Mount Tauhara
Mount Tauhara is a dormant lava dome volcano in New Zealand's North Island, reaching above sea level. It is situated in the area of caldera rim overlap of the Whakamaru Caldera and Taupō Volcano towards the centre of the Taupō Volcanic Zone, which stretches from Whakaari / White Island in the north to Mount Ruapehu in the south. It is east of the town of Taupō, next to the northeastern shore of Lake Taupō. Formed about 65,000 years ago, Mount Tauhara was not a violently explosive vent, instead slowly oozing a viscous dacitic lava. It is the largest mass of dacite within the Taupō volcano, whose material is 98% rhyolitic. Little evidence of its volcanic past remains today; the peak is covered in dense native bush. There is a steep walking track to the top of Mount Tauhara, starting at Mountain Road. On a clear day, the summit offers views over the Volcanic Plateau, encompassing the entirety of Lake Taupō in the southwest. The hike is relatively strenuous and takes ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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North Island
The North Island ( , 'the fish of Māui', historically New Ulster) is one of the two main islands of New Zealand, islands of New Zealand, separated from the larger but less populous South Island by Cook Strait. With an area of , it is the List of islands by area, world's 14th-largest island, constituting 43% of New Zealand's land area. It has a population of which is % of New Zealand's residents, making it the most populous island in Polynesia and the List of islands by population, 28th-most-populous island in the world. Twelve main urban areas (half of them officially cities) are in the North Island. From north to south, they are Whangārei, Auckland, Hamilton, New Zealand, Hamilton, Tauranga, Rotorua, Gisborne, New Zealand, Gisborne, New Plymouth, Napier, New Zealand, Napier, Hastings, New Zealand, Hastings, Whanganui, Palmerston North, and New Zealand's capital city Wellington, which is located at the south-west tip of the island. Naming and usage The island has been known ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lake Taupō
Lake Taupō (also spelled Taupo; or ) is a large crater lake in New Zealand's North Island, located in the caldera of 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. Geography 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, using gates b ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 ''hapū'' (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. ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Tauhara
Tauhara is a suburb and geothermal area of Taupō in the Waikato region of New Zealand's North Island. The area's main geographic feature, Mount Tauhara, is culturally significant to local . It is privately owned but has a public walking track and viewing areas, with panoramic views over Lake Taupō, The tracks were closed in 2015 due to vandalism, but later reopened when the vandalism subsequently stopped. In December 2018, the Taupō District Council reduced the speed limit on the main Tauhara Road from 70 km/h to 50 km/h. Demographics Tauhara covers and had an estimated population of as of with a population density of people per km2. Tauhara had a population of 4,617 in the 2023 New Zealand census, an increase of 216 people (4.9%) since the 2018 census, and an increase of 459 people (11.0%) since the 2013 census. There were 2,268 males, 2,343 females, and 6 people of other genders in 1,605 dwellings. 2.7% of people identified as LGBTIQ+. The median age ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 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 commonly defined as a vent or fissure 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 fo ... Geography of the Kermadec Islands ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Māori Language
Māori (; endonym: 'the Māori language', commonly shortened to ) is an Eastern Polynesian languages, Eastern Polynesian language and the language of the Māori people, the indigenous population of mainland New Zealand. The southernmost member of the Austronesian language family, it is related to Cook Islands Māori, Tuamotuan language, Tuamotuan, and Tahitian language, Tahitian. The Māori Language Act 1987 gave the language recognition as one of New Zealand's official languages. There are regional dialects of the Māori language. Prior to contact with Europeans, Māori lacked a written language or script. Written Māori now uses the Latin script, which was adopted and the spelling standardised by Northern Māori in collaboration with English Protestant clergy in the 19th century. In the second half of the 19th century, European children in rural areas spoke Māori with Māori children. It was common for prominent parents of these children, such as government officials, to us ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Ngati Tuwharetoa
''Ngati'' is a 1987 New Zealand feature film directed by Barry Barclay, written by Tama Poata and produced by John O'Shea (director), 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 people, 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 o ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Te Arawa
Te Arawa is a confederation of Māori people, Māori iwi and hapū (tribes and sub-tribes) of New Zealand who trace their ancestry to the ''Arawa (canoe), Arawa'' migration canoe (''waka''). The tribes are based in the Rotorua and Bay of Plenty areas and have a population of around 60,117 according to the 2018 New Zealand census, 2018 census, making the confederation the sixth biggest iwi in New Zealand. The Te Arawa iwi comprises 56 hapū (sub-tribes) and 31 marae (family groupings). History Te Arawa iwi are descended from people who migrated to New Zealand on the ''Arawa'' canoe. They settled in the Bay of Plenty Region, Bay of Plenty region, principally around the Lakes of Rotorua, Rotorua lakes. Three main subtribes developed: Ngāti Pikiao occupied the eastern end of Lake Rotoiti (Bay of Plenty), Lake Rotoiti and the area around Lake Rotoehu and Lake Rotomā; Tūhourangi occupied the upper Kaituna River, western Lake Rotoiti and the south-east side of Lake Rotorua inclu ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Pūtauaki
Pūtauaki, known in English as Mount Edgecumbe, is a dacite volcanic cone in the Bay of Plenty Region of New Zealand. Located east of Rotorua and three kilometres east of Kawerau, it is the easternmost vent of the Taupō Volcanic Zone adjacent to the Ōkataina volcanic centre. The mountain rises to above sea level, and is visible from the waters of the Bay of Plenty, to the north. A King of the Mountain race was run on Pūtauaki as part of the international King of the Mountain series between 1955 and 2020, and proceeds were donated to charity. History The last substantial volcanic eruption occurred at ± 130 BCE, producing a cubic kilometre of lava. There was a previous eruption dated to ± 50 BCE. The volcano produced the Edgecumbe Formation which are pyroxene-bearing andesite to dacite lava flows, domes and minor pyroclastic tephra. Captain James Cook named the mountain "Mount Edgecumbe" on 2 November 1769, possibly in honour of John Edgecombe, the sergeant of marines o ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Taranaki
Taranaki is a regions of New Zealand, region in the west of New Zealand's North Island. It is named after its main geographical feature, the stratovolcano Mount Taranaki, Taranaki Maunga, formerly known as Mount Egmont. The main centre is the city of New Plymouth. The New Plymouth District is one of three in the region and is home to more than 65 per cent of the population of Taranaki. The Stratford District includes the main centres of Stratford, New Zealand, Stratford, Midhirst, Toko and Whangamōmona, Whangamomona. The South Taranaki District includes Hāwera, Manaia, Taranaki, Manaia, Eltham, New Zealand, Eltham, and Ōpunake. Since 2005, Taranaki has used the promotional brand "Like no other". Geography Taranaki is on the west coast of the North Island, surrounding the volcanic peak of Mount Taranaki. The region covers an area of 7258 km2. Its large bays north-west and south-west of Cape Egmont are North Taranaki Bight and South Taranaki Bight. Mount Taranaki is t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Tongariro
Mount Tongariro (; ) is a complex volcano, 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 Mount Ruapehu, 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. Mount Ngauruhoe, Ngauruhoe, 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, ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |