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History Of New Plymouth
The city of New Plymouth, New Zealand, has a history that includes a lengthy occupation and residence by Maori, the arrival of white traders and settlers in the 19th century and warfare that resulted when the demands of the two cultures clashed. European settlement began in the early 1840s at a time when many original Maori inhabitants were absent, either because they had been taken captive by northern Maori warriors or had migrated south to avoid war. The rapid growth of the colonist population, coupled with insatiable demands for land by the New Zealand Company and the dubious practices it employed in purchasing it, created friction with local Maori, leading to a war in the 1860s. New Plymouth became a fortified garrison town and its residents suffered hunger and disease. Farming was impeded and immigration and trade came to a halt. In the aftermath of the war, as improved road and rail links with other towns resulted in a rapid growth of population and economic stability, the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Plymouth
New Plymouth ( mi, Ngāmotu) is the major city of the Taranaki region on the west coast of the North Island of New Zealand. It is named after the English city of Plymouth, Devon from where the first English settlers to New Plymouth migrated. The New Plymouth District, which includes New Plymouth City and several smaller towns, is the 10th largest district (out of 67) in New Zealand, and has a population of – about two-thirds of the total population of the Taranaki Region and % of New Zealand's population. This includes New Plymouth City (), Waitara (), Inglewood (), Ōakura (), Ōkato (561) and Urenui (429). The city itself is a service centre for the region's principal economic activities including intensive pastoral activities (mainly dairy farming) as well as oil, natural gas and petrochemical exploration and production. It is also the region's financial centre as the home of the TSB Bank (formerly the Taranaki Savings Bank), the largest of the remaining non-govern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earl Of Devon
Earl of Devon was created several times in the English peerage, and was possessed first (after the Norman Conquest of 1066) by the de Redvers (''alias'' de Reviers, Revieres, etc.) family, and later by the Courtenay family. It is not to be confused with the title of Earl of Devonshire, held, together with the title Duke of Devonshire, by the Cavendish family of Chatsworth House, Derbyshire, although the letters patent for the creation of the latter peerages used the same Latin words, ''Comes Devon(iae)''. It was a re-invention, if not an actual continuation, of the pre-Conquest office of Ealdorman of Devon. Close kinsmen and powerful allies of the Plantagenet kings, especially Edward III, Richard II, Henry IV and Henry V, the Earls of Devon were treated with suspicion by the Tudors, perhaps unfairly, partly because William Courtenay, 1st Earl of Devon (1475–1511), had married Princess Catherine of York, a younger daughter of King Edward IV, bringing the Earls of Devon very ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whanganui River
The Whanganui River is a major river in the North Island of New Zealand. It is the country's third-longest river, and has special status owing to its importance to the region's Māori people. In March 2017 it became the world's second natural resource (after Te Urewera) to be given its own legal identity, with the rights, duties and liabilities of a legal person. The Whanganui Treaty settlement brought the longest-running litigation in New Zealand history to an end. Geography With a length of , the Whanganui is the country's third-longest river. Much of the land to either side of the river's upper reaches is part of the Whanganui National Park, though the river itself is not part of the park. The river rises on the northern slopes of Mount Tongariro, one of the three active volcanoes of the central plateau, close to Lake Rotoaira. It flows to the north-west before turning south-west at Taumarunui. From here it runs through the rough, bush-clad hill country of the Kin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Egmont
Cape Egmont, splitting Northern and Southern Taranaki Bights, is the westernmost point of Taranaki, on the west coast of New Zealand's North Island. It is located close to the volcanic cone of Mount Taranaki or Mount Egmont. It was named ''Kaap Pieter Boreel'' by Dutch explorer Abel Tasman in 1642, but renamed ''Cape Egmont'' by British explorer James Cook in 1769. (Note: Tasman did not sight Mount Taranaki, due to bad visibility, but Cook did, and after naming the mountain Mount Egmont, bestowed the same name on the promontory, which became the enduring name). Ironically, the cape retained a Dutch name, as Cook named the mountain and cape after the Earl of Egmont, who claimed descent of the Dutch House of Egmond. In July 1862, Kapoaiaia near Cape Egmont was the site of a hui between 600 members of Taranaki, Ngāti Ruanui, Ngā Rauru and Whanganui Māori iwi, discussing the First Taranaki War (1860–1861). There, it was agreed that the lands East and West of New Plymout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Treaty Of Waitangi
The Treaty of Waitangi ( mi, Te Tiriti o Waitangi) is a document of central importance to the History of New Zealand, history, to the political constitution of the state, and to the national mythos of New Zealand. It has played a major role in the treatment of the Māori population in New Zealand, by successive governments and the wider population, a role that has been especially prominent from the late 20th century. The treaty document is an agreement, not a treaty as recognised in international law and it has no independent legal status, being legally effective only to the extent it is recognised in various statutes. It was first signed on 6 February 1840 by Captain William Hobson as Administrative consul, consul for the British The Crown, Crown and by Māori people, Māori chiefs () from the North Island of New Zealand. The treaty was written at a time when the New Zealand Company, acting on behalf of large numbers of settlers and would-be settlers, were establishing a colo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 servi ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hurunui River
The Hurunui River is the fourth largest of the four principal rivers in north Canterbury, New Zealand, with a catchment area of . The river flows from the eastern side of the Southern Alps, to the Pacific Ocean. Geography The head of the Hurunui River is at Harper Pass; on the other side of the pass is the Taramakau River. Some of the tributaries include the Jollie Brook, the Hurunui River South Branch, the Glenrae River and the Mandamus River. The Hurunui River flows through Lake Sumner. A hot pool has been constructed at the base of a small waterfall on a side stream of the river. Recreation The river has rapids rated class II and III on the international scale of river difficulty and is popular for kayaking. The best whitewater is considered to be below the confluence of the north and south branches of the river in Maori Gully and in the Harwarden Gorge. Chinook salmon (''Oncorhynchus tshawytscha'') were introduced from California in the 1900s for game fishing. Water ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aotea Harbour
Aotea Harbour ( mi, Aotea Moana) is a settlement and smallest of three large natural inlets in the Tasman Sea coast of the Waikato region of New Zealand's North Island. It is located between Raglan Harbour to the north and Kawhia Harbour to the south, 30 kilometres southwest of Hamilton. Geography Aotea Harbour is a drowned valley system following the post glacial Aranuian sea level rise of over 100m in the last 14,000 years, but its level may also be influenced by the Makomako and Te Maari faults. It has a high-tide area of and a low-tide area of . Most higher ground around the harbour is formed from Jurassic era graywacke stone, while the Aotea Harbour north head were formed from Quaternary marine deposits, wind blown north-east from the Tasman Sea. 54% of the area around the harbour is in sheep and beef grazing. Since 1850 native forest cover has declined from 98% to 28%, about 18% managed by the Department of Conservation. Waireinga/Bridal Veil Falls is located on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Company Ships
The New Zealand Company was a 19th-century English company that played a key role in the colonisation of New Zealand. The company was formed to carry out the principles of systematic colonisation devised by Edward Gibbon Wakefield, who envisaged the creation of a new-model English society in the southern hemisphere. Under Wakefield's model, the colony would attract capitalists who would then have a ready supply of labour—migrant labourers who could not initially afford to be property owners, but who would have the expectation of one day buying land with their savings. The New Zealand Company established settlements at Wellington, Nelson, Wanganui and Dunedin and also became involved in the settling of New Plymouth and Christchurch. It reached the peak of efficiency about 1841, encountered financial problems from 1843 from which it never recovered, and wound up in 1858. This list details the various ships used by the Company in establishing its settlements in New Zealand at We ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hussey Vivian, 1st Baron Vivian
Lieutenant General Richard Hussey Vivian, 1st Baron Vivian (28 July 177520 August 1842), known as Sir Hussey Vivian from 1815 to 1828 and Sir Hussey Vivian, Bt, from 1828 to 1841, was a British cavalry leader from the Vivian family. Early career Vivian was the son of John Vivian (1750–1826), of Truro, Cornwall, and his wife Betsey, daughter of the Reverend Richard Cranch, and the brother of John Henry Vivian. He was educated at Truro Grammar School, then at Harrow and Exeter College, Oxford, Vivian entered the army in 1793, and less than a year later became a captain in the 28th Foot. Under Lord Moira he served in the campaign of 1794 in Flanders and the Netherlands. At the end of the expedition, the 28th bore a distinguished part in Lord Cathcart's action of Geldermalsen. In 1798 Vivian was transferred to the 7th Light Dragoons (later Hussars), and in Sir Ralph Abercromby's division was present in the Helder campaign in Holland at the battles of Bergen and Alkmaar (19 Se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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