|
Mount Maunganui (mountain)
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] |
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 th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaimai Ranges
The Kaimai Range (sometimes referred to as the ''Kaimai Ranges'') is a mountain range in the North Island of New Zealand. It is part of a series of ranges, with the Coromandel Range to the north and the Mamaku Ranges to the south. The Kaimai Range separates the Waikato in the west from the Bay of Plenty in the east. The highest point of the range is Mount Te Aroha (952 m), at the foot of which is the town of Te Aroha. The range's terrain is rough, and only two roads pass over it: State Highway 2, across the northern end of the range through Karangahake Gorge, and State Highway 29 from Tauranga to Hamilton. Mt Te Aroha can be described as the northern head peak of the Kaimai Range. The New Zealand Ministry for Culture and Heritage gives a translation of "eat fermented food" for ''Kaimāī''. The Kaimai Ranges feature in local Maori folklore. The name Te Aroha translates from Maori as Te - The & Aroha - Love. Literally "the love". The name comes from a Maori legend that th ... [...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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...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 str ... [...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 ... [...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 "t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngati Pukenga
''Ngati'' is a 1987 New Zealand feature film directed by Barry Barclay, written by Tama Poata and produced by John O'Shea. Production ''Ngati'' is of historical and cultural significance in New Zealand as it is the first feature film written and directed by Māori. Producer John O'Shea, an icon in New Zealand's film industry, was the founder of independent film company Pacific Films. The film is set in 1948 in a small town on the east coast of New Zealand during the impending closure of a freezing works and the threat of unemployment for the local community. ''Ngati'' was screened as part of Cannes' Critics Week. Synopsis Set in and around the fictional town of Kapua in 1948, Ngati is the story of a Māori community. The film comprises three narrative threads: a boy, Ropata, is dying of leukaemia; the return of a young Australian doctor, Greg, and his discovery that he has Māori heritage; and the fight to keep the local freezing works open. Unique in tone and quietly powerful ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāi Te Rangi
Ngāi Te Rangi or Ngāiterangi is a Māori people, Māori iwi, based in Tauranga, New Zealand. Its rohe (tribal area) extends to Mayor Island / Tuhua and Waihi Beach, 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 Mt Maunganui, 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. #Governance, Ngā Pōtiki a Tamapahore Trust governs the hapū separately from the rest of the iwi. * Ngāi Tamawhariua hapū is based at Te Rangihouhiri/Orua ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Evelyn Stokes
Dame Evelyn Mary Stokes (née Dinsdale; 5 December 1936 – 15 August 2005) was a professor of geography at the University of Waikato in New Zealand and a member of the New Zealand government's Waitangi Tribunal. Throughout her life she worked for recognition of marginalised groups including women and Māori, and she published extensively on New Zealand historical geography and on Māori land issues.. Biography Evelyn Mary Dinsdale was born in Tauranga, New Zealand, on 5 December 1936. She was educated at Tauranga Primary School and Tauranga College, where she was one of the first non-Māori to join the local kapa haka group.. She then went to Canterbury University College, earning a master's degree with first class honours in geography in 1959. After earning this degree, she took a postgraduate teacher training course from Christchurch Teachers' College and taught briefly at Te Kuiti high school, fulfilling the requirements of the post primary teachers' bursary that had fu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
