Kawerau (soccer)
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Kawerau (soccer)
Kawerau is a town in the Bay of Plenty Region on the North Island of New Zealand. It is situated 100 km south-east of Tauranga and 58 km east of Rotorua. It is the seat of the Kawerau District Council, and the only town in Kawerau District. Kawerau is a small community, with an economy that is largely driven by the nearby pulp and paper mill that is run by Norske Skog and OJI Fibre Solutions. It is located along State Highway 34, southwest of Onepu, and is the terminus of the East Coast Main Trunk Railway, and the commencing point of the Murupara Branch railway. Kawerau is among the three towns in New Zealand with a majority Māori population, along with Ōpōtiki and Wairoa. Kawerau was one of the worst-affected towns in the 1987 Edgecumbe earthquake. History and culture European settlement Kawerau, one of the youngest towns in New Zealand, was founded in 1953 as a mill town for the new Tasman pulp and paper mill. The site for the mill was chosen by the Ta ...
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Urban Areas Of New Zealand
Statistics New Zealand defines urban areas of New Zealand for statistical purposes (they have no administrative or legal basis). The urban areas comprise List of cities in New Zealand, cities, List of towns in New Zealand, towns and other conurbations (an aggregation of urban settlements) of a thousand people or more. In combination, the urban areas of the country constitute New Zealand's urban population. As of , the urban population made up % of New Zealand's total population. The current standard for urban areas is the Statistical Standard for Geographic Areas 2018 (SSGA18), which replaced the New Zealand Standard Areas Classification 1992 (NZSAC92) in 2018. There are four classes of urban area under SSGA18: *Major urban areas, with a population of 100,000 or more. There are seven major urban areas which combined have a population of (% of the total population). *Large urban areas, with a population of 30,000 to 99,999. There are 13 large urban areas which combined have a pop ...
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Rotorua
Rotorua () is a city in the Bay of Plenty region of New Zealand's North Island. The city lies on the southern shores of Lake Rotorua, from which it takes its name. It is the seat of the Rotorua Lakes District, a territorial authority encompassing Rotorua and several other nearby towns. Rotorua has an estimated resident population of , making it the country's 12th largest urban area, and the Bay of Plenty's second largest urban area behind Tauranga. Rotorua is a major destination for both domestic and international tourists; the tourism industry is by far the largest industry in the district. It is known for its geothermal activity, and features geysers – notably the Pōhutu Geyser at Whakarewarewa – and hot mud pools. This thermal activity is sourced to the Rotorua Caldera, in which the town lies. Rotorua is home to the Toi Ohomai Institute of Technology. History The name Rotorua comes from the Māori language, where the full name for the city and lake is . ''Roto'' m ...
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Norske Skog
Norske Skog ASA, formerly Norske Skogindustrier ASA, which translates as ''Norwegian Forest Industries'', is a Norwegian pulp and paper company established in 1962. The company has long been one of the world's leading manufacturers of newsprint and magazine paper. Due to a declining market for publication paper, the company has increasingly focused on other uses of timber and recycled paper, such as packaging. The company is headquartered in Norway and has factories in five countries and an annual production of approximately 2 million tonnes of paper (2020). History Norske Skog started in 1962 with the construction of a paper mill at Skogn in Norway, with the plant opening in 1966 and a second paper machine added in 1967. Half the capital for the project was issued by the Norwegian Forest Owners Association. In 1972 Norske Skog started a cooperation with Follum Fabrikker in Hønefoss. By 1989 Norske Skog had acquired Follum Fabrikker and Union in Skien as well as Saugbrugsfore ...
