Taranaki Region
Taranaki is a region in the west of New Zealand's North Island. It is named after its main geographical feature, the stratovolcano Taranaki Maunga, formerly known as Mount Egmont. The main centre is the city of New Plymouth. The New Plymouth District is one of three in the region and is home to more than 65 per cent of the population of Taranaki. The Stratford District includes the main centres of Stratford, Midhirst, Toko and Whangamomona. The South Taranaki District includes Hāwera, Manaia, Eltham, and Ōpunake. Since 2005, Taranaki has used the promotional brand "Like no other". Geography Taranaki is on the west coast of the North Island, surrounding the volcanic peak of Mount Taranaki. The region covers an area of 7258 km2. Its large bays north-west and south-west of Cape Egmont are North Taranaki Bight and South Taranaki Bight. Mount Taranaki is the second highest mountain in the North Island, and the dominant geographical feature of the region. A Māor ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Taranaki
Taranaki is a regions of New Zealand, region in the west of New Zealand's North Island. It is named after its main geographical feature, the stratovolcano Mount Taranaki, Taranaki Maunga, formerly known as Mount Egmont. The main centre is the city of New Plymouth. The New Plymouth District is one of three in the region and is home to more than 65 per cent of the population of Taranaki. The Stratford District includes the main centres of Stratford, New Zealand, Stratford, Midhirst, Toko and Whangamōmona, Whangamomona. The South Taranaki District includes Hāwera, Manaia, Taranaki, Manaia, Eltham, New Zealand, Eltham, and Ōpunake. Since 2005, Taranaki has used the promotional brand "Like no other". Geography Taranaki is on the west coast of the North Island, surrounding the volcanic peak of Mount Taranaki. The region covers an area of 7258 km2. Its large bays north-west and south-west of Cape Egmont are North Taranaki Bight and South Taranaki Bight. Mount Taranaki is t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Regions Of New Zealand
New Zealand is divided into sixteen regions for local government in New Zealand, local government purposes. Eleven are administered by regional councils, and five are administered by Unitary authority#New Zealand, unitary authorities, which are territorial authorities of New Zealand, territorial authorities that also perform the functions of regional councils. Although technically a district but classed as a territory, The Chatham Islands Territory is outside the regions and is administered by the Chatham Islands Council, which is similar to a unitary authority, authorised under its own legislation. Current regions History and statutory basis The regional councils are listed in Part 1 of Schedule 2 of the Local Government Act 2002, along with reference to the ''New Zealand Gazette, Gazette'' notices that established them in 1989. The act requires regional councils to promote sustainable developmentthe social, economic, environmental and cultural well-being of their communitie ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Whangamōmona
Whangamōmona is a small township in the Stratford, New Zealand, Stratford District and Manawatū-Whanganui, Manawatū-Whanganui Region of New Zealand. It lies on New Zealand State Highway 43, State Highway 43, the "Forgotten World Highway", north-east of Stratford and south-west of Ōhura. By rail it is from Stratford on the Stratford–Okahukura Line, Stratford-Okahukura railway line.Wises New Zealand Guide, 7th Edition, 1979. p. 506. Demographics Whangamōmona statistical area covers and had an estimated population of as of with a population density of people per km2. Whangamōmona had a population of 126 at the 2018 New Zealand census, a decrease of 24 people (−16.0%) since the 2013 New Zealand census, 2013 census, and a decrease of 42 people (−25.0%) since the 2006 New Zealand census, 2006 census. There were 54 households, comprising 72 males and 54 females, giving a sex ratio of 1.33 males per female. The median age was 49.7 years (compared with 37.4 years nati ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mount Ruapehu
Mount Ruapehu (; English ) is an active stratovolcano at the southern end of the Taupō Volcanic Zone and North Island North Island Volcanic Plateau, volcanic plateau in New Zealand. It is northeast of Ohakune and southwest of the southern shore of Lake Taupō, within Tongariro National Park. The North Island's major ski resorts and only glaciers are on its slopes. Ruapehu, the largest active volcano in New Zealand, has the highest point in the North Island and has three major peaks: Tahurangi (2,797 m), Te Heuheu (2,755 m) and Paretetaitonga (2,751 m). The deep, active volcanic crater, crater is between the peaks and fills with water between major eruptions, being known as Crater Lake (). The name ''Ruapehu'' means "pit of noise" or "exploding pit" in Māori language, Māori. Geography Ruapehu is located in the centre of the North Island of New Zealand, northeast of Ohakune, New Zealand, and southwest of the southern shore of Lake Taupō, within Tongariro ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mount Ngauruhoe
Mount Ngauruhoe () is a volcanic cone in New Zealand. It is the youngest vent in the Mount Tongariro, Tongariro stratovolcano complex on the Central Plateau, New Zealand, Central Plateau of the North Island and first erupted about 2,500 years ago. Although often regarded as a separate mountain, geologically, it is a secondary cone of Mount Tongariro. The volcano lies between the active volcanoes of Mount Tongariro to the north and Mount Ruapehu to the south, to the west of the Rangipo Desert and to the south of the southern shore of Lake Taupō. Etymology Before the initial mapping of the area introduced labelling confusion, the local Māori name for the cone was Tongariro, and its summit crater was known as Ngāuruhoe. The local Māori traditions state that the volcano was named by Ngātoro-i-rangi, an ancestor of the local Māori iwi, Ngāti Tūwharetoa. Ngātoro-i-rangi called volcanic fire from his homeland Hawaiki, which eventually emerged at Ngauruhoe. The name ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mount Tongariro
Mount Tongariro (; ) is a compound volcano in the Taupō Volcanic Zone of the North Island of New Zealand. It is located to the southwest of Lake Taupō, and is the northernmost of the three active volcanoes that dominate the landscape of the central North Island. Geology Mount Tongariro is part of the Tongariro volcanic centre, which consists of four massifs made of andesite: Tongariro, Kakaramea-Tihia Massif, Pihanga, and Ruapehu at the southern end of the North Island Volcanic Plateau. The andesitic eruptions formed Tongariro, a steep stratovolcano, reaching a height of . Tongariro is composed of layers of both lava and tephra and the eruptions that built the current stratovolcano commenced about 275,000 years ago. Tongariro consists of at least 12 cones. Ngauruhoe, while often regarded as a separate mountain, is geologically a cone of Tongariro. It is also the most active vent, having erupted more than 70 times since 1839, the last episode in 1973 to 1975. Activ ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mount Taranaki Legend
Mount Taranaki (), officially Taranaki Maunga and also known as Mount Egmont, is a dormant stratovolcano in the Taranaki region on the west coast of New Zealand's North Island. At , it is the second highest mountain in the North Island, after Mount Ruapehu. It has a secondary cone, Fanthams Peak (), , on its south side. Name The name ''Taranaki'' is from the Māori language. The mountain was named after Rua Taranaki, the first ancestor of the iwi (tribe) called Taranaki, one of several iwi in the region. The Māori word ''tara'' means mountain peak, and ''naki'' may come from ''ngaki'', meaning "clear of vegetation." It was also named ("ice mountain") and ("hill of Naki") by iwi who lived in the region in "ancient times". Captain Cook named it Mount Egmont on 11 January 1770 after John Perceval, 2nd Earl of Egmont, a former First Lord of the Admiralty who had supported the concept of an oceanic search for '' Terra Australis Incognita''. Cook described it as "of a prodig ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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South Taranaki Bight
The South Taranaki Bight is a large bay on the west coast of New Zealand, south of Taranaki, west of the Manawatu, north and west of the western entrance of Cook Strait and north of the South Island. The name is sometimes used for a much smaller bay in South Taranaki, between the mouth of the Kaupokonui Stream directly south of Mount Taranaki and the mouth of the Pātea River. Approximately 18,000 years ago during the Last Glacial Maximum when sea levels were over lower than present day levels, the South Taranaki Bight was a coastal plain which connected the North and South Islands, featuring rivers which drained into the Cook Strait (then a harbour) to the south-east. Sea levels began to rise 7,000 years ago, eventually separating the islands and connecting the Cook Strait to the Tasman Sea. The bight was once a calving ground for southern right whales in winter and spring and early Europeans in New Zealand called it Mothering Bay after the large number of cow-calf pairs. ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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North Taranaki Bight
The North Taranaki Bight is a large bay that extends north and east from the north coast of Taranaki in New Zealand's North Island. The name is echoed by the South Taranaki Bight to the south of Cape Egmont. As with its southern counterpart, the size of the bight depends to a large extent on the source referring to it. Strict definitions refer to it stretching from the mouth of the Waitara River, 10 kilometres northeast of New Plymouth, to the mouth of the Mokau River. Looser descriptions refer to it extending as far north as Tirua Point, 50 kilometres southwest of Te Kūiti, or even to Albatross Point, close to the entrance to Kawhia Harbour. Some include New Plymouth in the bight. See also * South Taranaki Bight The South Taranaki Bight is a large bay on the west coast of New Zealand, south of Taranaki, west of the Manawatu, north and west of the western entrance of Cook Strait and north of the South Island. The name is sometimes used for a much smaller ... Ref ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Cape Egmont
Cape Egmont, splitting Northern and Southern Taranaki Bights, is the westernmost point of Taranaki, on the west coast of New Zealand's North Island. It is located close to the volcanic cone of Mount Taranaki or Mount Egmont. It was named ''Kaap Pieter Boreel'' by Dutch explorer Abel Tasman in 1642, but renamed ''Cape Egmont'' by British explorer James Cook in 1769. (Note: Tasman did not sight Mount Taranaki, due to bad visibility, but Cook did, and after naming the mountain Mount Egmont, bestowed the same name on the promontory, which became the enduring name). Ironically, the cape retained a Dutch name, as Cook named the mountain and cape after the Earl of Egmont, who claimed descent of the Dutch House of Egmond. In July 1862, Kapoaiaia near Cape Egmont was the site of a hui between 600 members of Taranaki, Ngāti Ruanui Ngāti Ruanui is a Māori people, Māori iwi traditionally based in the Taranaki Region, Taranaki region of New Zealand. In the 2006 census, 7,035 pe ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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2023 NZ Census Population Density - Taranaki Region
3 (three) is a number, numeral and digit. It is the natural number following 2 and preceding 4, and is the smallest odd prime number and the only prime preceding a square number. It has religious and cultural significance in many societies. Evolution of the Arabic digit The use of three lines to denote the number 3 occurred in many writing systems, including some (like Roman and Chinese numerals) that are still in use. That was also the original representation of 3 in the Brahmic (Indian) numerical notation, its earliest forms aligned vertically. However, during the Gupta Empire the sign was modified by the addition of a curve on each line. The Nāgarī script rotated the lines clockwise, so they appeared horizontally, and ended each line with a short downward stroke on the right. In cursive script, the three strokes were eventually connected to form a glyph resembling a with an additional stroke at the bottom: ३. The Indian digits spread to the Caliphate in the 9th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |