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Waimakariri River
The Waimakariri River is one of the largest rivers in Canterbury, on the eastern coast of New Zealand's South Island. It flows for in a generally southeastward direction from the Southern Alps across the Canterbury Plains to the Pacific Ocean. The river rises on the eastern flanks of the Southern Alps, eight kilometres southwest of Arthur's Pass. For much of its upper reaches, the river is braided, with wide shingle beds. As the river approaches the Canterbury Plains, it passes through a belt of mountains, and is forced into a narrow canyon (the Waimakariri Gorge), before reverting to its braided form for its passage across the plains. It enters the Pacific north of Christchurch, near the town of Kaiapoi. Instead of being unoccupied Crown land as are most New Zealand river beds, the bed of the Waimakariri River is vested in the Canterbury Regional Council (Environment Canterbury). Name The name ''Waimakariri'' comes from the Māori words ''wai'', meaning ''water'', and ''makari ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canterbury, New Zealand
Canterbury ( mi, Waitaha) is a region of New Zealand, located in the central-eastern South Island. The region covers an area of , making it the largest region in the country by area. It is home to a population of The region in its current form was established in 1989 during nationwide local government reforms. The Kaikoura District joined the region in 1992 following the abolition of the Nelson-Marlborough Regional Council. Christchurch, the South Island's largest city and the country's second-largest urban area, is the seat of the region and home to percent of the region's population. Other major towns and cities include Timaru, Ashburton, Rangiora and Rolleston. History Natural history The land, water, flora, and fauna of Waitaha/Canterbury has a long history stretching from creation of the greywacke basement rocks that make up the Kā Tiritiri o te Moana/Southern Alps to the arrival of the first humans. This history is linked to the creation of the earth, the s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Braided River
A braided river, or braided channel, consists of a network of river channels separated by small, often temporary, islands called braid bars or, in English usage, ''aits'' or ''eyots''. Braided streams tend to occur in rivers with high sediment loads or coarse grain sizes, and in rivers with steeper slopes than typical rivers with straight or meandering channel patterns. They are also associated with rivers with rapid and frequent variation in the amount of water they carry, i.e., with "flashy" rivers, and with rivers with weak banks. Braided channels are found in a variety of environments all over the world, including gravelly mountain streams, sand bed rivers, on alluvial fans, on river deltas, and across depositional plains. Description A braided river consists of a network of multiple shallow channels that diverge and rejoin around ephemeral ''braid bars''. This gives the river a fancied resemblance to the interweaved strands of a braid. The braid bars, also known as channel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waipara River (Canterbury)
The Waipara River is a river in Canterbury in the South Island of New Zealand. The river is about long, and its catchment area is . nvironment Canterbury The river passes through the small town of on its southeastward journey to the at the northern end of near [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ashley River / Rakahuri
The Ashley River (; officially Ashley River / Rakahuri) is in Canterbury region of New Zealand. It flows generally southeastwards for before entering the Pacific Ocean at Waikuku Beach, Pegasus Bay north of Christchurch. The town of Rangiora is close to the south bank of the Ashley River. The river's official name was changed from Ashley River to the dual name Ashley River / Rakahuri by the Ngāi Tahu Claims Settlement Act 1998. Though the lower reaches of the river are braided, part of the upper river flows through a canyon known as the Ashley Gorge. The river emanates from mountains in the west Lees Valley adjacent to Island Hills station and exits the hills at a gorge near Oxford township. It has tributaries of Duck Creek in this valley and is an accumulator of watershed between Lees Valley and Oxford township. Behind Waikuku Beach is one of the largest, least modified estuaries in New Zealand. It is abundant in bird life, including the wrybill (''Anarhynchus frontalis'') ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pegasus Bay
Pegasus Bay, earlier known as Cook's Mistake, is a bay on the east coast of the South Island of New Zealand, to the north of Banks Peninsula. Toponymy Pegasus Bay takes its name from the brig ''Pegasus'', a sealing ship that was sailing from Hobart to London via the ''sealing islands'' and was surveying this part of the South Island in 1809. Attempting to sail into Gore's Bay shown on Captain Cook's map between the supposed ''Island'' that Cook had named after Banks, the crew discovered a mistake in Cook's chart and found the island was a peninsula connected to the rest of the South Island mainland by a low-lying isthmus. Fortunately they discovered this before trying to pass between the supposed island and the mainland before dark while approaching from the north and were still in about of water. Captain Chace (or Chase) and his first officer William Stewart, who had also surveyed Stewart Island on the same journey, were reported in the Oriental Navigator in 1816. Charts ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banks Peninsula
Banks Peninsula is a peninsula of volcanic origin on the east coast of the South Island of New Zealand. It has an area of approximately and encompasses two large harbours and many smaller bays and coves. The South Island's largest city, Christchurch, is immediately north of the peninsula. Geology Banks Peninsula forms the most prominent volcanic feature of the South Island, similar to — but more than twice as large as — the older Dunedin volcano (Otago Peninsula and Harbour) to the southwest. Geologically, the peninsula comprises the eroded remnants of two large (Lyttelton formed first, then Akaroa), and the smaller Mt Herbert Volcanic Group. These formed due to intraplate volcanism between approximately eleven and eight million years ago (Miocene) on a continental crust. The peninsula formed as offshore islands, with the volcanoes reaching to about 1,500 m above sea level. Two dominant craters formed Lyttelton and Akaroa Harbours. The Canterbury ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Ellesmere / Te Waihora
