) of people and places, or in some traditions as dangerous, predatory beings, which for example would kidnap women to have as wives. Etymology and Pacific analogues Linguists have reconstructed the word ''taniwha'' to Proto-Oceanic *''tanifa'', with the meaning "shark species". In Tongan and Niuean, ''tenifa'' refers to a large dangerous shark, as does the Samoan ''tanifa''; the Tokelauan ''tanifa'' is a sea-monster that eats people. In most other Polynesian languages, the cognate words refer to sharks or simply fish. Some anthropologists have stated that the taniwha has "analogues that appear within other Polynesian cosmologies".A. Asbjørn Jøn,The Road and the Taniwha in ''Australian Folklore: A Yearly ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori Mythology
Māori mythology and Māori traditions are two major categories into which the remote oral history of New Zealand's Māori may be divided. Māori myths concern fantastic tales relating to the origins of what was the observable world for the pre-European Māori, often involving gods and demigods. Māori tradition concerns more folkloric legends often involving historical or semi-historical forebears. Both categories merge in to explain the overall origin of the Māori and their connections to the world which they lived in. Māori had yet to invent a writing system before European contact, beginning in 1769, so they had no method to permanently record their histories, traditions, or mythologies. They relied on oral retellings memorised from generation to generation. The three forms of expression prominent in Māori and Polynesian oral literature are genealogical recital, poetry, and narrative prose. Experts in these subjects were broadly known as . The rituals, beliefs, and ge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Captain James Cook
James Cook (7 November 1728 Old Style date: 27 October – 14 February 1779) was a British explorer, navigator, cartographer, and captain in the British Royal Navy, famous for his three voyages between 1768 and 1779 in the Pacific Ocean and to New Zealand and Australia in particular. He made detailed maps of Newfoundland prior to making three voyages to the Pacific, during which he achieved the first recorded European contact with the eastern coastline of Australia and the Hawaiian Islands, and the first recorded circumnavigation of New Zealand. Cook joined the British merchant navy as a teenager and joined the Royal Navy in 1755. He saw action in the Seven Years' War and subsequently surveyed and mapped much of the entrance to the St. Lawrence River during the siege of Quebec, which brought him to the attention of the Admiralty and the Royal Society. This acclaim came at a crucial moment for the direction of British overseas exploration, and it led to his commission in 1768 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Otago Peninsula
The Otago Peninsula ( mi, Muaūpoko) is a long, hilly indented finger of land that forms the easternmost part of Dunedin, New Zealand. Volcanic in origin, it forms one wall of the eroded valley that now forms Otago Harbour. The peninsula lies south-east of Otago Harbour and runs parallel to the mainland for 20 km, with a maximum width of 9 km. It is joined to the mainland at the south-west end by a narrow isthmus about 1.5 km wide. The suburbs of Dunedin encroach onto the western end of the peninsula, and seven townships and communities lie along the harbourside shore. The majority of the land is sparsely populated and occupied by steep open pasture. The peninsula is home to many species of wildlife, notably seabirds, pinnipeds, and penguins; several ecotourism businesses operate in the area. Geography The peninsula was formed at the same time as the hills facing it across the harbour, as part of the large, long-extinct, Dunedin Volcano. Several of the peninsula' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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