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Strath-Taieri
Strath Taieri is a large glacial valley and river plateau in New Zealand's South Island. It is surrounded by the rugged hill ranges to the north and west of Otago Harbour. Since 1989 it has been part of the city of Dunedin. The small town of Middlemarch is located at its southern end. The name is a hybrid word, from '' Strath'' (anglicised Irish and Scots Gaelic ''srath''), meaning a broad river valley, and the Māori name ''Taieri'' (alternative spelling Taiari) of the river which runs through it. History There is evidence that moa hunters (1300-1500) were once active on the Strath Taieri, the Taieri Gorge, at Deep Stream and Rocklands on the adjacent plateau to the south. A Māori route from the coast to the interior lay along the valley. Activity during the Classic period (1500–1642) is attested by a cave discovered in 1949 with its entrance blocked containing the bodies of a Māori woman and child. It is not clear if they were trapped deliberately or by accident. Thi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middlemarch, New Zealand
Middlemarch is a small town in the Otago region of New Zealand's South Island. It lies at the foot of the Rock and Pillar Range of hills in the broad Strath-Taieri valley, through which flows the middle reaches of the Taieri River. Since local government reorganisation in the late 1980s, Middlemarch and much of the Strath-Taieri has been administered as part of Dunedin city, the centre of which lies some 80 km to the southeast. Middlemarch is part of the Taieri electorate (formerly known as Dunedin South), and is currently represented in parliament by Ingrid Leary. Middlemarch has reticulated sewerage but no reticulated water supply. A description of 1903, that " e summer seasons are warm, but not enervating, and the winters cold, but dry" is still true today. It is a crucial service town for the local farming community, the terminus of the Taieri Gorge Railway, and the start of the Otago Central Rail Trail. Several suggestions exist about how the township was named. On ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 absorbed into the English and Scots languages. It is commonly used in rural Scotland to describe a wide valley, even by non-Gaelic speakers. In Scottish place-names, ''Strath-'' is of Gaelic and Brittonic origin. ''Strath-'' names have the genesis with Gaelic ''srath'' meaning "broad-valley", as well as with the Cumbric and Pictish cognates (c.f. Welsh ''ystrad''). Gaelic ''srath'' is derived from Old Irish ''srath'', recorded as having meant "grassland". The modern Scottish Gaelic sense of "broad-valley", paralleling the meaning of Brittonic cognates, developed from substrate influence from Pictish. Toponymy It occurs in numerous place names within Scotland including Strathspey and Strathclyde. Internationally, many places with Sc ... [...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 a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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, 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, 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 curli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dunstan Trail
Dunstan Trail, also known as Old Dunstan Road, is a historic route in Otago, New Zealand. The road was created during the Central Otago Gold Rush of the 1860s. At the time of the road's creation, it was the shortest route from the city of Dunedin to the goldfields around Clyde, or Dunstan as it was then known. Known at the time as "The Mountain Track", it was a dangerous route which claimed numerous lives.The Dunstan Trail , ''www.centralotagonz.com''. Retrieved 9 June 2019. The road begins at in Strath-Taieri, where it meets [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antimony
Antimony is a chemical element with the symbol Sb (from la, stibium) and atomic number 51. A lustrous gray metalloid, it is found in nature mainly as the sulfide mineral stibnite (Sb2S3). Antimony compounds have been known since ancient times and were powdered for use as medicine and cosmetics, often known by the Arabic name kohl. The earliest known description of the metal in the West was written in 1540 by Vannoccio Biringuccio. China is the largest producer of antimony and its compounds, with most production coming from the Xikuangshan Mine in Hunan. The industrial methods for refining antimony from stibnite are roasting followed by reduction with carbon, or direct reduction of stibnite with iron. The largest applications for metallic antimony are in alloys with lead and tin, which have improved properties for solders, bullets, and plain bearings. It improves the rigidity of lead-alloy plates in lead–acid batteries. Antimony trioxide is a prominent additive f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hindon, New Zealand
Hindon is a small settlement in inland Otago, in the South Island of New Zealand. It is located northwest of Dunedin in the Silverpeaks Range, close to the edge of the Strath Taieri. The Taieri Gorge Railway runs through Hindon on its way between Dunedin and Middlemarch. Hindon was named by provincial superintendent John Hyde Harris, who owned land in the area, though the origin of the name is not known. The area was a centre of activity during the latter part of the Otago Gold Rush, with several mines working the gold-bearing quartz reefs A reef is a ridge or shoal of rock, coral or similar relatively stable material, lying beneath the surface of a natural body of water. Many reefs result from natural, abiotic processes—deposition of sand, wave erosion planing down rock out ... at Hindon and nearby Barewood. The size of the township dwindled markedly after the end of the rush. Little remains of the mines, though some subsided shafts remain as hazards for local far ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Colin McCahon
Colin John McCahon (; 1August 191927May 1987) was a prominent New Zealand artist whose work over 45 years consisted of various styles, including landscape, figuration, abstraction, and the overlay of painted text. Along with Toss Woollaston and Rita Angus, McCahon is credited with introducing modernism to New Zealand in the mid-20th century. He is regarded as New Zealand's most important modern artist, particularly in his landscape work. Early life and education McCahon was born in Timaru on 1 August 1919 the second of three children of Ethel Beatrice Ferrier and her husband John Kernohan McCahon. He spent most of his childhood in Dunedin, although his family lived in Oamaru for one year. He showed an early interest in art, influenced by regular visits to exhibitions and the work of his maternal grandfather, photographer and painter William Ferrier, which hung in the family home. He attended the Maori Hill Primary School and Otago Boys' High School, which he called: "the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Macraes Flat
Macraes, formerly known as Macraes Flat, and known in Māori as Ōtī,Place names'' on Kāti Huirapa Runaka ki Puketeraki website, viewed 2012-01-04 is a town in the Waitaki District in Otago, New Zealand. It is known as a mining town, with a long history of gold extraction. The town sits 55 km north of Dunedin in New Zealand's South Island. The Macraes Mine, New Zealand New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island count ...'s largest gold mine, is nearby. The settlement was named after John McRae, who lived in the area in the late 1850s before gold was discovered nearby. In 2015 the name of the town was officially altered from Macraes Flat to Macraes. References Waitaki District Populated places in Otago Mining communities in New Zealand {{Otago-geo-stub ... [...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 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture reflects a high content of platy minerals, such as micas, talc, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building ( orogeny) and usually reflects a medium grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is usually given a name reflecting its protolith, such as ''sch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