Lake Ellesmere / Te Waihora is a broad, shallow coastal lake or waituna, in the Canterbury region of the South Island of New Zealand. It is directly to the west of Banks Peninsula, separated from the Pacific Ocean by the long, narrow, sandy Kaitorete Spit, or more correctly Kaitorete Barrier. It lies partially in extreme southeastern Selwyn District and partially in the southwestern extension of the former Banks Peninsula District, which now (since 2006) is a ward in the city of Christchurch. The lake holds high historical and cultural significance to the indigenous Māori population and the traditional Māori name ''Te Waihora'', means ''spreading waters''. It has officially had a dual English/Māori name since at least 1938. Geography and hydrology Currently Lake Ellesmere / Te Waihora is a brackish bar-type waterbody, commonly called a lake or lagoon. It covers an area of , and is New Zealand's 5th largest lake (by area). Waituna and river mouth lagoons, or hapua, for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Avon Heathcote Estuary
The Estuary of the Heathcote and Avon Rivers / Ihutai is the largest semi-enclosed shallow estuary in Canterbury and remains one of New Zealand’s most important coastal wetlands. It is well known as an internationally important habitat for migratory birds, and it is an important recreational playground and educational resource. It was once highly valued for ''mahinga kai'' (Māori for food gathering). Location The Avon River / Ōtākaro enters the estuary from the northwest, and the Ōpāwaho / Heathcote River from the south-west. The estuary has a triangular shape, a short inlet connection with Pegasus Bay, and is primarily enclosed by the long Brighton Spit, on which the suburbs New Brighton, South New Brighton and Southshore are located. The most prominent features of the inlet are the single deep channel between Rapanui Rock ("Shag Rock") and Brighton Spit. Description It is shallow with the mean at high water of ordinary spring tides (HWOST) of —and is predomin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Midland Line, New Zealand
The Midland line is a 212 km section of railway between Rolleston and Greymouth in the South Island of New Zealand. The line features five major bridges, five viaducts and 17 tunnels, the longest of which is the Otira tunnel. It is the route of the popular TranzAlpine passenger train. History Railway development in the South Island in the 1870s was concentrated on a main line linking the established centres of Christchurch, Timaru, Dunedin and Invercargill and light, easily constructed branch lines serving the arable plains; (see Vogel Era). These later included a branch to Springfield which was reached by January 1880. In 1882 the East and West Coast Railway League was formed and in 1884 a Royal Commission, although fully aware of the construction difficulties of the Waimakariri Valley-Arthurs Pass route, as compared with the somewhat easier but longer Hurunui Valley-Harpers Pass route, chose the more direct route. The construction of the line was rejected in 1883 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
William Courtenay, 11th Earl Of Devon
William Reginald Courtenay, 11th Earl of Devon PC (14 April 1807 – 18 November 1888), styled Lord Courtenay between 1835 and 1859, was a British politician who served as Chancellor of the Duchy of Lancaster from 1866 to 1867 and as President of the Poor Law Board from 1867 to 1868. Background and education Devon was the eldest son of William Courtenay, 10th Earl of Devon and his first wife Harriet Leslie Pepys, daughter of Sir Lucas Pepys, 1st Baronet. He was educated at Westminster School and at Christ Church, Oxford, and was called to the Bar, Lincoln's Inn, in 1832. Political career In 1841 Devon was elected to Parliament for South Devon as a Tory. However, when the Tories split over the Corn Laws in 1846, he joined the Peelites. In 1849 Devon was appointed poor-law inspector and retired from the House of Commons. He then served as secretary to the Poor Law Board from 1850 to 1859. The latter year he succeeded his father and took his seat in the House of Lords. He ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Joseph Thomas (surveyor)
Captain Joseph Thomas (1803–?) was a British explorer and the chief surveyor for Lyttelton, Sumner and Christchurch in New Zealand. He took up surveying after service in the British army, gaining the rank of lieutenant. In the 1840s, he explored many parts of New Zealand and worked for the New Zealand Company. This gained him employment with the Canterbury Association, which sent him to New Zealand in 1848. Thomas' role was to find a suitable site for their proposed settlement, and what became the Canterbury region with Christchurch as its capital was the result of his efforts. He was dismissed in early 1851 over quarrels with John Robert Godley, the agent of the Canterbury Association, just after the first settlers had arrived in the colony. Thomas' life after 1853 is unknown. Having allowed for Hagley Park as a generous central city green space is regarded as his major achievement, and it is his lasting legacy. Early life Thomas was born in Worcester, England, in 1803. At ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canterbury Association
The Canterbury Association was formed in 1848 in England by members of parliament, peers, and Anglican church leaders, to establish a colony in New Zealand. The settlement was to be called Canterbury, with its capital to be known as Christchurch. Organised emigration started in 1850 and the colony was established in the South Island, with the First Four Ships bringing out settlers steeped in the region's history. The Association was not a financial success for the founding members and the organisation was wound up in 1855. Formation of the Association The Association, founded in London on 27 March 1848, was incorporated by Royal Charter on 13 November 1849. The prime movers were Edward Gibbon Wakefield and John Robert Godley. Wakefield was heavily involved in the New Zealand Company, which by that time had already established four other colonies in New Zealand (Wellington, Nelson, Petre and Otago). Wakefield approached Godley to help him establish a colony sponsored by the Chu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
