Waipiata
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Waipiata
Waipiata is an historic place on the Otago Central Rail Trail, in Central Otago, New Zealand. Waipiata is also the name of many New Zealand coastal vessels, steamers, freighters and steamships. History Waipiata became a thriving township as the Otago Central Railway line snaked across the Maniototo Plain. A school opened in 1891. The nearby village of Kokonga was the railway camp. In 1914 the Waipiata Sanatorium, a private facility owned by Dr George Byres was constructed, a few kilometres south of Waipiata near the old Hamiltons gold field. In the early 1920s Dr Byres' facility was taken over by the Hospital Board and continued for a long period as a sanatorium for tuberculosis patients. The sanatorium closed in 1961 and the buildings became a corrective and training centre for the Justice Department until 1979, after which the government sold the site. Today it remains a privately owned property. A factory with 78 employees processed rabbits from 1901 at Coneys Creek (Green Brid ...
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Waipiata Children
Waipiata is an historic place on the Otago Central Rail Trail, in Central Otago, New Zealand. Waipiata is also the name of many New Zealand coastal vessels, steamers, freighters and steamships. History Waipiata became a thriving township as the Otago Central Railway line snaked across the Maniototo Plain. A school opened in 1891. The nearby village of Kokonga was the railway camp. In 1914 the Waipiata Sanatorium, a private facility owned by Dr George Byres was constructed, a few kilometres south of Waipiata near the old Hamiltons gold field. In the early 1920s Dr Byres' facility was taken over by the Hospital Board and continued for a long period as a sanatorium for tuberculosis patients. The sanatorium closed in 1961 and the buildings became a corrective and training centre for the Justice Department until 1979, after which the government sold the site. Today it remains a privately owned property. A factory with 78 employees processed rabbits from 1901 at Coneys Creek (Green Brid ...
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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 ...
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Maniototo
The Maniototo Plain, usually simply known as The Maniototo, 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, New Zealand, Ranfurly, Naseby, New Zealand, 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 Central Otago goldrush, and relics from that era can still be seen around the towns of Kyeburn, Naseby, New Zealand, Naseby, and Saint Bathans, New Zealand, St. Bathans. Sheep farming is the major source of income. The a ...
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Otago Central Rail Trail
The Otago Central Rail Trail is a 150-kilometre walking, cycling and horse riding track in the South Island of New Zealand. A pioneering project for New Zealand, the successful rail trail joined the New Zealand Cycle Trail umbrella organisation in 2012, having been one of the inspirations for it. The trail runs in an arc between Middlemarch and Clyde, along the route of the former Otago Central Railway. The trail has become a popular tourist attraction, with 10,000–12,000 users per year as a conservative estimate, and yearly (and ongoing) user increases for 6 out of the last 7 years (as of 2011). The trail is also accepted as being, by a large margin, the biggest non-farming economic factor in the Maniototo-Alexandra area. History The original railway line was completed at the turn of the 20th century, and provided a link between Central Otago and Dunedin until closure in 1990. The first 64 km from the junction with the Main South Line in Wingatui remain operational; the i ...
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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 milk bar. History During the Central Otago goldrush 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 ...
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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 Central 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 * Adams Ri ...
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The Lord Of The Rings (film Series)
''The Lord of the Rings'' is a film series, series of three epic film, epic fantasy film, fantasy adventure films directed by Peter Jackson, based on the novel ''The Lord of the Rings'' by J. R. R. Tolkien. The films are subtitled ''The Lord of the Rings: The Fellowship of the Ring, The Fellowship of the Ring'' (2001), ''The Lord of the Rings: The Two Towers, The Two Towers'' (2002), and ''The Lord of the Rings: The Return of the King, The Return of the King'' (2003). Produced and distributed by New Line Cinema with the co-production of WingNut Films, the series is an international venture between New Zealand and the United States. The films feature an ensemble cast including Elijah Wood, Ian McKellen, Liv Tyler, Viggo Mortensen, Sean Astin, Cate Blanchett, John Rhys-Davies, Christopher Lee, Billy Boyd (actor), Billy Boyd, Dominic Monaghan, Orlando Bloom, Hugo Weaving, Andy Serkis and Sean Bean. Set in the fictional world of Middle-earth, the films follow the hobbit Frodo Baggi ...
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Central 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 Gold Rush, California and Victorian Gold Rush, 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, New Zealand, Nelson in 1842. Commercial interests in Auc ...
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Asthenosphere
The asthenosphere () is the mechanically weak and ductile region of the upper mantle of Earth. It lies below the lithosphere, at a depth between ~ below the surface, and extends as deep as . However, the lower boundary of the asthenosphere is not well defined. The asthenosphere is almost solid, but a slight amount of melting (less than 0.1% of the rock) contributes to its mechanical weakness. More extensive decompression melting of the asthenosphere takes place where it wells upwards, and this is the most important source of magma on Earth. It is the source of mid-ocean ridge basalt (MORB) and of some magmas that erupted above subduction zones or in regions of continental rifting. Characteristics The asthenosphere is a part of the upper mantle just below the lithosphere that is involved in plate tectonic movement and isostatic adjustments. It is composed of peridotite, a rock containing mostly the minerals olivine and pyroxene. The lithosphere-asthenosphere boundary is con ...
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Maniototo Area School
Maniototo Area School is an area school in Ranfurly, Central Otago, New Zealand, serving students aged 5–18. Founded in 1879,''From Eweburn to Maniototo Area School, 125 Years of Change'' - Jack Rutherford it has students as of The school has a strong sporting tradition and an academic programme bolstered by video conferencing lessons and the OtagoNet project. Maniototo Area School hosts international students aged 11–18. It is located near a winter sports centre and the Otago Rail Trail. One area of special interest at the school is 'Bute Beds'. These are two fully furnished houses rented out as 'Bed and Breakfast' units by the school. These are used to support social studies projects and to provide extra resources. Notable alumni * Sean Becker – curler * Tania Murray – high jumper and triple jumper * Warren Dobson – curler * Andrew Hore – rugby union player * Tony Kreft – rugby union player * Peter Petherick Peter James Petherick (25 September 194 ...
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Central Otago
Central Otago is located in the inland part of the Otago region in the South Island of New Zealand. The motto for the area is "A World of Difference". The area is dominated by mountain ranges and the upper reaches of the Clutha River and tributaries. The wide flat plateau of the Maniototo which lies between the upper reaches of the Taieri River and the Clutha's northern tributary the Manuherikia River, Manuherikia is also part of Central Otago. Characterised by cold winters and hot, dry summers, the area is only lightly populated. First significant European occupation came with the discovery of gold at Gabriel's Gully near Lawrence, New Zealand, Lawrence in 1861, which led to the Central Otago goldrush. Other towns and villages include Alexandra, New Zealand, Alexandra, Bannockburn, New Zealand, Bannockburn, Clyde, New Zealand, Clyde, Cromwell, New Zealand, Cromwell, Millers Flat, New Zealand, Millers Flat, Naseby, New Zealand, Naseby, Omakau, Ranfurly, New Zealand, Ranfurly, Rox ...
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Magma
Magma () is the molten or semi-molten natural material from which all igneous rocks are formed. Magma is found beneath the surface of the Earth, and evidence of magmatism has also been discovered on other terrestrial planets and some natural satellites. Besides molten rock, magma may also contain suspended crystals and gas bubbles. Magma is produced by melting of the mantle or the crust in various tectonic settings, which on Earth include subduction zones, continental rift zones, mid-ocean ridges and hotspots. Mantle and crustal melts migrate upwards through the crust where they are thought to be stored in magma chambers or trans-crustal crystal-rich mush zones. During magma's storage in the crust, its composition may be modified by fractional crystallization, contamination with crustal melts, magma mixing, and degassing. Following its ascent through the crust, magma may feed a volcano and be extruded as lava, or it may solidify underground to form an intrusion, such as a ...
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