|
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 a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bay Of Plenty
The Bay of Plenty ( mi, Te Moana-a-Toi) is a region of New Zealand, situated around a bight of the same name in the northern coast of the North Island. The bight stretches 260 km from the Coromandel Peninsula in the west to Cape Runaway in the east. The Bay of Plenty Region, governed by the Bay of Plenty Regional Council, incorporates several large islands in the bay, in addition to the mainland area. Called ''Te Moana-a-Toi'' (the Sea of Toi) in the Māori language after Toi, an early ancestor, the name 'Bay of Plenty' was bestowed by James Cook in 1769 when he noticed the abundant food supplies at several Māori villages there, in stark contrast to observations he had made earlier in Poverty Bay. History According to local Māori traditions, the Bay of Plenty was the landing point of several migration canoes that brought Māori settlers to New Zealand. These include the '' Mātaatua'', '' Nukutere'', '' Tākitimu'', '' Arawa'' and '' Tainui'' canoes. Many of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Astronomer
An astronomer is a scientist in the field of astronomy who focuses their studies on a specific question or field outside the scope of Earth. They observe astronomical objects such as stars, planets, moons, comets and galaxies – in either observational (by analyzing the data) or theoretical astronomy. Examples of topics or fields astronomers study include planetary science, solar astronomy, the origin or evolution of stars, or the formation of galaxies. A related but distinct subject is physical cosmology, which studies the Universe as a whole. Types Astronomers usually fall under either of two main types: observational and theoretical. Observational astronomers make direct observations of celestial objects and analyze the data. In contrast, theoretical astronomers create and investigate models of things that cannot be observed. Because it takes millions to billions of years for a system of stars or a galaxy to complete a life cycle, astronomers must observe sna ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hastings, New Zealand
Hastings (; mi, Heretaunga) is an inland city of New Zealand and is one of the two major urban areas in Hawke's Bay, on the east coast of the North Island. The population of Hastings (including Flaxmere) is (as of with a further people in Havelock North and in Clive. Hastings is about 18 kilometres inland of the coastal city of Napier. These two neighbouring cities are often called "The Bay Cities" or "The Twin Cities". The city is the administrative centre of the Hastings District. Since the merger of the surrounding and satellite settlements, Hastings has grown to become one of the largest urban areas in Hawke's Bay. Hastings District is a food production region. The fertile Heretaunga Plains surrounding the city produce stone fruits, pome fruit, kiwifruit and vegetables, and the area is one of New Zealand's major red wine producers. Associated business include food processing, agricultural services, rural finance and freight. Hastings is the major service centre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Toi (name)
Toi is a fairly common man's name in Māori and other Polynesian languages. The best known men named Toi are the following from Māori legendary history, who are sometimes confused with one another: * Toi-te-huatahi, about whom there are various traditions. In Te Arawa tradition, a chief who never left Hawaiki. In the Ngati Awa tradition, a descendant of the fantail, the original settler of New Zealand. In the discredited 'orthodox' or " Great Fleet" story, a man from Hawaiki who settled at Whakatane after following his grandson Whatonga. *Toi-te-huatahi II, in the discredited Great Fleet story, a man who settled at Whakatāne after following his grandson Whatonga, much later than Toi-te-huatahi I. *Toi-kai-rākau, an ancestor of the Tūhoe tribe. In some traditions, this is an alternative name for Toi-te-huatahi. The descendants of Toi-kai-rākau are named ''Te Tini-a-Toi'' – the many descendants of Toi. In the part of the Bay of Plenty where the ''Mātaatua'' canoe lan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Te Herekiekie Grace
John is a common English name and surname: * John (given name) * John (surname) John may also refer to: New Testament Works * Gospel of John, a title often shortened to John * First Epistle of John, often shortened to 1 John * Second Epistle of John, often shortened to 2 John * Third Epistle of John, often shortened to 3 John People * John the Baptist (died c. AD 30), regarded as a prophet and the forerunner of Jesus Christ * John the Apostle (lived c. AD 30), one of the twelve apostles of Jesus * John the Evangelist, assigned author of the Fourth Gospel, once identified with the Apostle * John of Patmos, also known as John the Divine or John the Revelator, the author of the Book of Revelation, once identified with the Apostle * John the Presbyter, a figure either identified with or distinguished from the Apostle, the Evangelist and John of Patmos Other people with the given name Religious figures * John, father of Andrew the Apostle and Saint Peter * Pope Joh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Āpirana Ngata
Sir Āpirana Turupa Ngata (3 July 1874 – 14 July 1950) was a prominent New Zealand statesman. He has often been described as the foremost Māori politician to have served in Parliament in the mid-20th century, and is also known for his work in promoting and protecting Māori culture and language. Ngata practiced as a lawyer before entering politics in 1897, when he established the Young Māori Party alongside numerous alumni of Te Aute College, including future fellow cabinet minister Māui Pōmare. Here he challenged the traditional views of his people, advocating the abandonment of some traditional practices and customary healing in favour of science and Pākehā-style sanitation, which made him a controversial figure. In 1905, he was elected the Liberal Member of Parliament (MP) for Eastern Maori, retaining this seat for nearly 40 years. He served in government as Minister of Native Affairs from 1928 to 1934. In this he tried to accomplish as many reforms for Māori as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pākehā
Pākehā (or Pakeha; ; ) is a Māori term for New Zealanders primarily of European descent. Pākehā is not a legal concept and has no definition under New Zealand law. The term can apply to fair-skinned persons, or to any non- Māori New Zealander. Papa'a has a similar meaning in Cook Islands Māori. Historically before the arrival of other ethnic groups the word Māori meant 'ordinary' or 'normal'. The arrival of Europeans led to the formation of a new term to distinguish the self-regarded 'ordinary' or 'normal' Māori from the new arrivals. The etymology of the word ''Pākehā'' remains unclear, but the term was in use by the late-18th century. In December 1814 the Māori children at Rangihoua in the Bay of Islands were "no less eager to see the ''packaha'' than the grown folks". In Māori, plural noun-phrases of the term include (the definite article) and (the indefinite article). When the word was first adopted into English, the usual plural was 'Pakehas'. However, s ... [...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 P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waitaki River
The Waitaki River is a large braided river that drains the Mackenzie Basin and runs some south-east to enter the Pacific Ocean between Timaru and Oamaru on the east coast of the South Island of New Zealand. It starts at the confluence of the Ōhau and Tekapo rivers, now at the head of the artificial Lake Benmore, these rivers being fed by three large glacial lakes, Pukaki, Tekapo, and Ōhau at the base of the Southern Alps. The Waitaki flows through Lake Benmore, Lake Aviemore and Lake Waitaki, these lakes being contained by hydroelectric dams, Benmore Dam, Aviemore Dam and Waitaki Dam. The Waitaki has several tributaries, notably the Ahuriri River and the Hakataramea River. It passes Kurow and Glenavy before entering the Pacific Ocean. The River lends its name the Waitaki District on the south side of the river bank. The river's flow is normally low in winter, with flows increasing in spring when the snow cloaking the Southern Alps begins to melt, with flows throughout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clutha River
The Clutha River (, officially gazetted as Clutha River / ) is the second longest river in New Zealand and the longest in the South Island. It flows south-southeast through Central and South Otago from Lake Wānaka in the Southern Alps to the Pacific Ocean, south west of Dunedin. It is the highest volume river in New Zealand, and the swiftest, with a catchment of , discharging a mean flow of . The river is known for its scenery, gold-rush history, and swift turquoise waters. A river conservation group, the Clutha Mata-Au River Parkway Group, is working to establish a regional river parkway, with a trail, along the entire river corridor. Geography The ultimate source of the river is at the head of the Makarora River, close to the saddle of the Haast Pass, which flows into the northern end of Lake Wānaka. The southern end of the lake drains into the nascent Clutha close to Albert Town, where it is met by its first main tributary, the Hāwea River, the outflow of Lake W ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boulder Bank
The Boulder Bank (Māori: ''Te Taero a Keropa'' or ''Te Tāhuna o Tama-i-ea'') is a very unusual naturally formed landform in Nelson, New Zealand. It is a 13 kilometre long stretch of rocky substrate which begins at the Mackay Bluff and ends at the Cut of the Nelson Harbour. Haulashore Island was once a part of the Boulder Bank, but the Cut made it an island, and it is no longer connected to the Boulder Bank. The Boulder Bank separates Tasman Bay and the Nelson Haven and is managed as a scenic reserve by the Department of Conservation. Land access is gained along Boulder Bank Drive, signposted at the northern end of Nelson Haven on . Geology and geography The Boulder Bank is composed of granodiorite. The source of this rock is Mackay Bluff. It is still debated what process or processes have resulted in this odd structure. Longshore drift, however, is the most accepted hypothesis for creation. The main objection for longshore drift is that Tasman Bay does not receive enough wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
