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Paerau
Paerau is a small settlement in inland Central Otago in New Zealand's South Island. It is located in the Strath Taieri, the upper valley of the Taieri River, at the foot of the Rock and Pillar Range. "Paerau" is a Māori-language name meaning "one hundred ridges". Despite being geographically close to Middlemarch and Roxburgh, the terrain and roads mean that Ranfurly, New Zealand, Ranfurly and Patearoa are the more closely related communities of interest. Paerau is also colloquially referred to as ''Styx''. History As well as the Taieri River the district is also home to the Styx Creek, a small tributary of the Taieri River. The creek was given the name Styx (mythology), Styx by John Turnbull Thomson (1821–1884) chief surveyor of Otago after what is in mythology, the name of one of the five rivers which all converge at the centre of the Greek underworld on a great marsh, which sometimes is also called the Styx. Upstream of the confluence of the Taieri River with the Styx Cre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Styx Creek
Styx Creek is a small to medium-sized natural stream in the Central Otago region of New Zealand. It flows into the Taieri River in the valley near Paerau, about northwest of Dunedin. It was given the name Styx by John Turnbull Thomson (1821–1884) chief surveyor of Otago after what is in mythology, the Styx (mythology), name of one of the five rivers which all converge at the centre of the Greek underworld on a great marsh, which sometimes is also called the Styx. In the Paerau district upstream of the confluence of the Taieri River with the creek, the Taieri was forded by the Old Dunstan Road (Dunstan Trail) which provided the most direct route in the 19th century from Dunedin to the Central Otago goldfields. the trail crosses the Rock and Pillar Range from Clark's Junction (near Middlemarch) and descends into the Upper Taieri, whence it crosses the Taieri River. Originally the second overnighting stop from Dunedin (after Clark's Junction), its importance meant two hotels oper ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Poolburn Reservoir
Poolburn Reservoir, also known as Poolburn Dam, is a reservoir in Central Otago, New Zealand. Built during the Great Depression for irrigation but also as an employment initiative, the water is used by farmers in the Ida Valley. Geography The reservoir is located west of the Rough Ridge Range. Long Valley Creek feeds the reservoir, and the reservoir itself feeds the Pool Burn. The Pool Burn flows into the Ida Valley, combines with the Ida Burn, and breaks through the Raggedy Range as the Poolburn Gorge before flowing into the Manuherikia River. Access There is access to Poolburn Reservoir from either Omakau in the Manuherikia Valley () or from Oturehua in the Ida Valley (). There is also access from Paerau over the Rock and Pillar Range (), but this is a dry-weather road only that can be negotiated by four-wheel drive only, and is not generally recommended. The high parts of the road are closed from early June to late September each year, and Poolburn Reservoir thus cannot be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Moss Swamp
The Great Moss Swamp (also known as the Loganburn Reservoir) is located in Otago, New Zealand. It lies in the Maniototo, close to the former gold mining route of the Old Dunstan Road, 85 kilometres to the northwest of Dunedin city centre. It is classified as a regionally significant wetland. The swamp lies on the upper surface of the Rock and Pillar Range (the Rock and Pillars are a horst range, and thus have a very flat top). Originally an actual swamp, a dam to store water for irrigation and hydroelectricity has turned the 'swamp' into a lake. The swamp is drained by the Logan Burn, which feeds into the Taieri River at Paerau. There are still significant areas of swampy wetland at the southwestern end of the lake. The Loganburn Reservoir was finished in 1983, holding about 85 million cu m of water. In 2014 the dam was raised by 80 cm, through the addition of an 80 cm-high spillway, and increasing the height of the coping wall along the top of the dam. This increas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oxbow Lake
An oxbow lake is a U-shaped lake or pool that forms when a wide meander of a river is cut off, creating a free-standing body of water. In South Texas, oxbows left by the Rio Grande are called '' resacas''. In Australia, oxbow lakes are called billabongs. The word "oxbow" can also refer to a U-shaped bend in a river or stream, whether or not it is cut off from the main stream. Geology An oxbow lake forms when a meandering river erodes through the neck of one of its meanders. This takes place because meanders tend to grow and become more curved over time. The river then follows a shorter course that bypasses the meander. The entrances to the abandoned meander eventually silt up, forming an oxbow lake. Because oxbow lakes are stillwater lakes, with no current flowing through them, the entire lake gradually silts up, becoming a bog or swamp and then evaporating completely. When a river reaches a low-lying plain, often in its final course to the sea or a lake, it meanders wi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taieri River
The Taieri River 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; 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) 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 Railway, which follows a route into Central Otago through it. In the Taieri's lower reaches there is a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock And Pillar Range
The Rock and Pillar Range of high hills is located in the Maniototo, an area of inland Otago, New Zealand. They are surrounded by the Taieri River, which has its source in the range, flowing out across the scroll plain at Paerau, before almost doubling back on itself at Waipiata and flowing back along the other side through the Strath-Taieri. The town of Middlemarch lies close to the Taieri 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 persistent and highly unusual cloud formation associated with the range. This strange cloud formation, found only in one or two places in the world, is more or less stationary and is called the Taieri Pet by the local inhabitants. It is formed by high north ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Scroll Plain
A scroll plain occurs where a river meanders across an area with a very low gradient, usually with a fairly continuous discharge. In addition to meanders, scroll plains are also characterised by many oxbow lakes. See also *Strath A strath is a large valley, typically a river valley that is wide and shallow (as opposed to a glen, which is typically narrower and deep). Word and etymology An anglicisation of the Gaelic word ''srath'', it is one of many that have been abs ... References Geography articles needing expert attention Plains Topography {{Topography-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Otago Central Railway
The Otago Central Railway (OCR) or in later years Otago Central Branch Railway, now often referred to as the Taieri Gorge Railway, was a secondary railway line in Central Otago, in the South Island of New Zealand. Construction Construction of the OCR began in 1877 and the 27-km section to Hindon was opened in 1889. The line was completed to Middlemarch two years later. The 26 km section of line from Middlemarch to Hyde then opened in 1894. This was followed by the 16 km section from Hyde to Kokonga which opened in 1897. The section to Ranfurly opened in December 1898. The Ranfurly to Wedderburn section opened in 1900 followed by the Wedderburn to Ida Valley section which opened in 1901. The line was opened to Omakau in 1904. Omakau-Chatto Creek opened in July 1906 followed by the line reaching Alexandra in December 1906. The line was opened to Clyde in April 1907. There then followed a delay until the section through the Cromwell Gorge was resumed in 1914. The line re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gaol
A prison, also known as a jail, gaol (dated, standard English, Australian, and historically in Canada), penitentiary (American English and Canadian English), detention center (or detention centre outside the US), correction center, correctional facility, lock-up, hoosegow or remand center, is a facility in which inmates (or prisoners) are confined against their will and usually denied a variety of freedoms under the authority of the state as punishment for various crimes. Prisons are most commonly used within a criminal justice system: people charged with crimes may be imprisoned until their trial; those pleading or being found guilty of crimes at trial may be sentenced to a specified period of imprisonment. In simplest terms, a prison can also be described as a building in which people are legally held as a punishment for a crime they have committed. Prisons can also be used as a tool of political repression by authoritarian regimes. Their perceived opponents may be impri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
