Hector Mountains
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Hector Mountains
The Tapuae-o-Uenuku / Hector Mountains are a mountain range in the New Zealand region of Otago, near the resort town of Queenstown and just south of the more famous Remarkables. For most of its length, the mountains run adjacent to the southern reaches of Lake Wakatipu, before extending approximately further south, past the glacial moraine at Kingston on the southern end of the lake. On their eastern side, the mountains mark the edge of the Nevis valley, a largely tussocked area which saw significant activity during the Otago Gold Rush of the 1860s. Historically, the mountains were an important ''mahinga kai'' (food gathering-place) for Ngāi Tahu and other local Māori iwi, who used the area to hunt for weka and gather tikumu while visiting the region. Many of the peaks in the range remain unnamed, a group which until 2013 included its highest point. Following a joint process between Ngāi Tahu and the Central Otago District Council, four new names were added to the r ...
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The Remarkables
The Remarkables ( mi, Kawarau) are a mountain range and skifield in Otago in the South Island of New Zealand. Located on the southeastern shore of Lake Wakatipu, the range lives up to its name by rising sharply to create a remarkable backdrop for the waters. The range is clearly visible from the nearby town of Queenstown. The highest point in the range is Single Cone (2319 metres). The adjacent Tapuae-o-Uenuku / Hector Mountains southeast of the Remarkables culminate in Mount Tūwhakarōria (2307 m). There are a number of small lakes on the mountains including Lake Alta which forms part of the Remarkables Skifield. Name The original Ngāi Tahu inhabitants called the mountains , and gave the same name to the Kawarau River which starts beneath them. The mountains were named The Remarkables by Alexander Garvie in 1857-58, allegedly because they are one of only two mountain ranges in the world which run directly north to south. An alternate explanation for the name given by l ...
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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 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 interests in Auckland offered a £500 prize for anyone who could find payable qu ...
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Mataura River
The Mataura River is in the Southland Region of the South Island of New Zealand. It is long. Description The river's headwaters are located in the Eyre Mountains to the south of Lake Wakatipu. From there it flows southeast towards Gore, New Zealand, Gore, where it turns southward. It then passes through the town of Mataura, and enters the Pacific Ocean at Toetoes Bay on the southern coast of the South Island. Much of its channel is braided river, braided. The Mataura is renowned as a source of brown trout, and is a popular fishing venue, including whitebaiting. It has been identified as an Important Bird Area by BirdLife International because it supports breeding colonies of the endangered species, endangered black-billed gull. History Until about 18,000 years ago the Mataura drained Lake Wakatipu. The Kingston Flyer follows part of the former river bed, now blocked by glacial moraine. For Māori people, Māori, the Mataura was an important (traditional travel route) th ...
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Nevis River
The Nevis River is in Otago, New Zealand. It flows north for through rough country before meeting the Kawarau River, of which it is a tributary. A prominent rock outcrop close to this junction is known as the Nevis Bluff. The river was one of the sites of the Central Otago goldrush of the 1860s. Today, the region around the river is known for tourism and wine production. New Zealand's highest bungy jumping operation, the Nevis Highwire is above the river. A Water Conservation Order A water conservation order is a legal ruling to protect aspects of water bodies. It may be to protect the quantity of the water itself or for any issues relating to the water body as a whole. New Zealand In New Zealand, a Water Conservation Order i ... protects the river for its wild and scenic character and for recreational use, especially fishing and kayaking. The Water Conservation Order made provision for damming the river for hydro-electric development. Fish and Game New Zealand applied t ...
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Cardrona, New Zealand
Cardrona is the name of a locality in the Cardrona Valley in New Zealand, with the nearby skifield of Cardrona Alpine Resort and Mount Cardrona also using the same name. Established as a gold rush township in the 1860s on the banks of the small river of the same name, it is known for its distinctive hotel of gold rush vintage which is on the opposite side of the river to the original township of which few buildings remain. It is in a scenic setting on the Crown Range road which connects Wanaka and Queenstown. Recent developments include expanded facilities for guest accommodation at Benbrae Resort, recreational facilities, a distillery,. and a 400-house suburb. Cardrona is the home of the internationally known Race to the Sky hillclimb which was last held in 2015. History The name was given to the area by J. T. Thomson after the Scottish village of Cardrona. A long history, including the now almost-forgotten contribution of the labour from thousands of Chinese worke ...
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Pliocene
The Pliocene ( ; also Pleiocene) is the epoch in the geologic time scale that extends from 5.333 million to 2.58See the 2014 version of the ICS geologic time scale
million years ago. It is the second and most recent epoch of the Neogene Period in the . The Pliocene follows the Epoch and is followed by the Epoch. Prior to the 2009 ...
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Tectonic Uplift
Tectonic uplift is the geologic uplift of Earth's surface that is attributed to plate tectonics. While isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of crustal thickening (such as mountain building events), changes in the density distribution of the crust and underlying mantle, and flexural support due to the bending of rigid lithosphere. Tectonic uplift results in denudation (processes that wear away the earth's surface) by raising buried rocks closer to the surface. This process can redistribute large loads from an elevated region to a topographically lower area as well – thus promoting an isostatic response in the region of denudation (which can cause local bedrock uplift). The timing, magnitude, and rate of denudation can be estimated by geologists using pressure-temperature studies. Crustal thickening Crustal thickening has an upward component of motion and often occurs when continental crus ...
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South Island
The South Island, also officially named , is the larger of the two major islands of New Zealand in surface area, the other being the smaller but more populous North Island. It is bordered to the north by Cook Strait, to the west by the Tasman Sea, and to the south and east by the Pacific Ocean. The South Island covers , making it the world's 12th-largest island. At low altitude, it has an oceanic climate. The South Island is shaped by the Southern Alps which run along it from north to south. They include New Zealand's highest peak, Aoraki / Mount Cook at . The high Kaikōura Ranges lie to the northeast. The east side of the island is home to the Canterbury Plains while the West Coast is famous for its rough coastlines such as Fiordland, a very high proportion of native bush and national parks, and the Fox and Franz Josef Glaciers. The main centres are Christchurch and Dunedin. The economy relies on agriculture and fishing, tourism, and general manufacturing and services. ...
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Lake Te Kōhua
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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Cromwell, New Zealand
Cromwell (Māori: ''Tīrau'') is a town in Central Otago in the Otago region of New Zealand. Geography Cromwell is between (linking to Wānaka, north, and Queenstown via the Kawarau Gorge, west) and State Highway 8 leading to the Lindis Pass, northeast, and Alexandra, 33 km south. The road to Alexandra winds through the Cromwell Gorge. A point near Cromwell lies 119 kilometres from the sea, the farthest from the sea anywhere in New Zealand. A prominent feature surrounding much of the town is the man-made Lake Dunstan. Nearby settlements are at Bannockburn, Lowburn, Tarras, and Ripponvale. Cromwell has a strategic location between the Lindis and the Haast passes, and acts as a hub between the towns of Wānaka, Queenstown and Alexandra. Cromwell is also the home of the Cromwell Chafer Beetle ''(Prodontria lewisi)''. The 45th parallel south runs just north of the township. Cromwell lay at the confluence of the Clutha River and the Kawarau River, which wa ...
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Central Otago District Council
Central Otago District Council is the territorial authority for the Central Otago District of New Zealand. The council is led by the mayor of Central Otago The Mayor of Central Otago officiates over the Central Otago District of New Zealand which is administered by the Central Otago District Council. The first Mayor of Central Otago was W.S. McIntosh who was elected in 1989, when following the local ..., 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), Alex ...
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