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]   |
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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]   |
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Uruaokapuarangi
(also ; often known simply as ) was one of the great Māori migration canoes, ocean-going, voyaging canoes () that was used in the migrations that settled the South Island according to Māori mythology, Māori tradition. is linked to many southern , first landing near Nelson, New Zealand, Nelson. The was captained by Rākaihautū, who was accompanied by his wife Waiariki-o-āio, their son Te Rakihouia, and a man named Matiti. Origins Originally, was said to belong to a chief from Hawaiki, Te Patunuioāio named Taitewhenua. He decided to give the canoe to the renowned (astronomer) Matiti, who then gave it to Rākaihautū and encouraged him to use it to explore new lands. In the 9th century, Rākaihautū, accompanied by his wife Waiariki-o-āio, their son Te Rakihouia, Matiti, and other kin of the Te Kāhui Tipua, Te Kāhui Roko, and Waitaha (South Island iwi), Te Kāhui Waitaha tribes, set sail across the Pacific Ocean in search of new land. Voyage and arrival On the j ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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]   |
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Lake Wānaka
Lake Wānaka is New Zealand's fourth-largest lake and the seat of the town of Wānaka in the Otago region. The lake is 278 meters above sea level, covers , and is more than deep. "Wānaka" is the South Island dialect pronunciation of , which means "the lore of the tohunga or priest" or a place of learning. Geography Geography Lake Wānaka lies at the heart of the Otago Lakes in the lower South Island of New Zealand. The township of Wānaka, which sits in a glacier-carved basin on the shores of the lake, is the gateway to Mt Aspiring National Park. Lake Hāwea is a 15-minute drive away, en route to the frontier town of Makarora, the last stop before the West Coast Glacier region. To the south is the historic Cardrona Valley, a popular scenic alpine route to neighbouring Queenstown. Geology Lake Wānaka lies in a u-shaped valley formed by glacial erosion during the last ice age more than 10,000 years ago. It is fed by the Mātukituki and Makarora Rivers, and is the sourc ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lake Tekapo
__NOTOC__ Lake Tekapo ( mi, Takapō) is the second-largest of three roughly parallel lakes running north–south along the northern edge of the Mackenzie Basin in the South Island of New Zealand (the others are Lake Pukaki and Lake Ohau). It covers an area of , and is at an altitude of above sea level. The lake is fed at its northern end by both the braided Godley River and Macauley river, which have their sources in the Southern Alps to the north. The snow melt from the Southern Alps is tinged with a light turquoise colour from the glacial silt. This gives Lake Tekapo its distinctive colour. To the east of Lake Tekapo lies the Two Thumb Range with Mount Toby (2222m); Braun Elwert Peak (2086m); Dobson Peak (2095m) and Mount Maude (1797m) amongst the mountains over looking Lake Tekapo. On the western side of Lake Tekapo. Mount John (1031m) is closest to the town with Lake Alexandrina further north and Mistake Peak (1931m) sitting towards the head of the lake. Cowans Hill ( ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Māori Mythology
Māori mythology and Māori traditions are two major categories into which the remote oral history of New Zealand's Māori may be divided. Māori myths concern fantastic tales relating to the origins of what was the observable world for the pre-European Māori, often involving gods and demigods. Māori tradition concerns more folkloric legends often involving historical or semi-historical forebears. Both categories merge in to explain the overall origin of the Māori and their connections to the world which they lived in. Māori had yet to invent a writing system before European contact, beginning in 1769, so they had no method to permanently record their histories, traditions, or mythologies. They relied on oral retellings memorised from generation to generation. The three forms of expression prominent in Māori and Polynesian oral literature are genealogical recital, poetry, and narrative prose. Experts in these subjects were broadly known as . The rituals, beliefs, and ge ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lake Ohau
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ic ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lake Pukaki
Lake Pukaki is the largest of three roughly parallel alpine lakes running north–south along the northern edge of the Mackenzie Basin on New Zealand's South Island. The others are Lakes Tekapo and Ohau. All three lakes were formed when the terminal moraines of receding glaciers blocked their respective valleys, forming moraine-dammed lakes. The Alps2Ocean mountain bike trail follows the edge of Lake Pukaki for part of its length. Geography The glacial feed to the lakes gives them a distinctive blue colour, created by glacial flour, the extremely finely ground rock particles from the glaciers. Lake Pukaki covers an area of 178.7 km², and the surface elevation of the lake normally ranges from 518.2 to 532 metres above sea level. The lake is fed at its northern end by the braided Tasman River, which has its source in the Tasman and Hooker Glaciers, close to Aoraki / Mount Cook. To the west of Lake Pukaki lies the Ben Ohau mountain range with Ben Dhu (1607m) and Betty ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lake Rotoroa (Tasman)
Lake Rotoroa lies within the borders of Nelson Lakes National Park in the South Island, New Zealand. The lake is fed by the D'Urville and Sabine rivers. The greatest depth is 145 metres, and it has an area of just under 23.5 km. The lake is surrounded by beech forest. Rotoroa is a small community at the base of the lake. The Gowan River flows out of the lake at this point, thus making the lake one of the sources of the Buller River system. A track follows the northeast side of the lake and a water taxi travels the length of the lake to ferry trampers to and from the tracks at the head of the lake. The lake has introduced trout, which attract recreational fishermen. There is a fly-fishing lodge, Lake Rotoroa Lodge, on the lake. The word ''rotoroa'' is Māori Māori or Maori can refer to: Relating to the Māori people * Māori people of New Zealand, or members of that group * Māori language, the language of the Māori people of New Zealand * Māori culture * Coo ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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, spe ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Akaroa Harbour
Akaroa Harbour, is part of Banks Peninsula in the Canterbury region of New Zealand. The harbour enters from the southern coast of the peninsula, heading in a predominantly northerly direction. It is one of two major inlets in Banks Peninsula, on the coast of Canterbury, New Zealand; the other is Lyttelton Harbour on the northern coast. The name Akaroa is an alternative spelling of Whakaroa, Whangaroa or Wangaloa from the Kāi Tahu dialect of Māori. Whakaroa means "Long Harbour". The harbour was used commercially in the mid-19th century for ship-based and shore-based whaling. Cruise ships occasionally enter the harbour, with the passengers visiting Akaroa. Ōnawe Peninsula is at the head of the harbour, the former site of a Māori pā. Settlements Akaroa Harbour's waterfront has been continually inhabited since the 1840s. Akaroa, Duvauchelle, Takapūneke, Takamatua, Barrys Bay, French Farm and Wainui lie on the shoreline of the harbour. They are connected to the rest ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |