NoeFlandre/osm-polygon-wikidata-only huggingface dataset:
Національний парк Фіордленд

Національний парк Фіордленд (англ. Fiordland National Park) — найбільший національний парк Нової Зеландії. Географія Національний парк Фіордленд, площею понад 12 500 км², займає більшу частину Фіордленда, у гірській південно-західній частині Південного острова. Фіордленд зі своєї західної частини порізаний фіордами Тасманового моря, а зі сходу обмежений численними озерами. Озера, що розташовані на території Фіордленда (наприклад, озеро поурі), — найглибші в Новій Зеландії та найбільші за площею на Південному острові. Гори в цій частині Нової Зеландії досягають висоти в 2746 метрів. Є кілька мальовничих водоспадів, наприклад Сатерленд, Браун, Стерлінг та Бовен. Разом з національними парками Вестленд, Маунт-Кук та Маунт-Аспайрінґ національний парк Фіордленд утворює зону Всесвітньої спадщини Те-Вахіпоунаму. Національний парк Фіордленд був створений в 1952 році та до сьогоднішніх днів є одним із найбільш важкодоступних районів Нової Зеландії. 1990 року він включається в список Всесвітнього спадщини ЮНЕСКО. Клімат Західні схили гірських хребтів Фіордленда відносяться до одних з найвологіших регіонів на планеті. Клімат в заповіднику — різко океанічний. Температура взимку (в липні) становить приблизно 5 °C, влітку (в січні) — близько 23 °C. Схили гір покриті вологими тропічними лісами (сельва). Протягом 200 днів в році тут йдуть дощі, рівномірно випадаючи протягом року. У зв'язку з численними та тривалими опадами на морській поверхні під фіордах постійно зберігається 40-метровий шар прісної води. Флора та фауна У гірських лісах серед інших порід дерев зустрічаються сріблястий нотофагус віком до 800 років. В парковій зоні численні болота з відповідною рослинністю. У зоні національного парку проживають найбільша кількість лісових птахів Нової Зеландії, їх рідкісні представники, в тому числі останні збережені какапо та такахе. Зустрічаються також ківі бурий, скелястий кропив'яник, косоклюв, стрілець, новозеландські качки, векаралла, жовтолобий стрибаючий папуга. У Фіордленді водиться близько 3.000 видів комах, з яких 10 % зустрічається тільки на території парку. З завезених тварин у Фіордленді слід зазначити оленів вапіті, кускуса та щурів. У фіордах мешкають новозеландські морські котики, пінгвіни Вікторії, а також субтропічні губки, молюски та корали. Тут знаходиться найбільша у світі колонія чорних коралів. Посилання doc.govt.nz/templates/PlaceProfile.aspx?id=38468 Fiordland National Park — Department of Conservation (англ.) Te Wahipounamu (South-West New Zealand) — UNESCO Protected Areas Programme (англ.)
Mangakakahi

Mangakakahi is a suburb of Rotorua in the Bay of Plenty Region of New Zealand's North Island. Demographics Mangakakahi covers 2.81 km2 (1.08 sq mi) and had an estimated population of 2,380 as of June 2025, with a population density of 847 people per km2. Mangakakahi had a population of 2,223 in the 2023 New Zealand census, a decrease of 21 people (−0.9%) since the 2018 census, and an increase of 168 people (8.2%) since the 2013 census. There were 1,110 males, 1,101 females, and 12 people of other genders in 681 dwellings. 3.0% of people identified as LGBTIQ+. The median age was 32.0 years (compared with 38.1 years nationally). There were 561 people (25.2%) aged under 15 years, 483 (21.7%) aged 15 to 29, 978 (44.0%) aged 30 to 64, and 201 (9.0%) aged 65 or older. People could identify as more than one ethnicity. The results were 52.0% European (Pākehā); 54.9% Māori; 11.1% Pasifika; 8.4% Asian; 0.5% Middle Eastern, Latin American and African New Zealanders (MELAA); and 0.8% other, which includes people giving their ethnicity as "New Zealander". English was spoken by 94.7%, Māori by 18.4%, Samoan by 0.7%, and other languages by 7.2%. No language could be spoken by 3.2% (e.g. too young to talk). New Zealand Sign Language was known by 0.4%. The percentage of people born overseas was 15.0, compared with 28.8% nationally. Religious affiliations were 29.4% Christian, 0.7% Hindu, 0.3% Islam, 5.8% Māori religious beliefs, 0.5% Buddhist, 0.5% New Age, 0.1% Jewish, and 1.2% other religions. People who answered that they had no religion were 54.4%, and 7.7% of people did not answer the census question. Of those at least 15 years old, 186 (11.2%) people had a bachelor's or higher degree, 1,008 (60.6%) had a post-high school certificate or diploma, and 474 (28.5%) people exclusively held high school qualifications. The median income was $38,300, compared with $41,500 nationally. 57 people (3.4%) earned over $100,000 compared to 12.1% nationally. The employment status of those at least 15 was 873 (52.5%) full-time, 222 (13.4%) part-time, and 105 (6.3%) unemployed. Education Sunset Primary School is a co-educational state primary school, with a roll of 156 as of March 2026. Te Kura Kaupapa Māori o Hurungaterangi is a co-educational Māori language immersion school for Year 1 to 8 students, with a roll of 95. It opened in 1997 at the Hurungaterangi marae, and moved to its current site in 2005. Te Āhuru Mōwai, formerly Rotorua School for Young Parents, is also located in Mangakakahi. Sunset Intermediate School, later called Sunset Junior High School, opened in 1959 and closed in 2007. References
Mangakakahi

Mangakakahi est une banlieue de la cité de Rotorua dans la région de la baie de l’Abondance de l’Île du Nord de la Nouvelle-Zélande. Municipalités limitrophes Démographie Mangakakahi, comprenant la zone statistique de «Mangakakahi Central» et «Mangakakahi West», avait une population de 2 244 habitants lors du recensement de 2018 en Nouvelle-Zélande, en augmentation de 189 personnes( soit 9,2 %) depuis le recensement de 2013, et une augmentation de 135 personnes(soit 6,4 %) depuis le recensement de 2006 en Nouvelle-Zélande. Il y avait 723 logements. On comptait 1 110 hommes et 1 131 femmes, donnant un sexe-ratio de 0,98 homme pour une femme, avec 606 personnes (27,0 %) âgées de moins de 15 ans, 513 personnes (soit 22,9 %) âgées de 15 à 29 ans, 939 personnes (soit 41,8 %) âgées de 30 à 64 ans, et 183 personnes (8,2 %) âgées de 65 ou plus. L’ethnicité était pour 58,6 % européens/Pākehā, 54,3 % māoris, 8,4 % personnes du Pacifique, 6,7 % asiatiques, et 1,3 % d’une autre ethnicité (le total peut faire plus de 100 % dans la mesure où une personne peut s’identifier de multiples ethnies). La proportion de personnes nées outre-mer était de 11,9 %, comparée avec les 27,1 % au niveau national. Bien que certaines personnes refusent de donner leur religion: 54,7 % n’avaient aucune religion, 29,7 % étaient chrétiens, 0,7 % étaient hindouistes, 0,1 % étaient musulmans, 0,4 % étaient bouddhistes et 7,1 % avaient une autre religion. Parmi ceux d’au moins 15 ans d’âge, 168 personnes (soit 10,3 %) avaient un niveau de licence ou un degré supérieur, et 381 personnes (soit 23,3 %) n’avaient aucune qualification formelle. Le statut d’emploi de ceux d’au moins 15 ans était pour 774 personnes (soit 47,3 %) un emploi à plein temps , pour 252 personnes (soit 15,4 %) un emploi à temps partiel et 150 personnes (9,2 %) étaient sans emploi. Éducation L’école de « Sunset Primary School» est une école primaire, publique, mixte avec un effectif de 122 élèves en juillet 2022 L’école «Te Kura Kaupapa Māori o Hurungaterangi» est une école mixte de type école en immersion en langue Māori (en) pour les années 1 à 8 avec un effectif de 85 élèves L’école de « Rotorua School for Young Parents » est aussi localisée dans le secteur de Mangakakahi dans le district de Rotorua Voir aussi Liste des villes de Nouvelle-Zélande Notes et références (en) Cet article est partiellement ou en totalité issu de l’article de Wikipédia en anglais intitulé « Mangakakahi » (voir la liste des auteurs). Ressource relative à la géographie : New Zealand Gazetteer Portail de la Nouvelle-Zélande
Blue Lake (Tasman)

Rotomairewhenua / Blue Lake is a small lake in Nelson Lakes National Park, in the northern reaches of New Zealand's Southern Alps. Sacred to local Māori, it has the clearest natural fresh water in the world. Description The Blue Lake is drained by the west branch of the Sabine River, which is part of the Buller River system. It is fed by a short upper segment of the Sabine, which in turn is fed by underground seepage through the landslide debris impounding the much larger Lake Constance. Blue Lake is roughly boomerang shaped, running north then northwest, with each arm of the lake stretching some 200 metres (700 ft). Its waters are cold, ranging from 5 to 8 °C (41 to 46 °F). Clarity The lake has extremely clear water, and is the clearest natural body of fresh water yet reported. A 2011 study found its visibility ranged from 70 to 80 metres (230 to 260 ft), clearer than the 63 metres (207 ft) measured for Te Waikoropupu Springs, a previous record holder. For comparison, laboratory measurements show distilled water has a visibility of approximately 80 metres (260 ft). Scientists attribute the lake water's clarity to its passage underground from Lake Constance, which filters out nearly all the particles suspended in the water. Its clarity reveals water's natural blue-violet colour. Facilities and access Blue Lake is most often reached as a side trip from the Travers-Sabine Circuit, although a marked route to the south, over the Waiau Pass and another to the West, via Moss Pass continues beyond the lake. The nearby Blue Lake Hut, with 16 bunks, provides accommodation for more than 700 trampers each year. Māori history Blue Lake lies within the rohe (tribal area) of Ngāti Apa ki te Rā Tō. As part of the iwi's 2010 treaty settlement, the lake passed into tribal ownership and was then given back to the Crown. The lake was traditionally used in ceremonies to cleanse the bones and release the spirits of the dead, so they could begin their journey to Hawaiki, and the iwi regard its waters as tapu (sacred). (Blue Lake was used only for males; Lake Constance was used for females.) Its Māori name, Rotomairewhenua, means "the lake of peaceful lands". In August 2014, the official name for Blue Lake was altered to Rotomairewhenua / Blue Lake, following the Ngāti Apa ki te Rā Tō treaty settlement with the Crown. References
Waipu Scottish Migration Museum

The Waipu Scottish Migration Museum, also known as the Waipu Museum, is a local museum in the township of Waipu in the Whangarei District, Northland, New Zealand. The museum focuses on the local history of Scottish Nova Scotian migration to the township. In 2016, much of the museum's archival collection was included in the UNESCO New Zealand Memory of the World Register. History The Waipu Memorial Museum was opened in January 1953, established to celebrate the centennial of Scottish migration to Waipu. The building was constructed by descendants of the original settlers, and built in stone to resemble a Scottish highland crofter's dwelling, and was named the House of Memories by the descendants. Early collections included family heirlooms and family trees of the Waipu settlers, and while the facility operated long term, it was often closed. In 1981, resident Betty Powell took over the museum operations, developing the oral history and genealogy resources of the museum. In 2003 to celebrate the 150th anniversary, a modern extension to the museum was added. Part of the 150th anniversary celebrations included staging an updated version of a 1953 pageant based on the settlers history. The additional research into the story highlighted the need for the museum to more actively research Waipu's Scottish migration stories. The Waipu Museum sponsored a production of James McNeish's play The Rocking Cave (1973), performed in June 2007 at Waipu. During the 2010s, the Waipu Scottish Migration Museum was criticsed for not including Māori perspectives on the history of Waipu. In response, the museum's 2021 Strategic Plan included planned goals for the museum such as increasing the awareness of the Treaty of Waitangi, collaborating with local hapū Patuharakeke on content, and developing research and acquiring objects of significance related to Patuharakeke and early Scottish migrants. The archival documents of Scottish migration held at Waipu Museum were included in the UNESCO Memory of the World Aotearoa New Zealand Ngā Mahara o te Ao register in 2016. In 2019, a 200 year old antique doll which was part of the UNESCO collection was stolen from the Waipu Museum, returned two days later in a damaged condition. Displays and exhibits The museum tells the history of the area's Scottish migration history during the colonial era of New Zealand. References External links Waipu Museum website Scottish Migration Collection on the UNESCO Memory of the World Aotearoa New Zealand Trust website Waipu Museum at Auckland Libraries Heritage Collections
Macleans College

Das Macleans College ist ein College in Bucklands Beach, einem Stadtteil von Auckland, der größten Stadt Neuseelands. Die Schule wurde im Jahr 1980 von Generalgouverneur David Beattie eröffnet. 2010 hatte die Schule mehr als 2500 Schüler. Whanau House System Als erste öffentliche Schule Neuseelands macht das Macleans College Gebrauch vom sogenannten „Whanau House System“. Dieses unterteilt die Schule in acht Häuser, denen jeweils etwa 300 Schüler angehören. Dadurch entsteht innerhalb jedes Hauses ein Gefühl des Zusammenhaltes und der Zugehörigkeit. Im Schulalltag werden die Häuser sogar als Familienersatz bezeichnet. Vor allem Sportereignisse gestalten sich durch dieses System interessant, da die Möglichkeit besteht, verschiedene Häuser gegeneinander antreten zu lassen. Die acht Häuser wurden nach bekannten Neuseeländern benannt: Batten, Mansfield, Rutherford, Kupe, Hillary, Te Kanawa, Snell und Upham. Austauschschüler Die Schule finanziert sich hauptsächlich durch Gebühren zahlende ausländische Gastschüler. Der Preis für einen einjährigen Schulaufenthalt liegt 2010 bei 15.000 neuseeländischen Dollar (etwa 8500 € (Kurs 11/2010)). Schüler mit festem Wohnsitz in Neuseeland sind von dieser Gebühr befreit. Der Großteil der „International Students“ stammt aus Asien, hinzu kommen vor allem Europäer und Südamerikaner. 2010 lernen etwa 50 Deutsche am Macleans College. Bildungswege Den Schülern der Oberstufe bietet das Macleans College zwei verschiedene Bildungswege. Sie können entweder das neuseeländische (National Certificate of Educational Achievement) oder international anerkannte Prüfungen der Universität Cambridge (CIE) absolvieren. Außerschulische Aktivitäten Das Angebot der Schule umfasst sportliche Aktivitäten wie Fußball, Tennis, Hockey, Rugby, Cricket, Volleyball, Basketball, Tischtennis, Segeln, Mountainbiking, Rennradsport, Windsurfen oder Netball und kulturelle Aktivitäten wie Theater, Kunst und Sprachen. Weblinks Einzelnachweise
Lake Pupuwharau

Der Lake Pupuwharau ist ein See im Whakatāne District und zu einem kleinen Teil im Kawerau District in der Region Bay of Plenty auf der Nordinsel von Neuseeland. Geographie Der Lake Pupuwharau befindet sich rund 380 m östlich von Kawerau und rund 130 m südlich angrenzend zum Areal des Sägewerks der Stadt. Der See, der über einen einzigen, vom kleinen südlichen Feuchtgebiet zulaufenden Bach, aber keinen Abfluss verfügt, umfasst eine Fläche von rund 21,5 Hektar. Bei einem Seeumfang von rund 2,27 km erstreckt sich das Gewässer über eine Länge von rund 580 m in Nordnordost-Südsüdwest-Richtung und über eine maximale Breite von rund 540 m in Westnordwest-Ostsüdost-Richtung. Weniger als 200 m westlich angrenzend fließt der Tarawera River in Richtung Norden vorbei. Siehe auch Liste der Seen in Neuseeland Weblinks Lake Pupuwharau. In: New Zealand Gazetteer. Land Information New Zealand, abgerufen am 15. Februar 2023 (englisch). Einzelnachweise
Tauparikākā Marine Reserve

Tauparikākā Marine Reserve is a marine reserve located offshore about 20 kilometres (12 mi) north of Haast on the West Coast of New Zealand's South Island. It covers the area immediately offshore from Ship Creek, which is also known as Tauparikākā in Māori. The marine reserve was established in 2014 and is administered by the Department of Conservation. It is New Zealand's smallest marine reserve, covering an area of just 16 hectares (40 acres). Geography The reserve extends about 630 metres (2,070 ft) along the coastline from the Ship Creek Beach Walk north of Haast, and approximately 200 metres (660 ft) out from the shoreline. It adjoins the coastlines of Te Wahipounamu and Tauparikākā Mātaitai Reserve, and includes the Ship Creek tidal river mouth, lagoon and beach foreshore. Tauparikākā includes natural examples of different habitat types: sandy beaches, the stream mouth of Ship Creek, and the shore habitats reaching out to a depth of about 5 metres (16 ft). Tutumairekurai (Hector’s dolphins) swim the shallow waves and seabirds like fairy prions and muttonbirds. The reserve area lies within the narrow inner shelf zone, inshore of deeply incised submarine canyons. On shore from the reserve, there is an ancient kahikatea swamp forest and a dune lake, resembling how the West Coast landscape may have looked before human settlement. History While the area is known as Tauparikākā in Māori, it gained the European name Ship Creek after fragments of the ship Schomberg were found at the creek between 1871 and 1875. The marine reserve was established on 7 September 2014. It was created for educational rather than conservationist reasons, as a way for people to have easy viewing access to Hector’s dolphins. Recreation The marine reserve is accessible via a carpark and walkway on State Highway 6 north of Haast. According to the Department of Conservation, the marine reserve includes a range of habitats in a small area, including one of the best places to see Hector's dolphins without a boat. It recommends insect repellent and advises against swimming. Tauparikākā and Ship Creek is the starting point for walks around the nearby dune lake and swamp forest. A range of activities are banned in the marine reserve, including fishing, taking or killing marine life, and moving or removing any marine life or materials. People must not feed fish as it disturbs their natural behaviour, and they must take care when anchoring to avoid damaging the sea floor. Quad bikes and horses are allowed within the reserve, provided there is minimal disturbance to the site. Small stones, shells, driftwood, sand and gravel can be collected by hand. Pounamu (greenstone) can also be collected by Ngāi Tahu. See also Marine reserves of New Zealand References
Christchurch Bus Interchange

The Christchurch Bus Interchange is a bus station in the Christchurch Central City in New Zealand. Built as one of the 17 anchor projects identified in the Christchurch Central Recovery Plan, it opened in May 2015 after the previous Bus Exchange had been damaged in the 2011 Christchurch earthquake. History Historically, Cathedral Square was the main facility for public transport users in central Christchurch. That changed when the Bus Exchange opened in November 2000 in Lichfield Street, with most bus routes using an indoor facility off Lichfield Street with direct pedestrian access in City Mall. The building that housed the Bus Exchange was damaged in the 2011 Christchurch earthquake and was later demolished. From October 2011, a temporary station—Central Station—was established in a block further west. This block was surrounded by Lichfield, Colombo, Tuam, and Durham streets, and the facility was expected to be in use for "up to two years". The Bus Interchange was one of 17 anchor projects for the central city's earthquake recovery, outlined in the Christchurch Central Recovery Plan, published in July 2012. It set an indicative start date of 2012 and completion by June 2014. Christchurch City Council's District Plan was amended and two-thirds of the block surrounded by Lichfield, Manchester, Tuam, and Colombo streets designated for the Bus Interchange. The most significant building that had to be demolished to make way for the proposed Bus Interchange was Miller's Department Store, better known for its subsequent use from 1980 to 2010 as the head office of Christchurch City Council. Construction Construction of the Bus Interchange started in July 2014, after the projected completion date for the building. The recovery plan identified ECan (Environment Canterbury, the regional council), CCC (Christchurch City Council), CERA (Canterbury Earthquake Recovery Authority), NZTA (NZ Transport Agency), and the private sector as project partners, but the project was carried out by CERA. Central Station was in use until 25 May 2015, when Christchurch's new $53 million Bus Interchange building opened, with half of the 16 bays operational. On 20 August, the building was physically completed and further opened to the public, including bike parking and more seating. On 8 October, the remaining bays opened. Later retailers took spaces. Notes References Christchurch Central Recovery Plan: Te Mahere 'Maraka Ōtautahi' (PDF). Christchurch: Canterbury Earthquake Recovery Authority. March 2014. ISBN 978-0-478-39719-2.
Frying Pan Lake

