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Mauao
Mount Maunganui, or Mauao, commonly known by locals as The Mount, is a dormant volcanic cone at the end of a peninsula in the town of Mount Maunganui, by the eastern entrance to the Tauranga Harbour in New Zealand. It is considered very important and tapu (sacred) by the local Māori iwi, featuring extensively in local mythology. It is also of significant historical value. The summit is 232 metres above sea level. In recent years there have been several fires on the mountain, in turn triggering a number of replanting efforts. Since Mount Maunganui has been open to the general public it has become a popular location for many activities including scenic walks, jogging and even hang gliding. Maori legend In the ancient times of the Maori people there lived a nameless hill. He sat alone in a discarded inland area and was slave to Otanewainuku, the most prestigious mountain of Tauranga Moana. Nearby there lived a captivating hill whose name was Puwhenua; she was adorned with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Maunganui
Mount Maunganui (, ) is a major residential, commercial and industrial suburb of the Tauranga metropolitan area, located on a peninsula to the north-east of Tauranga's city centre. It was an independent town from Tauranga until the completion of the Tauranga Harbour Bridge in 1988, which connects Mount Maunganui to Tauranga's central business district. Mount Maunganui is also the name of the large lava dome which was formed by the upwelling of rhyolite lava about two to three million years ago. It is officially known by its Māori name '' Mauao'', but is colloquially known in New Zealand simply as ''The Mount''. The New Zealand Ministry for Culture and Heritage gives a translation of "large mountain" for ''Maunganui''. Geography Mount Maunganui is located atop a sand bar that connects Mauao to the mainland, a geographical formation known as a tombolo. Because of this formation, the residents of Mount Maunganui have both a harbour beach (Pilot Bay) and an ocean beach with g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tauranga
Tauranga () is a coastal city in the Bay of Plenty region and the fifth most populous city of New Zealand, with an urban population of , or roughly 3% of the national population. It was settled by Māori late in the 13th century, colonised by Europeans in the early 19th century, and was constituted as a city in 1963. The city lies in the north-western corner of the Bay of Plenty, on the south-eastern edge of Tauranga Harbour. The city extends over an area of , and encompasses the communities of Bethlehem, New Zealand, Bethlehem, on the south-western outskirts of the city; Greerton, on the southern outskirts of the city; Matua, west of the central city overlooking Tauranga Harbour; Maungatapu; Mount Maunganui, located north of the central city across the harbour facing the Bay of Plenty; Otūmoetai; Papamoa, Tauranga's largest suburb, located on the Bay of Plenty; Tauranga City; Tauranga South; and Welcome Bay. Tauranga is one of New Zealand's main centres for business, interna ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāi Te Rangi
Ngāi Te Rangi or Ngāiterangi is a Māori iwi, based in Tauranga, New Zealand. Its rohe (tribal area) extends to Mayor Island / Tuhua and Bowentown in the north, to the Kaimai Range in the west, south of Te Puke and to Maketu in the east. Ngāi Te Rangi is part of the Tauranga Moana iwi group, which also includes Ngāti Pūkenga and Ngāti Ranginui. The three iwi all consider Mauao (Mt Maunganui) sacred and share many things in common with one another. Collectively, the iwi are seeking compensation from the New Zealand Government for their losses from the New Zealand Wars but are yet to seek a settlement. Hapū and marae * Ngā Pōtiki hapū is based at Mangatawa Marae and Tamapahore wharenui at Kairua, and at Tahuwhakatiki/Romai marae and Rongomainohorangi wharenui at Welcome Bay. Ngā Pōtiki a Tamapahore Trust governs the hapū separately from the rest of the iwi. * Ngāi Tamawhariua hapū is based at Te Rangihouhiri/Oruarahi marae and Te Rangihouhiri wharenui on Matakana ... [...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 the de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tainui
Tainui is a tribal waka confederation of New Zealand Māori iwi. The Tainui confederation comprises four principal related Māori iwi of the central North Island of New Zealand: Hauraki, Ngāti Maniapoto, Ngāti Raukawa and Waikato. There are other Tainui iwi whose tribal areas lay outside the traditional Tainui boundaries – Ngāi Tai in the Auckland area, Ngāti Raukawa ki Te Tonga and Ngāti Toa in the Horowhenua, Kapiti region, and Ngāti Rārua and Ngāti Koata in the northern South Island. History Early history The Tainui iwi share a common ancestry from Polynesian migrants who arrived in New Zealand on the ''Tainui'' waka, which voyaged across the Pacific Ocean from Hawaiki to Aotearoa (North Island) approximately 800 years ago. According to Pei Te Hurinui Jones, the Tainui historian, Tainui first entered the Waikato about 1400 bringing with them kumara plants. By about 1450 they had conquered the last of the indigenous people in a battle at Atiamuri. Contact with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene Volcanoes
The Pleistocene ( , often referred to as the ''Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing a faunal interchange between the two reg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of The Bay Of Plenty Region
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava Domes
In volcanology, a lava dome is a circular mound-shaped protrusion resulting from the slow extrusion of viscous lava from a volcano. Dome-building eruptions are common, particularly in convergent plate boundary settings. Around 6% of eruptions on Earth are lava dome forming. The geochemistry of lava domes can vary from basalt (e.g. Semeru, 1946) to rhyolite (e.g. Chaiten, 2010) although the majority are of intermediate composition (such as Santiaguito, dacite-andesite, present day) The characteristic dome shape is attributed to high viscosity that prevents the lava from flowing very far. This high viscosity can be obtained in two ways: by high levels of silica in the magma, or by degassing of fluid magma. Since viscous basaltic and andesitic domes weather fast and easily break apart by further input of fluid lava, most of the preserved domes have high silica content and consist of rhyolite or dacite. Existence of lava domes has been suggested for some domed structures on the Mo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanoes Of The Bay Of Plenty Region
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Volcanoes In New Zealand
This is a partial list of active, dormant, and extinct volcanoes in New Zealand. Kermadec Arc and Havre Trough North Island Taupō Volcanic Zone Elsewhere Mangakino Culdera South Island Other Ross Dependency New Zealand also has ''de facto'' administration over Ross Dependency in Antarctica, which contains the following volcanoes: References External links {{GeoGroupTemplateNew Zealand's Volcanoesat GNS Science New Zealand Volcanoes Volcanoes A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates a ... Geography of the Kermadec Islands ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The New Zealand Herald
''The New Zealand Herald'' is a daily newspaper published in Auckland, New Zealand, owned by New Zealand Media and Entertainment, and considered a newspaper of record for New Zealand. It has the largest newspaper circulation of all newspapers in New Zealand, peaking at over 200,000 copies in 2006, although circulation of the daily ''Herald'' had declined to 100,073 copies on average by September 2019. Its main circulation area is the Auckland region. It is also delivered to much of the upper North Island including Northland, Waikato and King Country. History ''The New Zealand Herald'' was founded by William Chisholm Wilson, and first published on 13 November 1863. Wilson had been a partner with John Williamson in the ''New Zealander'', but left to start a rival daily newspaper as he saw a business opportunity with Auckland's rapidly growing population. He had also split with Williamson because Wilson supported the war against the Māori (which the ''Herald'' termed "the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
