NoeFlandre/osm-polygon-wikidata-only huggingface dataset:
Hanmer Springs Ski Area

Hanmer Springs Ski Area, located on Mount Saint Patrick, South Island, New Zealand is a club skifield 17 km (about 35 minutes' drive) from the town of Hanmer Springs. It has New Zealand's longest Poma lift at over 800m, a nutcracker rope tow and a new beginners fixed grip rope tow, giving access to trails rated as 10% beginner, 60% intermediate and 30% advanced. Elevation is 1769m at the top of the field with 52ha of ski terrain (310m vertical elevation). The 1000 metre long Poma lift was installed in 1981. It was purchased second-hand from Whakapapa Ski Field and installed by volunteers. All the holes for the towers were dug by hand. The facilities are run by the Amuri Ski Club Inc, a volunteer non-profit sports club for locals and visitors, with all proceeds from receipts being put back into upgrading facilities each year. The ski field was established in 1957. A groomer is used throughout the season which usually runs from the end of June until about mid September each year. The Hanmer Springs Ski Area was the first ski field to open in early June 2021 after a big snowfall brought snow to the field. Services Daily lessons are available and ski hire can be obtained from both the mountain and the village. A daily shuttle runs for those who are not confident on an alpine road, chains must be carried at all times and fitted when directed. References External links Official website
Hanover Hall

Hanover Hall is a community arts centre and event venue in central in Dunedin, New Zealand, opened in 2018 as home to the Dunedin Symphony Orchestra. The building was built in 1912 as the Hanover Street Baptist Church, located in Hanover Street 1 kilometre (0.62 mi) northeast of the city centre, close to the Otago Medical School. History Initially Dunedin Baptists worshipped with other Free Church groups until they established themselves in a building of their own. The church and its Sunday school were founded in 1863. A Superintendent of Otago Thomas Dick (1823–1900) was one of the initial trustees. Dr William Purdie, an Edinburgh graduate and an early and distinguished medical practitioner in Dunedin, was a founding father. The building was designed by Edmund Anscombe (1874–1948) and completed in 1912 as the first Baptist church in Dunedin. A number of notable politicians and other well-known New Zealanders have been connected with the church including Dame Silvia Cartwright, a former Governor-General of New Zealand, who spent most of her younger years in Dunedin. The congregation moved to another site in 1996. The building was unoccupied for a time before being used for a series of restaurants and bars, most latterly a nightclub called The Monkey Bar. In 2016 it was closed and purchased by a local couple for the purpose of housing the Dunedin Symphony Orchestra, and was officially reopened and renamed "Hanover Hall" in November 2018 by the Prime Minister of New Zealand, Jacinda Ardern. Features The structure is a fine design and was provided with good stained glass windows, some of which were removed when it was converted from a church to a bar. The present floor is apparently built some three feet above the original. While the overhead balcony pews appear to be intact they do not seem to be in good condition. One of the most interesting features is a pipe organ, which is believed to be only the second of its kind in New Zealand. (The other is at the Dunedin Town Hall.) The instrument has not been serviced for some time and it is uncertain whether it is in working condition. There is a bell tower, a prominent feature of the locality. The building has been classified a Category I historic place by Heritage New Zealand, with registration number 4792. References Further reading Hamilton, Derek; Hamilton, Judith (2009). Early Churches in and Around Dunedin (Paperback). Christchurch, NZ: Self-published. ISBN 978-0-473-15950-4.
Hāpuku River