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Kaingaroa Forest
Kaingaroa Forest covers 2900 km² of the Bay of Plenty region of New Zealand, and is the largest forest plantation in New Zealand, and the second largest in the Southern Hemisphere (after the 6000km² Sabie/Graskop plantation in South Africa). The forest stretches from Lake Taupō in the south to Kawerau to the north. The headquarters of the forest are at the small settlement of Kaingaroa, Bay of Plenty, 50 kilometres southeast of Rotorua. Prior to planting the area was a tussock and scrub plateau (ranging between and high), formed on volcanic ash. The New Zealand Ministry for Culture and Heritage gives a translation of "long area of land" for ''Kāingaroa''. The forest was first planted in the late 1920s and owned as a state asset by the New Zealand government. Experimental planting of douglas fir and radiata pine began on a block at Kaingaroa in 1901 and continued from 1906 using Waiotapu prison labour. By 1932 the pines averaged high and in diameter. Later plan ...
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Tarawera River
The Tarawera River is in the Bay of Plenty Region in the North Island of New Zealand. It flows from Lake Tarawera, northeastwards across the northern flanks of the active volcano Mount Tarawera, and past the town of Kawerau before turning north, reaching the Bay of Plenty west of Edgecumbe. The Tarawera Falls on the river are considered to be quite spectacular. Environmental issues The Tasman Pulp and Paper Mill, now owned by Norske Skog, has been discharging waste into the river since 1955. Local residents have erected signposts labelling the river as the "Black Drain" since the 1990s. The dark colour is due to the presence of pollution from farms, sewage and stormwater but it is predominantly from pulp and paper mill effluent. As of 1997, pulp and paper mills were discharging over 160 million litres of industrial waste into the river per day. By 2006, the oxygen levels in the river had reached a level where fish could survive, however the water colour was still dark. Since ...
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Geothermal Energy
Geothermal energy is the thermal energy in the Earth's crust which originates from the formation of the planet and from radioactive decay of materials in currently uncertain but possibly roughly equal proportions. The high temperature and pressure in Earth's interior cause some rock to melt and solid mantle to behave plastically. This results in parts of the mantle convecting upward since it is lighter than the surrounding rock. Temperatures at the core–mantle boundary can reach over 4000 °C (7200 °F). Geothermal heating, using water from hot springs, for example, has been used for bathing since Paleolithic times and for space heating since ancient Roman times. More recently geothermal power, the term used for generation of electricity from geothermal energy, has gained in importance. It is estimated that the earth's geothermal resources are theoretically more than adequate to supply humanity's energy needs, although only a very small fraction is currently being ...
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Mill Town
A mill town, also known as factory town or mill village, is typically a settlement that developed around one or more mills or factories, usually cotton mills or factories producing textiles. Europe Italy * ''Crespi d'Adda'', UNESCO World Heritage Site * ''Nuovo quartiere operaio'' in Schio * ''Villaggio Leumann'' a Collegno * ''Villaggio Frua'' in Saronno * ''Villaggio operaio della Filatura'' in Tollegno Poland Żyrardów The town grew out of a textile factory founded in 1833 by the sons of Feliks Lubienski, who owned the land where it was built. They brought in a specialist from France and his newly designed machines. He was French inventor, Philippe de Girard from Lourmarin. He became a director of the firm. The factory town developed during the 19th century into a significant textile mill town in Poland. In honour of Girard, 'Ruda Guzowska' as the original estate was called, was renamed Żyrardów, a toponym derived of the polonised spelling of Girard's name. Most of ...
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1987 Edgecumbe Earthquake
The 1987 Edgecumbe earthquake measured 6.5 on the moment magnitude scale and struck the Bay of Plenty region of New Zealand at 1:42 pm on 2 March. The hypocentre was at a shallow depth of 8 km. The epicentre was south-south-east of the town of Matata, and north-north-west of Edgecumbe, on the Rangitaiki Plains (the floodplain of the Rangitaiki River, the Tarawera River and the Whakatane River). It was the most damaging earthquake New Zealand had experienced since the 1968 Inangahua earthquake. Main event The main shock was preceded for two weeks by earthquake swarms in two areas of the Bay of Plenty. A swarm started on 21 February off-shore from Maketu, near Te Puke, 40 kilometres from the main shock's epicentre, and another swarm started on 26 February between Matata and Thornton, very close to the epicentre. Then there was a 5.2 earthquake at 1:35 pm on 2 March, followed by the main shock seven minutes later. The main shock appears to have actually consisted ...
