NoeFlandre/osm-polygon-wikidata-only huggingface dataset:
Вестленд (національний парк)

Національний парк Вестленд Таї Поутіні (англ. Westland Tai Poutini National Park) — національний парк в Новій Зеландії, розташований в західній часті Південного острова, між Південними Альпами і узбережжям острова. Парк заснований в 1960 році. Площа парку — 1175,47 км². На території парку розташовані декілька крупних льодовиків, в тому числі льодовик Фокса і льодовик Франца Йосифа. У парку популярне полювання на оленя, сарн і тарів. По парку протікає річка Карангаруа. У 2010 році до парку були приєднані більше 4400 гектарів землі, більша частина яких розташовується на схід від лагуни Окаріто. Посилання Kate Wilkinson (17 липня 2010). beehive.govt.nz - New additions to Westland National Park. Архів оригіналу за 3 березня 2012. Процитовано 2011–4–12. : Cite має пустий невідомий параметр: |description= (довідка)Обслуговування CS1: Сторінки з неправильним форматом в діапазонах дат (посилання)
Terrace End Cemetery

Terrace End Cemetery is the oldest cemetery in Palmerston North, New Zealand. Almost 10,000 people have been buried in the cemetery since Rangitāne gifted the land to the fledgling Palmerston North settlement in 1875. Plots are now closed, but the descendants of those buried at the cemetery can be buried with their relatives. The cemetery was replaced by Kelvin Grove Cemetery in 1927. Burials George Snelson the first Mayor of Palmerston North and is considered Palmerston North's founding father. Edward McKenna a British Army soldier and a recipient of the Victoria Cross. Jimmy Nash a Mayor of Palmerston North. Joseph Hodgens a politician for the New Zealand Labour Party. Rangi Mawhete a land agent, interpreter and politician. Sarah McMurray a woodcarver and craftswoman. References External links Palmerston North cemeteries search Terrace End Cemetery at Find a Grave
Tuamarina Cemetery

Tuamarina Cemetery is one of the largest cemeteries in the Marlborough Region of New Zealand. The cemetery predates Omaka Cemetery and has been open to the public for burials since 1866, notwithstanding the burials of twenty two men there in 1843. History The site of Tuamarina Cemetery was first used for burials in 1843, when the Rev. Samuel Ironside interred most of the twenty two men who were killed during the Wairau Affray, the first clash of arms between British settlers and Māori in New Zealand after the signing of the Treaty of Waitangi. After fighting began, many of the surviving party of British settlers retreated to the top of the hill, where they surrendered and were subsequently killed as utu. Felix Wakefield designated the area as a cemetery and was instrumental in the installation of a monument to the deceased. On 9 March 1866 the monument was unveiled by William Henry Eyes and Wakefield in a large ceremony. The original monument face was updated in 1869 after multiple spelling errors were noted. Inside the cemetery is also a memorial to the soldiers from the Marlborough region killed during the Second Boer War. The memorial was unveiled on 3 June 1904 in the presence of a large audience. Also present is a 1917 75 mm Skoda Howitzer, brought back to New Zealand in the 1920s, which acts as a memorial to all servicemen and women buried in the cemetery. Below the cemetery is also the Eileen Duggan Green, a small park with a memorial in memory of poet Eileen Duggan who was born and raised in the district. The memorial was unveiled on the 7 October 2009 by then-Deputy Mayor Jenny Andrews as part of Marlborough's 150th Anniversary Celebrations. Notable burials John Clervaux Chaytor (1836–1920), Farmer and businessman. Father of Sir Edward Walter Clervaux Chaytor. Arthur Wakefield (1799–1843), Royal Navy Captain and a New Zealand Company Official who was killed during the Wairau Affray. References External links Official website and interment records
Hillsborough Cemetery

Hillsborough Cemetery is a large cemetery located in the Auckland isthmus suburb of Hillsborough. Location The cemetery lies on a ridge at the south of the Auckland isthmus, overlooking the Manukau Harbour. The cemetery is split in two by a large forested valley, adjacent to the Hillsborough Reserve. Erosion is a problem for the cemetery, due to its hillside location. The cemetery is a part of the Waikōwhai Walkway, which extends for 10 km (6.2 mi) linking Onehunga to Lynfield Cove. Road access is by Clifton Road, off Hillsborough Road, Route 15. History Hillsborough Cemetery is one of the older cemeteries in the Auckland Region. It was purchased by the Onehunga Borough Council and established in 1916, to provide more space for burials as Waikaraka Cemetery, closer to Onehunga, no longer had available space. During the first six years of operation, very few burials were undertaken at the cemetery, primarily of paupers along the eastern section along Goodall Street. Onehunga Borough Council advertised for a caretaker for Hillsborough Cemetery in 1917, when Waikaraka Cemetery was nearly full. Agreement was reached with Mount Roskill Road Board about access, though further discussed in 1923 and 1935. The cemetery was primarily in use between 1916 and 1976, and it served as an administration hub for the cemeteries of the area, and people were able to reach the cemetery through a bus service, which stopped within the cemetery. The cemetery features sections for three religious orders: St Mary's of Ponsonby, Little Sisters of the Poor (also of Ponsonby) and the Sisters of the Good Shepherd, of Waikōwhai. The final plots in the cemetery were sold in 1974, however burials have continued in the reserved plots. Burials Some of the notable people buried at the cemetery include: Bessie Blomfield (1880–1984), New Zealand artist known as Elizabeth Kendon, and daughter of Charles Blomfield Charles Blomfield (1848–1926), New Zealand artist James Bradney (1853–1936), New Zealand politician Bill Cunningham (1874–1927), New Zealand rugby union player Hannah Dudley (1862–1931), Australian missionary to Suva Emily Patricia Gibson (1864-1947), Auckland feminist, socialist and proofreader Edith Searle Grossmann (1863–1931), New Zealand teacher and novelist Richard Henry (1845–1929), New Zealand conservationist Henry Kelliher (1896–1991), New Zealand businessman Bobby Leach (1858–1926), the second person to go over the Niagara Falls Nisbet McRobie (1872–1929), New Zealand rugby union player, master printer, newspaper proprietor, and politician. William Joseph Napier (1857–1925), New Zealand politician Annette Paul (1863–1952), New Zealand salvation army officer Margaret Beveridge Stevenson (1865–1941), New Zealand Baháʼí follower See also List of cemeteries in New Zealand Notes
Madills Farm Reserve

Madills Farm Reserve, also known as Madills Farm, is a reserve and sports ground in the suburb of Kohimarama in Auckland, New Zealand. It is the home ground of Eastern Suburbs and the Kohimarama Yacht club. History Before European settlers arrived in New Zealand, the Madills Farm area was known by Māori as Waipara ra which meant duck water. In 1919 a Mr William Madill, a local farmer, was granted a 21-year lease of a 119 acre block estate at £246 per annum, that would include what is now known as Madills Farm Reserve. Madill surrendered part of the land back to the Trust in 1920 as they had decided to subdivide the land near the beach however he farmed the remainder until 1944. In 1943 the Melanesian Trust Board subdivided the land and planned to build houses and shops on it, but they also set aside 30 acres to be developed as reserve land by the local council for recreational purposes. The site was used as a land-fill until the Council finalised the purchase in 1959. In 1975, Council considered developing playing fields for rugby, hockey and football, as well as building sports complex on the area. This was opposed by local residents so the sports complex was never built. Ground layout The reserve is divided into two open spaces, one with informal recreation and the other with organised recreation, which has the playing fields. References External links Friends of Madills Farm Eastern Suburbs AFC Kohimarama Yacht Club Parnell Cricket Club
Chalice (Christchurch)

The Chalice, manchmal auch Millennium Cone genannt, ist eine aus Stahl und Aluminium gefertigte Skulptur auf dem Cathedral Square in der neuseeländischen Großstadt Christchurch. Sie ist zusammen mit der nach dem Erdbeben beschädigten Christ Church Cathedral das Wahrzeichen der Stadt. Anlass für den Bau des „Kelches“ war die 150-Jahr-Feier der Stadt Christchurch und der Region Canterbury durch die Canterbury Association im Jahr 2001. Das Kunstwerk wurde am 10. September 2001 durch das erstmalige Einschalten des Flutlichtes im Inneren eingeweiht. Der neuseeländische Künstler und Bildhauer Neil Dawson hat die Skulptur entworfen. In Aluminium ließ er 42 Blätter einheimischer Pflanzenarten in das aus sechseckigen Waben aufgebaute Stahlskelett einarbeiten. Die Blätter repräsentieren heimische Baumarten: Mapou, Kowhai, Mahoe, Totara, Karamu, Titoki, Ngaio, Maratata und Koromiko. Die Skulptur stelle eine Verbindung zu Christchurchs Spitznamen „Gartenstadt“ her. Das Werk misst 18 Meter in der Höhe, 2 Meter Durchmesser an der Basis und 8,5 Meter Durchmesser über den oberen Rand. Die Basis entspringt aus einem aus sechs Segmenten gefertigten Ring mit drei Metern Durchmesser aus dunklem Granit. Die Skulptur ist im Inneren blau und außen silberfarbig lackiert und wird nachts von innen und außen beleuchtet. Der prominente Christchurcher Architekt Peter Beaven nannte die Skulptur „vent to an underground toilet“ („Abluftschacht einer unterirdischen Toilette“). Weblinks Einzelnachweise
The Chalice

The Chalice is a sculpture in Cathedral Square, Christchurch, New Zealand. Designed by sculptor Neil Dawson, it was created to mark the 150th anniversary of the settlement of Canterbury, and installed in the square in 2001. The conical sculpture features the leaves of New Zealand native plants. Design The Chalice was designed by sculptor Neil Dawson and is 18 metres tall. It is the shape of a cone, with its diameter at the ground being 2 metres and at the top 8.5 metres. It has steel hexagons with aluminium leaf patterns of native plants within them. The exterior is painted silver and the interior blue. The shape of the sculpture was made to reflect the shape of the spire of Christ Church Cathedral. History The Chalice was made to celebrate the 150th anniversary of the settlement of Canterbury and was placed in Cathedral Square in 2001 at a cost of $400,000. Shortly after the sculpture's lighting ceremony on 10 September 2001, the September 11 attacks occurred and the Chalice became a location where the local community placed flowers and messages for the victims of the attacks. When the 2011 Christchurch earthquake occurred, the Chalice was not damaged, unlike other structures in Cathedral Square, such as Christ Church Cathedral which lost its spire. At the time Dawson said, for this reason, that the sculpture "could become a sign of the recovery rather than a sign of the quake". In March 2025 restoration began on the Chalice with a budget of $400,000. It involved temporarily removing the leaves for repainting, placing scaffolding around the structure and wrapping it to protect it from dust and the weather. The lighting was also replaced and corrosion was fixed. Christchurch City councillor James Gough criticised the cost and called for an "immediate halt" on the work, saying that the funds would be better allocated to "roads, footpaths and essential core services". The restoration was part of the council's long term plan and had been approved by a "delegated authority" however. Gallery References External links Media related to Chalice, Christchurch at Wikimedia Commons
Езерото на шампанското

-38.37, 176.35 Езерото на шампанското (на английски: Champagne Pool) e кратерно езеро намиращо се на Северния остров в Нова Зеландия, на около 30 км югозападно от град Роторуа и на 50 км североизточно от езеро Таупо. Диаметъра на кратера е 65 метра, дълбочината му е около 62 метра и езерото е напълнено с 50 000 м³ вода. На мястото му имало удивително красиви бели и розови скални тераси, но през 1886 г. изригнал вулканът Маунт Тарауера. От кратера се издигали пламъци на височина 300 м., а тътенът от изригванията се чувал на 160 км. На мястото на терасите се появило блестящо смарагдово зелено езеро, димящи от пара скали и нови тераси, оцветени в зелено, оранжево, кафяво и черно. Топлият извор който днес затопля езерото се формирал преди около 900 години. Този извор затопля водата на езерото до температура, достигаща 260 °C, но температурата спада когато водата достигне повърхността на езерото, така че температурата на повърхността на езерото е между 73 °C и 75 °C.
Champagne Pool

Champagne Pool - en anglès literalment “piscina de xampany” - és un llac a l'Illa del Nord de Nova Zelanda. És un llac natural d'aigües calentes de la zona termal de Wai-O-Tapu, a la regió de Waikato. La font calenta és a uns 30 km al sud-est de Rotorua i 50 km al nord-est de Taupo. El nom de Champagne Pool es deu a les abundants emanacions de diòxid de carboni (CO₂) que recorden les bombolles en un got de xampany. La font calenta es va formar fa uns 900 anys a causa d'una erupció hidrotermal, el que la fa, a escala geològica, un sistema relativament jove. El seu cràter té prop de 65 metres de diàmetre i aconsegueix una profunditat de l'ordre de 62 metres i un volum estimat de 50.000 m³. Característiques tèrmiques i químiques Les aigües més profundes de Champagne Pool són a una temperatura d'uns 260 °C però la temperatura de l'aigua del llac és entre 73 °C i 75 °C a causa del seu refredament al contacte amb l'atmosfera. El seu pH és relativament constant, de l'ordre de 5,5, a causa del tamponament pel flux de CO₂. Entre els gasos del llac el més abundant és el diòxid de carboni (CO₂), però també, en menor mida, hi ha el nitrogen (N₂), metà (CH₄), hidrogen (H₂), sulfur d'hidrogen (H₂S) i rastres d'oxigen (O₂). El fluid geotermal silícic està saturat per metal·loides com l'orpiment (As₂S₃) i l'estibina (Sb₂S₃) que precipiten i formen dipòsits ataronjats, que contrasten fortament amb el to grisenc del sílice de les ribes de Champagne Pool. Característiques biològiques Mentre que les característiques geoquímiques de Champagne Pool són ben conegudes, molt pocs estudis s'han interessat per les formes de vida microbiana que podria acollir. L'H₂ i també el CO₂ o l'O₂ H podrien constituir fonts d'energia que permetrien el desenvolupament autotròfic de microorganismes metanògens o hidrogen-oxidants. A Champagne Pool s'han descobert dues noves espècies de bacteris i una d'archaea. El bacteri CP.B2 nomenada Venenivibrio stagnispumantis suporta continguts relativament fortes en compostos d'arsènic i d'antimoni i representa un nou gènere i una nova espècie en l'ordre de Aquificae. Referències
Champagne Pool

Der Champagne Pool ist mit einem Durchmesser von 65 m, einer Tiefe von 62 m und einem geschätzten Wasservolumen von 50.000 m3 eine der größten Thermalquellen Neuseelands. Der Champagne Pool gehört zu dem 18 km2 großen Geothermalgebiet Wai-O-Tapu, das 20 km südlich von Rotorua beginnt. Der Pool selbst befindet sich weitere 7 km südlich und ist über den Park Wai-O-Tapu Thermal Wonderland zugänglich. Der State Highway 5 führt westlich in der Nähe des Sees vorbei. Das 74 °C heiße Wasser ist übersättigt mit den Metalloidverbindungen Orpiment (As2S3) und Stibnit (Sb2S3), welche ausfallen und ein orangefarbiges Sediment bilden. Der Name „Champagne Pool“ leitet sich von dem kontinuierlichen Strom an Gasblasen ab, die zur Wasseroberfläche aufsteigen, vergleichbar Gasperlen in einer Flöte Champagner. Das entweichende Gasgemisch besteht hauptsächlich aus Kohlendioxid (CO2), zu einem geringen Anteil aus Stickstoff (N2), Methan (CH4), Wasserstoff (H2), Wasserstoffsulfid (H2S) und Spuren von Sauerstoff (O2). Im Champagne Pool findet sich das bisher einzige bekannte Vorkommen des Bakteriums Venenivibrio stagnispumantis. Siehe auch Liste der Seen in Neuseeland Weblinks Einzelnachweise
Champagne Pool

Champagne Pool is a prominent geothermal feature within the Waiotapu geothermal area in the North Island of New Zealand. The terrestrial hot spring is located about 30 km (20 mi) southeast of Rotorua and about 50 km (30 mi) northeast of Taupō. The name Champagne Pool is derived from the abundant efflux of carbon dioxide (CO2), similar to a glass of bubbling champagne. The hot spring was formed 900 years ago by a hydrothermal eruption, which makes it in geological terms a relatively young system. Its crater is about 65 m (213 ft) in diameter with a maximum depth around 62 m (203 ft) and is filled with an estimated volume of 50,000 m3 (1,800,000 ft3) of geothermal fluid. Hydrochemistry The deep geothermal water below Champagne Pool is of the order of 260 °C (500 °F) but water temperature within the pool is maintained at 73 °C (163 °F) to 75 °C (167 °F) by losing heat to the atmosphere. The pH of 5.5 is relatively constant due to buffering by the flux of CO2. Gases are mainly CO2, but to lesser extent nitrogen (N2), methane (CH4), hydrogen (H2), hydrogen sulphide (H2S), and traces of oxygen (O2). The siliceous geothermal fluid is oversaturated with metalloid compounds such as orpiment (As2S3) and stibnite (Sb2S3), which precipitate and form orange subaqueous deposits. The colourful deposits are in sharp contrast to the grey-white silica sinter surrounding Champagne Pool. Biology Although Champagne Pool is geochemically well characterised, few studies have addressed its role as a potential habitat for microbial life forms. H2 and either CO2 or O2 would be available as metabolic energy sources for autotrophic growth of methanogenic or hydrogen-oxidising microorganisms. Culture-independent methods provided evidence for filamentous, coccoid, and rod-shaped cell morphologies in the hot spring. Two novel bacteria and a novel archaeon have been successfully isolated from Champagne Pool. Bacterial isolate CP.B2 named Venenivibrio stagnispumantis tolerates relatively high concentrations of arsenic and antimony compounds and represents a novel genus and species within the order Aquificales. See also Hot springs in New Zealand References External links Media related to Champagne Pool at Wikimedia Commons
Champagne Pool

Champagne Pool es un lago de Nueva Zelanda, situado en la isla Norte. Es un lago natural de aguas calientes de la zona termal de Wai-O-Tapu, en la región de Waikato. La fuente caliente está situada a unos 30 km al sureste de Rotorua y 50 km al nordeste de Taupo. El nombre de Champagne Pool se debe a las abundantes emanaciones de dióxido de carbono (CO2) que recuerdan las burbujas en una copa de champán. La fuente caliente se formó hace unos 900 años debido a una erupción hidrotermal,​ lo que lo hace, a escala geológica, un sistema relativamente joven. Su cráter tiene cerca de 65 metros de diámetro y alcanza una profundidad del orden de 62 metros y un volumen estimado de 50.000 m³.​ Características térmicas y químicas Las aguas más profundas de Champagne Pool están a una temperatura de aproximadamente 260 °C,​ pero la temperatura del agua del lago se sitúa entre 73 °C y 75 °C a causa de su enfriamiento al contacto con la atmósfera. Su pH es relativamente constante, del orden de 5,5, a causa del tamponamiento por el flujo de CO2. Entre los gases del lago, el más abundante es el dióxido de carbono (CO2), pero también, en una menor medida, se encuentra nitrógeno (N2), metano (CH4), hidrógeno (H2), sulfuro de hidrógeno (H2S) y rastros de oxígeno (O2).​ El fluido geotermal silíceo está saturado por metaloides como el oropimente (As2S3) y la estibina (Sb2S3), que precipitan y forman depósitos anaranjados,​ que contrastan fuertemente con el tono grisáceo del sílice de las orillas de Champagne Pool. Características biológicas Mientras que las características geoquímicas de Champagne Pool son bien conocidas, muy pocos estudios se han interesado por las formas de vida microbiana que podría acoger. El H2 y también el CO2 o el O2H podrían constituir fuentes de energía que permitirían el desarrollo autotrófico de microorganismos metanógenos o hidrógeno-oxidantes. Dos nuevas bacterias y una nueva archaea han sido descubiertas en Champagne Pool.​ La bacteria CP.B2 nombrada Venenivibrio stagnispumantis soporta contenidos relativamente fuertes en compuestos de arsénico y de antimonio, y representa un nuevo género y una nueva especie en el orden de Aquificae.​ Referencias
Champagne Pool

Champagne Pool est un bassin naturel d’eau chaude de la zone thermale de Wai-O-Tapu dans la région du Waikato en Nouvelle-Zélande. La source chaude est située à environ 30 km au sud-est de Rotorua et 50 km au nord est de Taupo. Le nom de Champagne Pool provient des abondantes émanations de dioxyde de carbone (CO2) qui rappellent les bulles dans un verre de Champagne. La source chaude s'est formée il y a 900 ans à la suite d'une éruption hydrothermale, ce qui en fait, à l'échelle géologique, un système relativement jeune. Son cratère fait environ 65 mètres de diamètre et atteint une profondeur de l'ordre de 62 mètres pour un volume estimé à 50 000 m3 . Caractéristiques thermiques et chimiques Les eaux profondes sous Champagne Pool sont à une température d'environ 260 °C mais la température de l'eau du bassin est comprise entre 73 °C et 75 °C du fait de son refroidissement au contact de l'atmosphère. Son pH est relativement constant, de l'ordre de 5,5, du fait du tamponnement par le flux de CO2. Les gaz sont principalement du CO2, mais aussi, dans une moindre mesure, de l'azote (N2), du méthane (CH4), de l'hydrogène (H2), du sulfure d'hydrogène (H2S) et des traces d'oxygène (O2). Le fluide géothermal siliceux est saturé de métalloïdes tels que l'orpiment (As2S3) et la stibine (Sb2S3) qui précipitent et forment des dépôts orangés. Les dépôts colorés contrastent fortement avec le gris-blanc de la silice des abords de Champagne Pool. Caractéristiques biologiques Tandis que les caractéristiques géochimiques de Champagne Pool sont bien connues, seules quelques études se sont intéressées aux formes de vie microbienne qu'il pourrait accueillir. Le H2 et aussi le CO2 ou le O2 pourraient constituer des sources d'énergie permettant le développement autotrophe de micro-organismes methanogènes ou hydrogène-oxydants. Deux nouvelles bactéries et une nouvelle archaea ont été isolées à Champagne Pool. La bactérie CP.B2 nommée Venenivibrio stagnispumantis supporte de relativement fortes teneurs en composés d'arsenic et d'antimoine et représente un nouveau genre et une nouvelle espèce dans l'ordre des Aquificales. Notes et références Article connexe Liste des lacs de Nouvelle-Zélande Liens externes Ressource relative à la géographie : New Zealand Gazetteer Portail du volcanisme Portail des lacs et cours d'eau Portail de la Nouvelle-Zélande