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Maniototo
The Maniatoto Plain, usually simply known as The Maniatoto, is an elevated inland region in Otago, New Zealand. The region roughly surrounds the upper reaches of the Taieri River and the Manuherikia River. It is bounded by the Kakanui Range to the north and the Rock and Pillar Range to the southeast. It has a harsh, dry climate, ranging from over 30 °C in mid-summer to -15 °C in mid-winter. The region is sparsely populated, with the largest centres being Ranfurly, Naseby, Wedderburn and Oturehua. Part of the Canterbury-Otago tussock grasslands the land surrounding the plain is hilly, with many outcrops of rock which also break up the plain in places. During the 1860s the region was one of the sites of the Otago gold rush, and relics from that era can still be seen around the towns of Kyeburn, Naseby, and St. Bathans. Sheep farming is the major source of income. The area is closely associated with the sport of curling. Naseby has the only indoor curling rink ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ranfurly, New Zealand
Ranfurly is a town in the Central Otago District of Otago, New Zealand. Located north of Dunedin, it lies in the dry rough plain of Maniototo at a moderately high altitude (around above sea level) close to a small tributary of the Taieri River. It operates as a service town for the local farming community. The town was formerly known as Eweburn, one of the "farmyard" names bestowed by former Otago Chief Surveyor John Turnbull Thomson on many small streams and locations in the district. The modern name honours the Fifth Earl of Ranfurly, who served as Governor of New Zealand (1897–1904) at the time of the extension of the Otago Central Railway to the area. Ranfurly is well known for its Art Deco buildings, such as its hotel and the dairy. History During the Otago gold rush of the 1860s, several important deposits of the precious metal were found near Ranfurly, notably at Kyeburn and Naseby, close to the southwestern face of the Kakanui Range. After the gold-rush faded Ranf ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Naseby, New Zealand
Naseby is a small town, formerly a borough, in the Maniototo area of Central Otago, New Zealand. It is named after a village in Northamptonshire, England, which was the site of a major battle during the English Civil War. Previous names of the township were Parker's, Hogburn and Mt Ida. The town catch phrase is "2000 feet above worry level" indicating its altitude. Naseby is 395 km (5 hours drive) from Christchurch and 143 km (1 hour 45 minutes drive) from Dunedin. History An important township during the gold rush of the 1860s, Gold was discovered in the Hogburn in 1863. Much of the town has been preserved from this time and has something of the air of a working museum. At its peak, the population of the town was around 4,000 miners. Eighteen stores, 14 hotels, two butchers and a hospital had also been built to service the miners. In 1898, a railway line was constructed 12 km away in Ranfurly and as a result services gradually moved away from Naseby to Ranf ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kakanui Range
The Kakanui Range (or Kakanui Mountains) is a range of high hills located inland from Oamaru in the South Island of New Zealand. The range forms a boundary between the valley of the Waitaki River to the north and the high plateau known as the Maniototo and the upper watershed of the Taieri River to the southwest. The western Kakanui Range is crossed by road at Danseys Pass, which has a saddle A saddle is a supportive structure for a rider of an animal, fastened to an animal's back by a girth. The most common type is equestrian. However, specialized saddles have been created for oxen, camels and other animals. It is not know ... at . The eastern portions start to the north east of The Pigroot and Pigroot Hill to the east of the road is a foothill of the range. Geology The southwestern slopes of the Kakanui Range were a major goldfield during the Otago gold rush of the 1860s. Relics from this goldrush can be found at Kyeburn and Naseby. The Kakanui Range i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hyde, New Zealand
Hyde is a locality in Otago Otago (, ; ) is a regions of New Zealand, region of New Zealand located in the southern half of the South Island and administered by the Otago Regional Council. It has an area of approximately , making it the country's second largest local go ..., New Zealand, located in the Strath-Taieri. It is close to the northern end of the Rock and Pillar Range on New Zealand State Highway 87, State Highway 87 between Middlemarch, New Zealand, Middlemarch and Ranfurly, New Zealand, Ranfurly. Hyde is best known as the site of the Hyde railway disaster of 4 June 1943, in which 21 people were killed when an express train on the Otago Central Railway derailed at high speed in a cutting near the town. At the time, it was the worst railway accident in New Zealand's history; it has only been passed by the Tangiwai disaster of 24 December 1953, which claimed the lives of 151 people. The site of the Hyde disaster can now be walked as part of the Otago Central Rail ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Otago District Council
Central Otago District Council is the territorial authority for the Central Otago District of New Zealand New Zealand () is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and List of islands of New Zealand, over 600 smaller islands. It is the List of isla .... The council is led by the mayor of Central Otago, who is currently . There are also 11 ward councillors. Composition Councillors * Mayor * Vincent Ward: Tamah Alley, Lynley Claridge, Ian Cooney, Martin McPherson, Tracy Paterson * Cromwell Ward: Neil Gillespie, Shirley Calvert, Cheryl Laws, Nigel McKinlay * Maniototo Ward: Stuart Duncan * Teviot Valley Ward: Stephen Jeffery Community boards * Cromwell Community Board * Maniototo Community Board * Teviot Valley Community Board * Vincent Community Board History The council was established in 1989, through the merger of Cromwell Borough Council (established in 1866), Al ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oturehua
The township of Oturehua is in the Ida Valley of the Maniototo, in Central Otago, in the South Island of New Zealand. The settlement stands at 500 metres above sea level, some 25 kilometres from Ranfurly, to which it is connected by both road and the Otago Central Rail Trail long-distance walking track. The population was 112 residents at last count. The New Zealand Ministry for Culture and Heritage gives a translation of "place where the summer star stands still" for ''Ōturēhua''. History Oturehua lies beneath a Rough Ridge, a range of hills. The township was also called Rough Ridge until 1907. The area has changed little from its description in 1905 when it was described as good arable land, from which large crops are successfully raised. In 1905, the township comprised a post and telegraph office, a store, a hotel near the railway station, a school, coal pits and a flour mill. Of these, only the Gilchrist's General Store and the Oturehua Tavern remain. In 1967 member ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock And Pillar Range
The Rock and Pillar Range (), is a range of high hills is located in the Maniototo, an area of inland Otago, New Zealand. The range is surrounded on three sides by the Taieri River, which has its source in the Lammerlaw Range. The river flows out across the scroll plain at Paerau, along the north west flanks of the Rock and Pillar Range before almost doubling back on itself at Waipiata and flowing back along the eastern side past Hyde through the Strath-Taieri. The town of Middlemarch lies close to the Taieri River to the east of the range, and Patearoa lies to the northwest. The Rock and Pillars are a horst range, caused by movement on two parallel faults uplifting the area in between. Thus, the range is characterised by a very flat top, with steep escarpments on either side. The Great Moss Swamp lies on the upper surface of the range. There is a often persistent and unusual cloud formation associated with the range. This strange cloud formation, is more or less statio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manuherikia River
The Manuherikia River is located in Otago in the South Island of New Zealand. It rises in the far north of the Maniototo, with the West Branch draining the eastern side of the St Bathans Range, and the East Branch draining the western flanks of the Hawkdun Range. The river continues southwest through the wide Manuherikia Valley to its confluence with the Clutha River at Alexandra. During the 1860s the Manuherikia was one of the centres of the Otago gold rush. The river is crossed by two historically significant bridges, the curved Manuherikia Bridge No.1 (number 70 on the Otago Central Railway line), a concrete pier bridge completed in 1903, and a stone pier bridge at Ophir built in 1880. The Māori spelling for the river is Manuherekia, meaning "at long last". See also *List of rivers of New Zealand This is a list of all waterways named as rivers in New Zealand. A * Aan River * Acheron River (Canterbury) * Acheron River (Marlborough) * Ada River (New Zealand), Ada ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taieri River
The Taieri River (a misspelling of the original Māori name ''Taiari'' ) is the fourth-longest river in New Zealand and is in Otago in the South Island. Rising in the Lammerlaw Range, it initially flows north, then east around the Rock and Pillar range before turning southeast, reaching the sea south of Dunedin. The upper reaches meander in a series of convoluted loops across a floodplain above Paerau, close to the aptly named locality of Serpentine, New Zealand, Serpentine; the river has created many small oxbow lakes in this area, some of which have been converted into water meadows. From here the river runs through two small hydroelectric power stations before reaching Patearoa in The Maniototo. The Taieri then arcs through almost 180 degrees, entering a broad glacial valley (the Strath-Taieri, New Zealand, Strath-Taieri) surrounded by rugged hill ranges. Immediately downstream the river has cut a steep-sided declivity, the Taieri Gorge. This is known for the Taieri Gorge Ra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ida Valley
The Ida Valley lies east of the Manuherikia River, Manuherikia Valley in :en:Central Otago, Central Otago, New Zealand. At an altitude of around , the 40 km long flat and wide valley is a relatively dry region with cold winters and hot summers, much like the rest of Central Otago. Most agricultural production in the Ida Valley is lamb, including merino, and stud cattle. The valley is named after thIdaburn Idaburn flows from Mount Ida in the Ida Range, through the northern section of the Ida Valley, breaks through Raggedy Ridge through the Poolburn Gorge and into Manuherikia River. The Idaburn is joined by the Pool Burn (which drains the valley's southern section) shortly before entering the Poolburn Gorge. The largest settlement in the sparsely populated Ida Valley is Oturehua, a small village at the northern end. Other localities include "Moa Creek", "Poolburn", "Ida Valley" and "Idaburn" which are groups of a few houses and farms rather than villages. Poolburn is th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Otago Gold Rush
The Otago gold rush (often called the Central Otago gold rush) was a gold rush that occurred during the 1860s in Central Otago, New Zealand. This was the country's biggest gold strike, and led to a rapid influx of foreign miners to the area – many of them veterans of other hunts for the precious metal in California and Victoria, Australia. The number of miners reached its maximum of 18,000 in February 1864. The rush started at Gabriel's Gully but spread throughout much of Central Otago, leading to the rapid expansion and commercialisation of the new colonial settlement of Dunedin, which quickly grew to be New Zealand's largest city. Only a few years later, most of the smaller new settlements were deserted, and gold extraction became more long-term, industrialised-mechanical process. Background Previous gold finds in New Zealand Previously gold had been found in small quantities in the Coromandel Peninsula (by visiting whalers) and near Nelson in 1842. Commercial inte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
