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Timeline Of Auckland History
This is a timeline of the history of the city of Auckland in New Zealand. 13th century *c. 13th century – Estimated date for first Māori arrivals in the Auckland area. Oral histories tell of the voyager Kupe visiting Paratutae Island. 14th century *c. 14th century **Earliest known archaeological evidence of settlements around the Manukau Harbour, including Ihumātao and Puhinui. **Estimated date for the arrival of the '' Tainui'' and '' Arawa'' migratory waka. The ''Tainui'' was hauled over Te Tō Waka, the portage at Ōtāhuhu between the east and west coasts. Rakataura, tohunga of the ''Tainui'' waka, travelled the area and named many of the features (including Karangahape Road). 15th century *c. 1450 **Eruption of Rangitoto Island.Devora (2020). ''Rangitoto: Odd one out. The story of Auckland's largest volcano''. Devora Fact Sheet 03. Ngāi Tai ki Tāmaki ancestors were living on adjoining Motutapu Island, and footprints in the ash layers between the c. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
History Of Auckland
The human history of the Auckland () metropolitan area stretches from early Māori settlers in the 14th century to the first European explorers in the late 18th century, over a short stretch as the official capital of (European-settled) New Zealand in the middle of the 19th century to its current position as the fastest-growing and commercially dominating metropolis of the country. Māori occupation Pre-European occupation Māori people settled the Auckland isthmus around 1350, calling it ' or ', meaning "Tāmaki desired by many", in reference to the desirability of its natural resources and geography. The narrow isthmus was a strategic location with its two harbours providing access to the sea on both the west and east coasts. It had fertile soils that facilitated horticulture and the two harbours provided plentiful ''kai moana'' (seafood). Māori constructed terraced '' pā'' (fortified villages) on the volcanic peaks. However, for most of the period Māori living in def ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāti Manuhiri
Ngāti Manuhiri is a Māori iwi of the Mahurangi Peninsula area of New Zealand. They have an interest in the region from the Okura River in the south to Mangawhai in the north, and extending out to Great Barrier Island. They are descended from Manuhiri, one of the sons of Maki, founder of the Te Kawerau iwi. They have a marae near Leigh. The iwi is descended from the Moekākara and Tainui waka (arrival canoes). See also *List of Māori iwi This is a list of iwi (New Zealand Māori tribes). List of iwi This list includes groups recognised as iwi (tribes) in certain contexts. Many are also hapū (sub-tribes) of larger iwi. Moriori are included on this list. Although they are distinc ... References External links Ngāti Manuhiri Settlement Trust {{Maori-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Kawerau ā Maki
Te Kawerau ā Maki, Te Kawerau a Maki, or Te Kawerau-a-Maki is a Māori ''iwi'' (tribe) of the Auckland Region of New Zealand. It had 251 registered adult members as of June 2017. Auckland Council gave it land for a marae at Te Henga (Bethells Beach) in 2018; it has no ''wharenui'' (meeting house) yet. History Te Kawerau ā Maki are the descendants of the ''rangatira'' (chief) Maki and his wife Rotu, who migrated with their family and followers from Kawhia to Tāmaki Makaurau (Auckland) in the early 1600s. Te Kawerau trace their ancestry from a number of Māori migration canoes, particularly the Tainui, but also Aotea, Tokomaru, Kahuitara and Kurahaupō. Tainui ancestors including Hoturoa and the tohunga Rakataura (Hape) are particularly important in Te Kawerau whakapapa, as is the ancient turehu ancestor and tohunga Tiriwa. Maki and his people were related to a number of groups who had occupied the Auckland region since the fourteenth century, including the Tainui ''hapū'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaipara River
The Kaipara River drains the area to the northwest of Auckland, New Zealand. It flows north from the northern foothills of the Waitākere Ranges, meandering past the town of Helensville. It is joined by the Kaukapakapa River in its lower tidal reaches shortly before entering the southern Kaipara Harbour. Other major tributaries are the Ararimu, Ahukuramu, Waimauku and Waipatukahu streams. The area around the river was historically occupied by the Te Taoū hapu of Ngāti Whātua in the lower catchment near present-day Helensville, and by Te Kawerau ā Maki Te Kawerau ā Maki, Te Kawerau a Maki, or Te Kawerau-a-Maki is a Māori '' iwi'' (tribe) of the Auckland Region of New Zealand. It had 251 registered adult members as of June 2017. Auckland Council gave it land for a marae at Te Henga (Bethells ... in the upper sections near Kumeū. During European settlement in the latter 19th century, the course of the river was altered to better use the river to float timber for millin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tāmaki Māori
Tāmaki Māori are Māori ''iwi'' and ''hapū'' (tribes and sub-tribes) who have a strong connection to Tāmaki Makaurau (the Auckland Region), and whose rohe was traditionally within the region. Among Ngā Mana Whenua o Tāmaki Makaurau (the Māori tribes of Auckland), also known as the Tāmaki Collective, there are thirteen iwi and hapū, organised into three rōpū (collectives), however Tāmaki Māori can also refer to subtribes and historical iwi not included in this list. Ngāti Whātua Rōpū Ngāti Whātua descend from the '' Māhuhu-ki-te-rangi'' waka, which landed north of the Kaipara Harbour. The rōpū includes Ngāti Whātua o Kaipara, Ngāti Whātua Ōrākei and Te Rūnanga o Ngāti Whātua. Te Rūnanga o Ngāti Whātua is a Māori Trust Board formed in the mid 2000s to represent the interests of Ngāti Whātua iwi and hapū collectively, including those outside of Ngāti Whātua o Kaipara and Ngāti Whātua Ōrākei. The rūnanga represents Ngā Oho, Ngāi Tāh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kawhia Harbour
Kawhia Harbour (Maori: ''Kāwhia'') is one of three large natural inlets in the Tasman Sea coast of the Waikato region of New Zealand's North Island. It is located to the south of Raglan Harbour, Ruapuke and Aotea Harbour, 40 kilometres southwest of Hamilton, New Zealand, Hamilton. Kawhia is part of the Otorohanga, Ōtorohanga District Council and is in the King Country. It has a high-tide area of and a low-tide area of . Te Motu Island is located in the harbour. The settlement of Kawhia is located on the northern coast of the inlet, and was an important port in early colonial New Zealand. The area of Kawhia comprises and is the town block that was owned by the New Zealand Government. The government bought it from the New Zealand European, Europeans in 1880 "not from the original Māori people, Māori owners, but from a European who claimed ownership in payment of money owed by another European". History and culture Early history The Kawhia Harbour is the southernmost l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Auckland Volcanic Field
The Auckland volcanic field is an area of monogenetic volcanoes covered by much of the metropolitan area of Auckland, New Zealand's largest city, located in the North Island. The approximately 53 volcanoes in the field have produced a diverse array of maars (explosion craters), tuff rings, scoria cones, and lava flows. With the exception of Rangitoto, no volcano has erupted more than once, but the other eruptions lasted for various periods ranging from a few weeks to several years. Rangitoto erupted several times and recently twice; in an eruption that occurred about 600 years ago, followed by a second eruption approximately 50 years later. The field is fuelled entirely by basaltic magma, unlike the explosive subduction-driven volcanism in the central North Island, such as at Mount Ruapehu and Lake Taupō.Ian E.M. Smith and Sharon R. Allen. Auckland volcanic field geology'. Volcanic Hazards Working Group, Civil Defence Scientific Advisory Committee. Retrieved 30 March 2013. Also ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Korowai-o-Te-Tonga Peninsula
Te Korowai-o-Te-Tonga Peninsula, also known as South Head and by its former name of the South Kaipara Peninsula, is a long peninsula in the North Island of New Zealand, extending north along the western edge of the Kaipara Harbour for some from near Helensville to the harbour's mouth. The peninsula was officially renamed in 2013 as part of a Treaty of Waitangi settlement. The name, which is Māori for "The cloak of the south", reflects the peninsula's geographical role in guarding the southern half of the Kaipara Harbour from the Tasman Sea and prevailing westerly winds. The mouth of the Kaipara Harbour separates the peninsula from the larger Pouto Peninsula to the north. Geography The Peninsula is mostly low-lying or gently undulating, rising to only some at its highest point. It is bounded in the west by the Tasman Sea, with the long beaches of Te Oneone Rangatira Beach and Muriwai Beach along its Tasman coast. The settlement of Muriwai lies immediately to the south of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Motutapu Island
Motutapu Island (otherwise known as ''Motutapu'') is a island in the Hauraki Gulf to the northeast of the city of Auckland, New Zealand. The island is part of the Hauraki Gulf Maritime Park. Its full name, rarely used, is ''Te Motutapu a Taikehu'', "The sacred island of Taikehu", Taikehu having been a tohunga (tribal priest) of the Tainui iwi. 'Motutapu', meaning "sacred" or "sanctuary" island, is a term used for various islands in a number of Polynesian cultures. The island can be accessed via regular ferry services departing from Auckland City. Geography Approximately 18,000 years ago during the Last Glacial Maximum when sea levels were over 100 metres lower than present day levels, Motutapu Island was landlocked to the North Island, surrounded by a vast coastal plain where the Hauraki Gulf / Tīkapa Moana exists today. Sea levels began to rise 7,000 years ago, after which Motutapu became an island separated from the rest of New Zealand. The island is now linked by an artif ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāi Tai Ki Tāmaki
Ngāi Tai ki Tāmaki is a Māori tribe that is based in the area around Clevedon, part of the Auckland region (''Tāmaki'' in the Māori language). It is one of the twelve members of the Hauraki Collective of tribes. The founding ancestors of Ngāi Tai ki Tāmaki came to New Zealand in the ''Tainui'' migration canoe and left it when it was dragged across Te Tō Waka, the portage from the Tāmaki River to the Manukau Harbour. Their descendants occupied parts of the Hauraki Gulf, including east Auckland as far inland as Otara and Maungarei, as well as Clevedon, Maraetai and Howick. Te Irirangi Drive, a major highway in Manukau City, is named after one of their ''rangatira'' (chiefs), Tara Te Irirangi. Ngāi Tai has a marae at Umupuia Beach, between Maraetai and Clevedon. They also use the Ngāti Tamaoho marae at Karaka. In 2015 the Crown settled with Ngāi Tai ki Tāmaki over historic grievances, including both financial and cultural compensation. See also *List of iwi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rangitoto Island
Rangitoto Island is a volcanic island in the Hauraki Gulf near Auckland, New Zealand. The wide island is a symmetrical shield volcano cone, reaching a height of . Rangitoto is the youngest and largest of the approximately 50 volcanoes of the Auckland volcanic field, with its present form related to an eruption about 600 years ago and covering an area of . It is separated from the mainland of Auckland's North Shore by the Rangitoto Channel. Since World War II, it has been linked by a causeway to the much older, non-volcanic Motutapu Island. is Māori for 'Bloody Sky',What happened to local Maori? (from the Rangitoto page on the website) with the name coming from the full phras ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
