Peter Seton Hay
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Peter Seton Hay
Peter Seton Hay (1852–19 March 1907) was a New Zealand civil engineer and public servant. He was born in Glasgow, Lanarkshire, Scotland on 12 July 1852. He was brought to Dunedin in April 1860. In 1875, he joined the Public Works Department, as an engineering cadet, and was awarded a University of Otago BA in 1877 and an MA in 1878. He married Mary Clarke on 22 April 1879 and was survived by her, four sons and a daughter. Peter Seton Hay helped build parts of the Main South Line, Central Otago, Midland and Catlins River railways, before moving to the Wellington head office in 1884. His works then included Timaru Harbour, the NIMT (with the Makohine, Mangaweka, Hapuawhenua, Taonui, Manganui-a-te-ao and Makatote viaducts), Awatere bridge; Farewell Spit Lighthouse, Rakaia Gorge Bridge, Christchurch Exhibition towers, Motueka Harbour and reports on the hydroelectric potential of the Waikato, Waikaremoana, Mangawhero–Wanganui and Lakes Coleridge, Hawea, Te Anau ...
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Glasgow
Glasgow ( ; sco, Glesca or ; gd, Glaschu ) is the most populous city in Scotland and the fourth-most populous city in the United Kingdom, as well as being the 27th largest city by population in Europe. In 2020, it had an estimated population of 635,640. Straddling the border between historic Lanarkshire and Renfrewshire, the city now forms the Glasgow City Council area, one of the 32 council areas of Scotland, and is governed by Glasgow City Council. It is situated on the River Clyde in the country's West Central Lowlands. Glasgow has the largest economy in Scotland and the third-highest GDP per capita of any city in the UK. Glasgow's major cultural institutions – the Burrell Collection, Kelvingrove Art Gallery and Museum, the Royal Conservatoire of Scotland, the Royal Scottish National Orchestra, Scottish Ballet and Scottish Opera – enjoy international reputations. The city was the European Capital of Culture in 1990 and is notable for its architecture, cult ...
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Rakaia Gorge
The Rakaia Gorge is located on the Rakaia River in inland Canterbury in New Zealand's South Island. Like its neighbour, the Waimakariri River, the Rakaia runs through wide shingle beds for much of its length, but is forced through a narrow canyon as it approaches the Canterbury Plains. In the 1870s, there were proposals to extend the Whitecliffs Branch railway into the Rakaia Gorge, and an 1880 Royal Commission on New Zealand's railway network was in favour of this proposal, but it never came to fruition. The Rakaia Gorge bridge was completed in 1882 and provides an inland alternative to the more frequently used Rakaia River bridge just north of the town of Rakaia. The bridge carries State Highway 77 and the Inland Scenic Route and connects the settlements of Glentunnel and Methven Swimming at the top bridges of the gorge is a favoured pastime for locals and tourists alike. Swimming in the main river can be done but only by strong swimmers. There is a perfect swimming ho ...
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1853 Births
Events January–March * January 6 – Florida Governor Thomas Brown signs legislation that provides public support for the new East Florida Seminary, leading to the establishment of the University of Florida. * January 8 – Taiping Rebellion: Zeng Guofan is ordered to assist the governor of Hunan in organising a militia force to search for local bandits. * January 12 – Taiping Rebellion: The Taiping army occupies Wuchang. * January 19 – Giuseppe Verdi's opera ''Il Trovatore'' premieres in performance at Teatro Apollo in Rome. * February 10 – Taiping Rebellion: Taiping forces assemble at Hanyang, Hankou, and Wuchang, for the march on Nanjing. * February 12 – The city of Puerto Montt is founded in the Reloncaví Sound, Chile. * February 22 – Washington University in St. Louis is founded as Eliot Seminary. * March – The clothing company Levi Strauss & Co. is founded in the United States. * March 4 – Inauguration of Franklin Pierce as 14th President of the ...
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Waiouru
Waiouru is a small town in the Ruapehu District, in New Zealand's Manawatū-Whanganui region. It is located on the south-eastern North Island Volcanic Plateau, north of Palmerston North and 25 kilometres south-east of Mount Ruapehu. The town had a population of 765 in the 2018 census. The main attraction of Waiouru is the National Army Museum, opened in 1978, which features static displays of New Zealand's military heritage. The rest of the township consists of a small cluster of a police station, two garages, a petrol station/postal agency, a panel beater, two motels, a tavern and half a dozen cafe/restaurants spread along the highway. There are three unmanned diesel refueling sites for the 700+ big freight trucks that pass through Waiouru each day. Nearby are the yards of a roading contractor and a maintenance contractor. A grocery store, hairdresser and beautician are in the Army housing area two kilometres away, and a medical centre, public library, cafe and department s ...
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Pleurisy
Pleurisy, also known as pleuritis, is inflammation of the membranes that surround the lungs and line the chest cavity (pleurae). This can result in a sharp chest pain while breathing. Occasionally the pain may be a constant dull ache. Other symptoms may include shortness of breath, cough, fever, or weight loss, depending on the underlying cause. The most common cause is a viral infection. Other causes include bacterial infection, pneumonia, pulmonary embolism, autoimmune disorders, lung cancer, following heart surgery, pancreatitis and asbestosis. Occasionally the cause remains unknown. The underlying mechanism involves the rubbing together of the pleurae instead of smooth gliding. Other conditions that can produce similar symptoms include pericarditis, heart attack, cholecystitis, pulmonary embolism, and pneumothorax. Diagnostic testing may include a chest X-ray, electrocardiogram (ECG), and blood tests. Treatment depends on the underlying cause. Paracetamol (acetaminop ...
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Lake Manapouri
Lake Manapouri is located in the South Island of New Zealand. The lake is situated within the Fiordland National Park and the wider region of Te Wahipounamu South West New Zealand World Heritage Area. Māori History According to Māori people, Māori legend Lake Manapouri was created by the tears of two sisters, Moturua and Koronae, who were daughters of an old chief in the region. Koronae journeyed deep into the forest one day only to become stranded after a fall. Her sister Moturua went looking for her and when she found Koronae she realised that Koronae could not be rescued. Moturua lay with Koronae and there they lay until they died, their tears creating Lake Manapouri. Lake Manapouri means anxious or sorrowful heart because of the grief of the two sisters. However, the present name was given by mistake. An early settler accidentally called it by the name of one of the Mavora Lakes, which lie between Lake Te Anau and Lake Wakatipu. The original name of the lake is believ ...
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Lake Te Anau
Lake Te Anau is in the southwestern corner of the South Island of New Zealand. The lake covers an area of , making it the second-largest lake by surface area in New Zealand (after Lake Taupō) and the largest in the South Island. It is the largest lake in Australasia by fresh water volume. The main body of the lake runs north-south, and is 65 km in length. Three large fiords form arms to the lake on its western flank: North Fiord, Middle Fiord and South Fiord. These are the only inland fiords that New Zealand has, the other 14 are out on the coast. Several small islands lie in the entrance to Middle Fiord, which forks partway along its length into northwest and southwest arms. The surface of the lake is at an altitude of 210 m. It has a maximum depth of 417 m, so much of its bed lies below sea level, with the deepest part of the lake being 226 metres below sea level. Several rivers feed the lake, of which the most important is the Eglinton River, which joins the lake from ...
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Lake Hāwea
Lake Hāwea is New Zealand's List of lakes in New Zealand#Largest lakes, ninth largest lake. The lake is in the Otago Region at an altitude of 348 metres. It covers 141 km² and reaches 392 metres deep. Lake Hāwea is named after a Māori people, Māori tribe who preceded the Waitaha (South Island iwi), Waitaha people in the area. Lake Hāwea stretches 35 kilometres from north to south. It lies in a U-shaped valley, glacial valley formed during the last ice age, and is fed by the Hunter River (New Zealand), Hunter River. Nearby Lake Wānaka lies in a parallel glacial valley eight kilometres to the west. At their closest point, a rocky ridge called The Neck, the lakes are only 1000 metres apart. Lake Hāwea is dammed to the south by an ancient terminal moraine created some 10,000 years ago. In 1958 the lake was artificially raised 20 metres to store more water for increased hydroelectric power generation at the Roxburgh Dam. The only flat land around the lake is at its s ...
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Lake Coleridge
Lake Coleridge ( mi, Whakamatau) is located in inland Canterbury, in New Zealand's South Island. Located to the northwest of Methven, it has a surface area of . The lake is situated in an over-deepened valley formed by a glacier over 20,000 years ago in the Pleistocene era. It currently has no natural outflows. There is a small settlement at the lake. Ecology Early colonial explorers found the shores of the lake covered in mānuka (or kānuka), kōwhai, cabbage trees, flax and general swamp plants. The lake was also surrounded by Southern Rata trees, and native beech trees. The lake itself was fairly lacking in aquatic plants due to a lack of nutrients. The lake was known for a population of large eels. Human activity has significantly changed the ecology. Colonial settlers introduced game fish including rainbow trout, brown trout, Atlantic salmon and Chinook salmon. The changing water levels caused by the operation of the Coleridge Power Station killed most of the ...
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Tongariro Power Scheme
The Tongariro Power Scheme is a 360 MW hydroelectricity scheme in the central North Island of New Zealand. The scheme is currently operated by electricity generation company Genesis Energy. The scheme takes water from tributaries of the Rangitikei, Whangaehu, Whanganui, and Tongariro rivers, which drain a area covering Ruapehu, Ngauruhoe, Tongariro and the western Kaimanawa Ranges. The water is then sent through a large canal and tunnel system to generate electricity at three hydro power stations, located at Rangipo (120 MW), Tokaanu (240 MW) and Mangaio (2MW). The water is then drained into Lake Taupō where it is stored for further use in the succession of Waikato River power stations. The scheme generates approximately 1350 GWh of electricity annually, and contributes 4 percent of New Zealand's electricity generation. History Plans to realise the potential of electricity generation in the central North Island volcanic plateau date back to the early years of the 20th centu ...
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Lake Waikaremoana
Lake Waikaremoana is located in Te Urewera in the North Island of New Zealand, 60 kilometres northwest of Wairoa and 80 kilometres west-southwest of Gisborne. It covers an area of . From the Maori Waikaremoana translates as 'sea of rippling waters'. The lake lies in the heart of Tuhoe country. The hamlet of Aniwaniwa and the Waikaremoana Holiday Park are located on the lakeshore, along SH38 (from Wai-O-Tapu via Murupara to Wairoa), which connects the lake to the central North Island (Rotorua) and Gisborne. There is a Department of Conservation office at Aniwaniwa. Several walks start here, including a short stroll to Aniwaniwa Falls. The village of Onepoto is located on the lake's southern shores, close to the lake's old overflow channel and the intake of the Waikaremoana hydroelectric power scheme. The name Onepoto means short beach , and refers to the small bay to the north of the village with a beach only 60 metres long.Wises New Zealand Guide, 7th edition 1979 Lake Wa ...
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Waikato River
The Waikato River is the longest river in New Zealand, running for through the North Island. It rises on the eastern slopes of Mount Ruapehu, joining the Tongariro River system and flowing through Lake Taupō, New Zealand's largest lake. It then drains Taupō at the lake's northeastern edge, creates the Huka Falls, and flows northwest through the Waikato Plains. It empties into the Tasman Sea south of Auckland, at Port Waikato. It gives its name to the Waikato region that surrounds the Waikato Plains. The present course of the river was largely formed about 17,000 years ago. Contributing factors were climate warming, forest being reestablished in the river headwaters and the deepening, rather than widening, of the existing river channel. The channel was gradually eroded as far up river as Piarere, leaving the old Hinuera channel through the Hinuera Gap high and dry. The remains of the old course are seen clearly at Hinuera, where the cliffs mark the ancient river edges. The Wai ...
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