|
Ngātoro-i-rangi
In Māori tradition, Ngātoro-i-rangi (Ngātoro) is the name of a tohunga (priest) prominent during the settling of New Zealand ( Aotearoa) by the Māori people, who came from the traditional homeland Hawaiki on the '' Arawa'' canoe. He is the ancestor of Ngāti Tūwharetoa and his travels around Lake Taupō and up onto the Volcanic Plateau are the basis of Ngāti Tūwharetoa's claim to those regions. Rangiātea Ngātoro-i-rangi was the son of Rakauri and Hineruarangi and was raised at Te Vaitoa in Rangiātea. He was descended from the Ngāti Ohomairangi tribe and was direct successor to the high priest of Taputapuatea marae at Rangiātea. He also had ancestral connections to Aitutaki, Rarotonga, Rangiātea (Ra'iatea) and other islands in the area. Puha-o-rangi, the father of Ohomairangi, was the progenitor of all of the Te Arawa people. He was trained at Taputapuātea marae as a priest and navigator and was renowned for his skills and status. He made a number of journeys around ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāti Tūwharetoa
Ngāti Tūwharetoa is an iwi descended from Ngātoro-i-rangi, the priest who navigated the Arawa canoe to New Zealand. The Tūwharetoa region extends from Te Awa o te Atua (Tarawera River) at Matatā across the central plateau of the North Island to the lands around Mount Tongariro and Lake Taupō. Tūwharetoa is the sixth largest iwi in New Zealand, with a population of 35,877 of the 2013 New Zealand census, and 40% of its people under the age of 15. The tribe consists of a number of ''hapu'' (subtribes) represented by 33 ''marae'' (meeting places). The collective is bound together by the legacy of Ngātoro-i-rangi as epitomised in the ariki (paramount chief), currently Sir Tumu te Heuheu Tūkino VIII. In the 2013 New Zealand census 35,877 people identified as Ngāti Tūwharetoa. By the 2018 New Zealand census, there were at least 47,103 people identifying with the iwi, including 44,448 identifying with the Taupō branch, and 2,655 identifying with the Kawerau branch. Histor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arawa (canoe)
''Arawa'' was one of the great ocean-going, voyaging canoes in Māori traditions that was used in the migrations that settled New Zealand. The Te Arawa confederation of Māori iwi and hapū based in the Rotorua and Bay of Plenty areas trace their ancestry from the people of this canoe. Background Te Arawa's ancestors on board the ''Arawa'' were of the Ngāti Ohomairangi of Ra'iātea Island. Following a battle that broke out between them and Uenuku, in which their own Whakatūria fell in battle, Tama-te-kapua promised to captain the voyage to the islands of New Zealand, which had been discovered by Ngāhue of the '' Tāwhirirangi'' canoe. Construction of the canoe A large tree was cut down by four men called Rata, Wahieroa, Ngāhue and Parata, to make the waka which came to be known as ''Arawa''. "Hauhau-te-rangi" and "Tuutauru" (made from New Zealand greenstone brought back by Ngāhue) were the adzes used for the time-consuming and intensive work. Upon completion, the w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tainui (canoe)
In Māori tradition, ''Tainui'' was one of the great ocean-going canoes in which Polynesians migrated to New Zealand approximately 800 years ago. In Māori tradition, the ''Tainui'' waka was commanded by the chief Hoturoa, who had decided to leave Hawaiki because over-population had led to famine and warfare. The crew of the ''Tainui'' were the ancestors of the iwi that form the Tainui confederation. Crafting The Tainui waka (canoe) was made from a great tree, at a place in Hawaiki known then as Maungaroa, on the spot where a stillborn child had been buried. According to Te Tāhuna Herangi the waka was named after the child who had been called Tainui. The canoe was made by Rakatāura, an expert boat builder in the tradition of Rātā, or according to Wirihana Aoterangi by Rātā himself. It was built with three adzes (''toki''): ''Hahau-te-pō'' ('Chop the night-world') to chop down the tree, ''Paopao-te-rangi'' ('Shatter the heavens') to split the wood, and ''Manu-tawhi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāuruhoe
Mount Ngāuruhoe (also spelled Ngauruhoe; Māori: ''Ngāuruhoe'') is a volcanic cone in New Zealand. It is the youngest vent in the Tongariro stratovolcano complex on the Central Plateau of the North Island and first erupted about 2,500 years ago. Although often regarded as a separate mountain, geologically, it is a secondary cone of Mount Tongariro. The volcano lies between the active volcanoes of Mount Tongariro to the north and Mount Ruapehu to the south, to the west of the Rangipo Desert and 25 kilometres to the south of the southern shore of Lake Taupō. Etymology The local Māori traditions state that the volcano was named by Ngātoro-i-rangi, an ancestor of the local Māori iwi, Ngāti Tūwharetoa. Ngātoro-i-rangi called volcanic fire from his homeland Hawaiki, which eventually emerged at Ngāuruhoe. The name given by Ngātoro-i-rangi (Ngāuruhoe) either commemorates his slave, who had died from the cold before the fire arrived, or refers to the insertions ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Whakaari
Whakaari / White Island (, mi, Te Puia Whakaari, lit. "the dramatic volcano"), also known as White Island or Whakaari, is an active andesite stratovolcano situated from the east coast of the North Island of New Zealand, in the Bay of Plenty. The island covers an area of approximately , which is just the peak of a much larger submarine volcano. The island is New Zealand's most active cone volcano, and has been built up by continuous volcanic activity over the past 150,000 years. The nearest mainland towns are Whakatane and Tauranga. The island has been in a nearly continuous stage of releasing volcanic gas at least since it was sighted by James Cook in 1769. Whakaari erupted continually from December 1975 until September 2000, and also erupted in 2012, 2016, and 2019. Sulphur was mined on the island until the 1930s. Ten miners were killed in 1914 when part of the crater wall collapsed. The main activities on the island now include guided tours and scientific research. Acces ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tama-te-kapua
In Māori mythology, Māori tradition of New Zealand, Tama-te-kapua, also spelt Tamatekapua and Tama-te-Kapua and also known as Tama, was the captain of the ''Arawa (canoe), Arawa'' canoe which came to New Zealand from Polynesia in about 1350. The reason for his leaving his homeland was that he and his brother Whakaturia had stolen breadfruit (''kuru'' or ''poroporo'') from a tree belonging to a chief named Uenuku. They had stolen the fruit in revenge for the theft and consumption of a dog belonging to Haumai-tāwhiti by Toi-te-huatahi and Uenuku. The two brothers fled after tribal war broke out because of the incident. Tama Te Kapua also took two women who were the wives of other men with him, one of whom was Whakaotirangi. The other was the wife of Ruao. Tama-te-kapua asked Ruao to fetch an axe left by his house, and while he was ashore, Tama-te-kapua raised the anchor and left Ruao behind. Some legends describe Tama-te-kapua asking Ngātoro-i-rangi, tohunga and navigator of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Taupō
Lake Taupō (also spelled Taupo; mi, Taupō-nui-a-Tia or ) is a large crater lake in New Zealand's North Island, located in the caldera of the Taupō Volcano. The lake is the namesake of the town of Taupō, which sits on a bay in the lake's northeastern shore. With a surface area of , it is the largest lake by surface area in New Zealand, and the second largest freshwater lake by surface area in geopolitical Oceania after Lake Murray in Papua New Guinea. Motutaiko Island lies in the southeastern area of the lake. Lake Taupō has a perimeter of approximately and a maximum depth of . It is drained by the Waikato River (New Zealand's longest river), and its main tributaries are the Waitahanui River, the Tongariro River, and the Tauranga Taupō River. It is a noted trout fishery with stocks of introduced brown and rainbow trout. The level of the lake is controlled by Mercury Energy, the owner of the eight hydroelectric dams on the Waikato River downstream of Lake Taupō, usin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pacific Ocean
The Pacific Ocean is the largest and deepest of Earth's five oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean (or, depending on definition, to Antarctica) in the south, and is bounded by the continents of Asia and Oceania in the west and the Americas in the east. At in area (as defined with a southern Antarctic border), this largest division of the World Ocean—and, in turn, the hydrosphere—covers about 46% of Earth's water surface and about 32% of its total surface area, larger than Earth's entire land area combined .Pacific Ocean . '' Britannica Concise.'' 2008: Encyclopædia Britannica, Inc. The centers of both the |
Taupō Volcanic Zone
The Taupō Volcanic Zone (TVZ) is a volcanic area in the North Island of New Zealand that has been active for the past two million years and is still highly active. Mount Ruapehu marks its south-western end and the zone runs north-eastward through the Taupō and Rotorua areas and offshore into the Bay of Plenty. It is part of the larger Central Volcanic Region that extends further westward through the western Bay of Plenty to the eastern side of the Coromandel Peninsula and has been active for four million years. At Taupō the rift volcanic zone is widening east–west at the rate of about 8 mm per year while at Mount Ruapehu it is only 2–4 mm per year but this increases at the north eastern end at the Bay of Plenty coast to 10–15 mm per year. It is named after Lake Taupō, the flooded caldera of the largest volcano in the zone, the Taupō Volcano and contains a large central volcanic plateau as well as other landforms associated with its containing tectonic i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tongariro
Mount Tongariro (; ) is a compound volcano in the Taupō Volcanic Zone of the North Island of New Zealand. It is located to the southwest of Lake Taupō, and is the northernmost of the three active volcanoes that dominate the landscape of the central North Island. Geology Mount Tongariro is part of the Tongariro volcanic centre, which consists of four massifs made of andesite: Tongariro, Kakaramea-Tihia Massif, Pihanga, and Ruapehu at the southern end of the North Island Volcanic Plateau. The andesitic eruptions formed Tongariro, a steep stratovolcano, reaching a height of . Tongariro is composed of layers of both lava and tephra and the eruptions that built the current stratovolcano commenced about 275,000 years ago. Tongariro consists of at least 12 cones. Ngāuruhoe, while often regarded as a separate mountain, is geologically a cone of Tongariro. It is also the most active vent, having erupted more than 70 times since 1839, the last episode in 1973 to 1975. Activity ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Ngāuruhoe")
.jpg "Click for more on -> Pacific Ocean")
