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Maungarei
Maungarei (officially known as Maungarei / Mount Wellington) is a 135-metre volcanic peak and Tūpuna Maunga (ancestral mountain) located in the Auckland volcanic field of Auckland, New Zealand. It is the youngest onshore volcano of the Auckland volcanic field, having been formed by an eruption around 10,000 years ago. It is the largest of Auckland's scoria cones and has a near-circular base with a flattish rim and three small craters. It is situated in the Mount Wellington suburb of East Auckland. Geology A number of lava flows were created by the mountain's eruption, including one which was six kilometres in length, stretching to the Manukau Harbour at Southdown. Another lava flow blocked the course of a river valley, forming Lake Waiatarua. History The name is short for Te Maungarei ā Pōtaka, the ancient Ngāi Tai ki Tāmaki / Te Waiōhua chief whose domain included the mountain and surrounding areas. Maungarei is also translated as "the watchful mountain" or "t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tūpuna Maunga O Tāmaki Makaurau
The Tūpuna Maunga o Tāmaki Makaurau (ancestral mountains of Auckland) are 14 volcanic cones that hold great historical, spiritual, ancestral and cultural significance to the 13 Māori people, Māori iwi and hapū of Ngā Mana Whenua o Tāmaki Makaurau (also known as the Tāmaki Collective), who have owned them since 2014. Ownership and management In 2014, the 'Ngā Mana Whenua o Tāmaki Makaurau Collective Redress Deed' passed into law. Through the Treaty of Waitangi claims and settlements, Treaty of Waitangi settlement between the Monarchy of New Zealand, Crown and the Tāmaki Collective, ownership of the 14 Tūpuna Maunga, was vested to the collective. The legislation specified that the land be held in trust "for the common benefit of Ngā Mana Whenua o Tāmaki Makaurau and the other people of Auckland". The Tūpuna Taonga Trust is the legal entity set up to receive the cultural redress over the maunga on behalf of the collective, with a primary focus of "enduring protecti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Wellington, New Zealand
Mount Wellington is a suburb in East Auckland, New Zealand, located 10 kilometres southeast of the city centre. It is surrounded by the suburbs of Stonefields, Tamaki, Panmure, Penrose, and Ellerslie, and by the Tamaki River. The suburb is named after the volcanic peak of Maungarei / Mount Wellington. Sylvia Park is a large business park and shopping centre located in the suburb. Geography and early history Maungarei / Mount Wellington is a 135-metre volcanic peak of the Auckland volcanic field. It is the youngest onshore volcano of the Auckland volcanic field, having been formed by an eruption around 10,000 years ago. It is the largest of Auckland's scoria cones. Prior to European settlement, the area around Maungarei was bracken scrub and not densely forested. The southern section, closer to Mount Richmond, was primarily broadleaf and podocarp forest with patches of clear scrubland. The isthmus south of the mountain was traditionally settled by Ngāi Tāhuhu, desc ... [...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 Waiōhua
Te Waiohua or Te Wai-o-Hua is a Māori iwi (tribe) confederation that thrived in the early 18th century. The iwi's rohe (tribal area) was primarily the central Tāmaki Makaurau area (the Auckland isthmus) and the Māngere peninsula, until the 1740s when the paramount chief Kiwi Tāmaki was defeated by the Ngāti Whātua hapū Te Taoū. The descendants of the Waiohua confederation today include Ngāti Te Ata Waiohua, Te Ākitai Waiohua, Ngā Oho of Ngāti Whātua Ōrākei and Waikato Tainui. History Waiohua was a confederation of tribes of the Tāmaki Makaurau region, who were united as a single unit by Huakaiwaka (from which the name of the tribe, ''The Waters of Hua'', can be traced). Huakaiwaka lived and died at Maungawhau / Mount Eden. The three main groups who Huakaiwaka merged were known as Ngā Oho, based in Papakura, Ngā Riki, based in South Auckland with a rohe spanning from Papakura to Ōtāhuhu, and Ngā Iwi, who settled from Ōtāhuhu to the North Shore. The confe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stonefields
Stonefields is a suburb in Auckland, New Zealand, located 8 kilometres southeast of the city centre. Stonefields is surrounded by the suburbs of Mount Wellington, Saint Johns and Glen Innes. History The 100 hectares site of single basalt lava flow from the nearby scoria cone of Maungarei/ Mt Wellington was purchased by Percy Winstone in the mid 1930's. Quarrying began in 1936 and by 1969, the quarry reached a production total of 1 million tonnes per year. When the quarry was worked out by the year 2000, in excess of 35 million tonnes had been produced and used to build the city of Auckland. Once the quarry ceased operations, there was much debate on its future use. A landfill rubbish site was considered and the plan was discarded due to the risk of leachate into ground water. Instead, Stonefields, a housing development was agreed. The former rock quarry was to be one of the largest blocks of undeveloped land in Auckland, able to take a $1.5 billion housing subdivision for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Waiatarua
The Waiatarua Reserve is a nature reserve on the eastern Auckland isthmus in New Zealand, close to the suburbs of Remuera, Meadowbank and St Johns. Originally the site of a freshwater lake, Waiatarua was drained in 1929. Since 1987, the reserve has been redeveloped as an urban wetland. Geology Lake Waiatarua formed after the eruption of Maungarei / Mount Wellington, when a lava flow blocked the flow of a river valley which flowed into the Tāmaki River, approximately 9,000 years ago. History The traditional Tāmaki Māori name for the lake, Waiatarua, means the "Waters of Reflection". The lake was an important freshwater resource for Ngāti Whātua Ōrākei, prior to European settlement. During the early colonial period of New Zealand, it was named Lake St John. The land adjoining the lake was acquired by Bishop Selwyn in 1851, as a part of the grounds of the St John's College. In the 1870s, it was considered as a source for drinking water for the city of Auckland, h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monarchy Of New Zealand
The monarchy of New Zealand is the constitutional system of government in which a hereditary monarch is the sovereign and head of state of New Zealand. The current monarch, King Charles III, ascended the throne following the death of his mother, Queen Elizabeth II, on 8 September 2022. The King's eldest son, William, Prince of Wales, is the heir apparent. The Treaty of Waitangi between Queen Victoria and Māori chiefs () was signed in 1840, and as a result, the British sovereign became New Zealand's head of state. New Zealand gradually became independent from Britain and the monarchy evolved to become a distinctly New Zealand institution, represented by unique symbols. The New Zealand monarch is currently shared with 14 other countries (realms) within the Commonwealth of Nations, all independent and the monarchy of each being legally distinct. As a result, the current monarch is officially titled ''King of New Zealand'' ( mi, Kīngi o Aotearoa) and, in this capacity, h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Treaty Of Waitangi
The Treaty of Waitangi ( mi, Te Tiriti o Waitangi) is a document of central importance to the history, to the political constitution of the state, and to the national mythos of New Zealand. It has played a major role in the treatment of the Māori population in New Zealand, by successive governments and the wider population, a role that has been especially prominent from the late 20th century. The treaty document is an agreement, not a treaty as recognised in international law and it has no independent legal status, being legally effective only to the extent it is recognised in various statutes. It was first signed on 6 February 1840 by Captain William Hobson as consul for the British Crown and by Māori chiefs () from the North Island of New Zealand. The treaty was written at a time when the New Zealand Company, acting on behalf of large numbers of settlers and would-be settlers, were establishing a colony in New Zealand, and when some Māori leaders had petitioned the Briti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''labes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kohimarama
Kohimarama is a coastal residential Auckland suburb, located to the east of the city. Kohimarama is situated between Mission Bay and St Heliers and has an accessible beach with a boardwalk and green recreational spaces located amongst residential areas. Local government of Kohimarama is the responsibility of the Ōrākei Local Board, which also includes the suburbs of Ōrākei, Mission Bay, St Heliers, Glendowie, St Johns, Meadowbank, Remuera and Ellerslie.Retrieved 2013-03-10. Demographics Kohimarama covers and had an estimated population of as of with a population density of people per km2. Kohimarama had a population of 4,350 at the 2018 New Zealand census, an increase of 207 people (5.0%) since the 2013 census, and an increase of 315 people (7.8%) since the 2006 census. There were 1,707 households, comprising 2,064 males and 2,283 females, giving a sex ratio of 0.9 males per female. The median age was 44.7 years (compared with 37.4 years nationally), with 753 peo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saint Heliers
Saint Heliers is an affluent seaside suburb of Auckland with a population of as of This suburb is popular amongst visitors for the beaches, cafés, and views of Rangitoto Island, the distinctive volcanic island in the Hauraki Gulf. St. Heliers is located at the eastern end of Tamaki Drive, and used to be the place where the Tamaki River, Tamaki estuary formally divided Auckland from Manukau City, until the entire Auckland region was amalgamated under a single city authority, the Auckland Council, in 2010. Local government of St. Heliers is the responsibility of the Ōrākei Local Board, which also covers the suburbs of Ōrākei, Kohimarama, Mission Bay, New Zealand, Mission Bay, Glendowie, New Zealand, Glendowie, Saint Johns, New Zealand, St Johns, Meadowbank, New Zealand, Meadowbank, Remuera and Ellerslie, New Zealand, Ellerslie. Demographics Saint Heliers covers and had an estimated population of around 12,000 as of August 2022 with a population density of people per km2. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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