Frying Pan Lake nebo také Waimangu Cauldron je termální pramen na Novém Zélandu. Má rozlohu 3,8 hektaru, průměrná hloubka činí šest metrů a maximální přes dvacet metrů a objem 200 000 m³, řadí se tak k největším geotermálním jezerům na světě. Pramen se nachází v kráteru Echo, který náleží k chráněné oblasti údolí Waimangu nedaleko města Rotorua (region Bay of Plenty). Horké prameny zde vznikly v důsledku erupce sopky Mount Tarawera 10. června 1886, k poslednímu výbuchu došlo 22. února 1973. Voda dosahuje teploty 55-60 °C a má pH 3,8, díky unikajícímu oxidu uhličitému a sulfanu jezero neustále bublá a hladina je zahalena oblaky páry. Ve vodě žijí termofilní organismy, jako je Cyanidium caldarium. Reference Externí odkazy Obrázky, zvuky či videa k tématu Frying Pan Lake na Wikimedia Commons
Frying Pan Lake

Der Frying Pan Lake (auch Waimangu-Kessel) ist ein See vulkanischen Ursprungs in Neuseeland. Geographie Der See liegt auf der Nordinsel Neuseelands im Waimangu Volcanic Rift Valley. Er entstand erst am 10. Juni 1886 durch den Ausbruch des Mount Tarawera. Er befindet sich zusammen mit dem ehemaligen Waimangu-Geysir in einem der damals entstandenen Krater, dem Echo-Krater etwa 10 km südwestlich vom heutigen Gipfel. Nordöstlich des Sees befindet sich der größere Lake Rotomahana, die nächstliegende Ansiedlung ist Waimangu etwa 1 km südwestlich. Ron Keam von der Universität Auckland führte 1976 bis 1978 eine umfassende Vermessung des Sees und engmaschige Tiefemessungen mit einem Lot durch. Dazu verwendete er zum Schutz gegen das heiße Wasser ein mit Polyurethanschaum wärmegedämmtes Holz-Dingi. Der See ist mit einer Fläche von 3,8 ha und einem Volumen von etwa 200.000 m³ die größte Thermalquelle der Welt. Der See ist etwa 300 m lang und 200 m breit. Der Grund ist über große Strecken und im Mittel 6 m tief. Einige Teile erstrecken sich in größere Tiefe: die größte Tiefe ermittelte Keam mit 20,88 m im Ostteil des Sees, eine weitere tiefe Stelle mit bis zu 15,03 m befindet sich am Südende des Sees. Seine Wassertemperatur beträgt im Mittel 45 °C bis 55 °C. Der pH-Wert des Wassers beträgt 3,5 und liegt damit im sauren Bereich. Geschichte Der Bereich um den See erlebte seit der Eruption, die zu seiner Entstehung führte, keine weiteren Vulkanausbrüche. In den Jahren 1915, 1917, 1924 und 1973 kam es jedoch zu Ausbrüchen von Dampf und Heißwasser. In den Jahren von 1900 bis 1904 war unmittelbar nordwestlich vom heutigen See der größte Geysir der Welt, der Waimangu-Geysir, aktiv. Siehe auch Liste der Seen in Neuseeland Einzelnachweise