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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] |
Banks Penin & Christchurch NZ
A bank is a financial institution that accepts Deposit account, deposits from the public and creates a demand deposit while simultaneously making loans. Lending activities can be directly performed by the bank or indirectly through capital markets. Because banks play an important role in financial stability and the economy of a country, most jurisdictions exercise a Bank regulation, high degree of regulation over banks. Most countries have institutionalized a system known as fractional reserve banking, under which banks hold liquid assets equal to only a portion of their current liabilities. In addition to other regulations intended to ensure accounting liquidity, liquidity, banks are generally subject to minimum capital requirements based on an international set of capital standards, the Basel Accords. Banking in its modern sense evolved in the fourteenth century in the prosperous cities of Renaissance Italy but in many ways functioned as a continuation of ideas and concept ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pacific Plate
The Pacific Plate is an oceanic tectonic plate that lies beneath the Pacific Ocean. At , it is the largest tectonic plate. The plate first came into existence 190 million years ago, at the triple junction between the Farallon, Phoenix, and Izanagi Plates. The Pacific Plate subsequently grew to where it underlies most of the Pacific Ocean basin. This reduced the Farallon Plate to a few remnants along the west coast of North America and the Phoenix Plate to a small remnant near the Drake Passage, and destroyed the Izanagi Plate by subduction under Asia. The Pacific Plate contains an interior hot spot forming the Hawaiian Islands. Boundaries The north-eastern side is a divergent boundary with the Explorer Plate, the Juan de Fuca Plate and the Gorda Plate forming respectively the Explorer Ridge, the Juan de Fuca Ridge and the Gorda Ridge. In the middle of the eastern side is a transform boundary with the North American Plate along the San Andreas Fault, and a boundary with the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Joseph Banks
Sir Joseph Banks, 1st Baronet, (19 June 1820) was an English naturalist, botanist, and patron of the natural sciences. Banks made his name on the 1766 natural-history expedition to Newfoundland and Labrador. He took part in Captain James Cook's first great voyage (1768–1771), visiting Brazil, Tahiti, and after 6 months in New Zealand, Australia, returning to immediate fame. He held the position of president of the Royal Society for over 41 years. He advised King George III on the Royal Botanic Gardens, Kew, and by sending botanists around the world to collect plants, he made Kew the world's leading botanical garden. He is credited for bringing 30,000 plant specimens home with him; amongst them, he was the first European to document 1,400. Banks advocated British settlement in New South Wales and the colonisation of Australia, as well as the establishment of Botany Bay as a place for the reception of convicts, and advised the British government on all Australian matte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
James Cook
James Cook (7 November 1728 Old Style date: 27 October – 14 February 1779) was a British explorer, navigator, cartographer, and captain in the British Royal Navy, famous for his three voyages between 1768 and 1779 in the Pacific Ocean and to New Zealand and Australia in particular. He made detailed maps of Newfoundland prior to making three voyages to the Pacific, during which he achieved the first recorded European contact with the eastern coastline of Australia and the Hawaiian Islands, and the first recorded circumnavigation of New Zealand. Cook joined the British merchant navy as a teenager and joined the Royal Navy in 1755. He saw action in the Seven Years' War and subsequently surveyed and mapped much of the entrance to the St. Lawrence River during the siege of Quebec, which brought him to the attention of the Admiralty and the Royal Society. This acclaim came at a crucial moment for the direction of British overseas exploration, and it led to his commission in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hapū
In Māori and New Zealand English, a ' ("subtribe", or "clan") functions as "the basic political unit within Māori society". A Māori person can belong to or have links to many hapū. Historically, each hapū had its own chief and normally operated independently of its iwi (tribe). Etymology The word literally means "pregnant", and its usage in a socio-political context is a metaphor for the genealogical connection that unites hapū members. Similarly, the Māori word for land, whenua, can also mean "placenta", metaphorically indicating the connection between people and land, and the Māori word for tribe, iwi, can also mean "bones", indicating a link to ancestors. Definition As named divisions of (tribes), hapū membership is determined by genealogical descent; a hapū consists of a number of (extended family) groups. The Māori scholar Hirini Moko Mead states the double meanings of the word hapū emphasise the importance of being born into a hapū group. As a metaphor t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāi Tahu
Ngāi Tahu, or Kāi Tahu, is the principal Māori (tribe) of the South Island. Its (tribal area) is the largest in New Zealand, and extends from the White Bluffs / Te Parinui o Whiti (southeast of Blenheim), Mount Mahanga and Kahurangi Point in the north to Stewart Island / Rakiura in the south. The comprises 18 (governance areas) corresponding to traditional settlements. Ngāi Tahu originated in the Gisborne District of the North Island, along with Ngāti Porou and Ngāti Kahungunu, who all intermarried amongst the local Ngāti Ira. Over time, all but Ngāti Porou would migrate away from the district. Several were already occupying the South Island prior to Ngāi Tahu's arrival, with Kāti Māmoe only having arrived about a century earlier from the Hastings District, and already having conquered Waitaha, who themselves were a collection of ancient groups. Other that Ngāi Tahu encountered while migrating through the South Island were Ngāi Tara, Rangitāne, Ngāti T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kāti Māmoe
Kāti Māmoe (also spelled Ngāti Māmoe but not by the tribe themselves) is a historic Māori iwi. Originally from the Hastings area, they moved in the 16th century to the South Island which at the time was already occupied by the Waitaha. A century later, the Ngāti Māmoe were largely subsequently absorbed via marriage and conquest by the Ngāi Tahu, who migrated south in turn. There is no distinct Ngāti Māmoe organisation today but many Ngāi Tahu have Ngāti Māmoe links in their whakapapa. In the far south of the island especially, "... southern Māori still think of themselves as Ngai Tahu-Ngati Mamoe, a synthesis of the two tribal groups ...." According to Edward Shortland, Kāti Māmoe's historical hapū included Kāti Rakai and Kāti Hinekato. History Early history Kāti Māmoe's descent is traced from the ancestor Hotumāmoe, said to be a descendant of Toi, a great-great-great grandson of Rākaihautū. Hotumāmoe is said to have lived in the Heretaunga District. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rākaihautū
Rākaihautū was the captain of the canoe () and a Polynesian ancestor of various , most famously of Waitaha and other southern groups, though he is also known in the traditions of Taitokerau, and in those of Rarotonga. In Māori traditions, once Rākaihautū landed the at the top of the South Island, he moved southward and dug up many of the island's major lakes using a magical (digging stick), filling them with food for his many descendants. Origin Rākaihautū originally sailed with his wife Waiariki-o-āio, their son Te Rakihouia, and their people from Te-patunui-o-āio aboard the canoe over 34 generations ago. The crew included some of Rākaihautū's kin who were of the tribes Te Kāhui Tipua, Te Kāhui Roko, and Te Kāhui Waitaha. Rākaihautū's daughter Te Uhi-tataraiakoa stayed behind in Te-patunui-o-āio. On the journey to the South Island the heavens and the ocean blocked the canoe's path, until Rākaihautū chanted a and cut a passage with his adze ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waitaha (South Island Iwi)
Waitaha, an early Māori iwi, inhabited the South Island of New Zealand. They were largely absorbed via marriage and conquest - first by the Ngāti Māmoe and then by Ngāi Tahu - from the 16th century onward. Today those of Waitaha descent are represented by the Ngāi Tahu iwi. Like Ngāi Tahu today, Waitaha was itself a collection of various ancient iwi. Kāti Rākai was said to be one of Waitaha's hapū. History Origins Waitaha's earliest ancestors are traditionally traced as arrivals from Te Patunui-o-āio in Eastern Polynesia aboard the canoe (waka), of which Rākaihautū had been the captain. He was accompanied by his wife and son, Waiariki-o-āio and Te Rakihouia, the renowned (astronomer) Matiti, Waitaa, and other kin of the Te Kāhui Tipua, Te Kāhui Roko, and Te Kāhui Waitaha iwi. When genealogies are interpreted with 25–30 years' worth of lifespan for at least 34 generations, these people are calculated to have lived in or around the 9th century at the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori People
The Māori (, ) are the indigenous Polynesian people of mainland New Zealand (). Māori originated with settlers from East Polynesia, who arrived in New Zealand in several waves of canoe voyages between roughly 1320 and 1350. Over several centuries in isolation, these settlers developed their own distinctive culture, whose language, mythology, crafts, and performing arts evolved independently from those of other eastern Polynesian cultures. Some early Māori moved to the Chatham Islands, where their descendants became New Zealand's other indigenous Polynesian ethnic group, the Moriori. Initial contact between Māori and Europeans, starting in the 18th century, ranged from beneficial trade to lethal violence; Māori actively adopted many technologies from the newcomers. With the signing of the Treaty of Waitangi in 1840, the two cultures coexisted for a generation. Rising tensions over disputed land sales led to conflict in the 1860s, and massive land confiscations, to which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Port Hills
The Port Hills are a range of hills in Canterbury Region, so named because they lie between the city of Christchurch and its port at Lyttelton. They are an eroded remnant of the Lyttelton volcano, which erupted millions of years ago. The hills start at Godley Head, run approximately east–west along the northern side of Lyttelton Harbour, and continue running to the south, dividing the city from the harbour. The range terminates near Gebbies Pass above the head of the harbour. The range includes a number of summits between 300 and 500 metres above sea level. The range is of significant geological, environmental and scenic importance. History The volcano is one of two from which Banks Peninsula was originally formed 12 million years ago. The area was first populated by Māori during the 14th century. During early European settlement some 500 years later the Port Hills presented a challenging barrier between the harbour and the planned settlement of Christchurch, their st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Foehn Wind
A Foehn or Föhn (, , ), is a type of dry, relatively warm, downslope wind that occurs in the lee (downwind side) of a mountain range. It is a rain shadow wind that results from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes (see orographic lift). As a consequence of the different adiabatic lapse rates of moist and dry air, the air on the leeward slopes becomes warmer than equivalent elevations on the windward slopes. Foehn winds can raise temperatures by as much as 14 °C (25 °F) in just a matter of hours. Switzerland, southern Germany and Austria have a warmer climate due to the Foehn, as moist winds off the Mediterranean Sea blow over the Alps. Etymology The name ''Foehn'' (german: Föhn, ) arose in the Alpine region. Originating from Latin ''(ventus) favonius'', a mild west wind of which Favonius was the Roman personification and probably transmitted by rm, favuogn or just ''fuogn'', the term was adopted as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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