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Wairoa
Wairoa is a town and territorial authority district in New Zealand's North Island. The town is the northernmost in the Hawke's Bay region, and is located on the northern shore of Hawke Bay at the mouth of the Wairoa River and to the west of Māhia Peninsula. It is on State Highway 2, northeast of Napier, and southwest of Gisborne. Wairoa is the nearest town to the Te Urewera protected area and former national park that is accessible from Wairoa via State Highway 38. It is the largest town in the district of Wairoa, and is one of three towns in New Zealand where Māori outnumber other ethnicities, with 62.29% of the population identifying as Māori. History Early history Te Wairoa was originally a Māori settlement. The ancestral waka (canoe) Tākitimu travelled up the river and landed at Mākeakea, near where Tākitimu meeting house stands today. The Wairoa river (full name: Te Wairoa Hōpūpū Hōnengenenge Matangirau) was an important source of food as well as a t ...
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Ōpōtiki
Ōpōtiki (; from ''Ōpōtiki-Mai-Tawhiti'') is a small town in the eastern Bay of Plenty in the North Island of New Zealand. It houses the headquarters of the Ōpōtiki District Council and comes under the Bay of Plenty Regional Council. Geography The town of Ōpōtiki is situated exactly on latitude 38° South. The climate is temperate. Summer temperatures reach the mid-20s (Celsius, mid-70s Fahrenheit) on the coast and encourage a continuation of the beach culture of the Bay of Plenty. Winter days are often cloudless, the daytime temperature never drops below freezing but there may be a mild frost at night. Winter snow falls along the crest of the ranges, and on the higher peaks (over 1000 m) may remain for a few weeks. Rain occurs at any season. Severe localised rainstorms ('cloudbursts') may occur in the high country and have caused flash flooding including past inundations of Ōpōtiki township. Demographics The Ōpōtiki urban area, as defined by Statistics New Zeala ...
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Murupara Branch
The Murupara Branch is a long branch railway line from the East Coast Main Trunk (ECMT) at Kawerau to Murupara, built to serve a new pulp and paper mill harvesting the radiata pine trees of the Kaingaroa Forest on the Kaingaroa Plateau in the Bay of Plenty, New Zealand. The line was the last major extension of the New Zealand Railways Department (NZR) network, of from Hawkens Junction, west of Edgecumbe, to Kawerau and 57 km from Kawerau to Murupara. The portion from Hawkens Junction to Kawerau was known as the Kawerau Branch until 1978, when it became part of the ECMT, and the former ECMT from Hawkens Junction to Taneatua became the Taneatua Branch. History Construction of the line began in 1951, but in March 1953 it was decided to build the mill at Kawerau not Murupara, because Kawerau had geothermal steam for energy, and the climate of Murupara in winter is misty, so was less suitable for a large town. The branch was built via Kawerau to Murupara rather than directly ...
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East Coast Main Trunk Railway
The East Coast Main Trunk (ECMT) is a railway line in the North Island of New Zealand, originally running between Hamilton and Taneatua via Tauranga, connecting the Waikato with the Bay of Plenty. The ECMT now runs between Hamilton and Kawerau, with a branch line to Taneatua from the junction at Hawkens. The line is built to narrow gauge of , the uniform gauge in New Zealand. It was known as the East Coast Main Trunk Railway until 2011, when the word "Railway" was dropped. History Construction In 1880, the North Island Main Trunk railway had reached Frankton, Waikato, Frankton, Hamilton, New Zealand, Hamilton, from Auckland. From there, it was delayed by construction of the Claudelands Bridge, original Waikato River bridge (now carrying road traffic as part of Claudelands Road), before the line made its way to Morrinsville in October 1884, Te Aroha in March 1886 and Paeroa in 1898. There were also minor delays, such as in the delivery of Podocarpus totara, totara sleepers. The ...
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