Der Hāpuku River ist ein Fluss im Kaikoura District der Region Canterbury auf der Südinsel von Neuseeland. Geographie Der Hāpuku River entspringt an der Südflanke des 2608 m hohen Manakau, dem höchsten Berg der Gebirgskette der Seaward Kaikōura Range. Auf seinem 19 km langen Weg bis zum Pazifischen Ozean verläuft der Fluss in südliche bis südöstliche Richtung. Sein Mündungsgebiete liegt 10 km nordöstlich von Kaikōura. Der größte Nebenfluss des Hāpuku River ist der Puhi Puhi River, der von Norden kommend, kurz vor der Brücke des New Zealand State Highway 1 in den Hāpuku River mündet. Der jährlich Niederschlag in seinem Wassereinzugsgebiet liegt zwischen 844 mm in der Küstenregion und 1750 mm in den Bergregionen. Nutzung Dem Flussbett im unteren flacheren Teil des Flusses wird Geröll entnommen und in dem direkt am Fluss liegenden Steinberechwerk zu Schotter unterschiedlicher Größe verarbeitet. Der Fluss eignet sich begrenzt zum Angeln. Kaikōura-Erdbeben Neuseelandweite Beachtung fand der Fluss infolge des Kaikōura-Erdbeben vom 16. November 2016. Das Beben, das eine Stärke von 7,8 aufwies, führte durch einen Erdrutsch verursacht, im oberen Flussverlauf zu einem 150 m hohen Damm, der durch das aufgestaute Wasser in ersten Annahmen zu brechen drohte. Für die Anwohner und Nutzer des Flusses wurden Warnungen ausgesprochen. Doch drei Tage nach dem Beben wurde eine Entwarnung gegeben, mit dem Hinweis, dass die Situation jederzeit sich wieder ändern könne. Zum Dezember hin, hatte sich schon ein beachtlicher See gebildet, der den Verantwortlichen Sorge bereitete. Anfang Januar 2017 wurde ein Warnsystem installiert, dass bei einem Dammbruch die Anwohner und die Nutzer des State Highway 1 in dem betreffenden Bereich warnen soll. So wurde an beiden Seiten der Brücke, die den Fluss überquert, eine Warnlampe mit Hinweisschild installiert, sodass bei einer aktiven Warnlampe die Brücke nicht mehr überquert werden darf. Es wurde angenommen, dass bei einem Dammbruch die Brücke und Straße gefährdet wären und der Flut- und Geröllwelle nicht standhalten würden. Weblinks Hapuku River Catchment. Land, Air, Water Aotearoa (LAWA), abgerufen am 24. Februar 2017 (englisch). Einzelnachweise
Hāpuku River

The Hāpuku River begins in the Seaward Kaikōura Range of New Zealand and flows south-east to enter the Pacific Ocean at Hapuku, between Clarence and Kaikōura. The name comes from the Māori word hāpuku or hāpuka, a deep-water marine fish. Its main tributary is the Puhi Puhi River. The first road bridge across the Hāpuku was completed in 1915, although the approaches were a little later. The foundations were made 26 ft (7.9 m) deeper than originally specified in order to reach a solid footing. The current State Highway 1 bridge was constructed in 1983 and is 11 spans, 227 m (745 ft) long, and 8.6 m (28 ft) wide. The Main North Line railway bridge was constructed in 1940 and is 23 spans of 67 ft (20 m), with a total length of 1,500 ft (460 m). While other rivers were affected by serious flooding in 1953, the Hāpuku rose only 6.5 ft (2.0 m) at the railway bridge. Presumably this was due to the short catchment, the tectonic uplift of its headwaters and the width of the braided river bed, which is a source of railway ballast. However, an 1868 flood had more of an impact upstream, leaving a 30 ft (9.1 m) bank and a 1941 flood damaged the railway. As of March 2025, two main options for the Whale Trail cycle path from Picton to Kaikōura to cross the Hāpuku River were under evaluation: either a clip-on addition to the State Highway 1 road bridge, or a new suspension bridge. Wildlife associated with the area include black-eyed geckos, found near the headwaters of the north branch Hāpuku River, and bluff wetas. Banded dotterels breed in the Hāpuku. Introduced species include red deer, goats (kept at low levels by culling), pigs and chamois. There were two Department of Conservation huts in the valley; Hapuku Hut and Barratts Bivvy, linked by walking tracks. However, a slip triggered by the 2016 Kaikōura earthquake blocked the river, with water building up behind the slip and destroying Barratts Hut and Bivvy. Hapuka railway station was open from 13 March 1944 to 29 March 1981. A passing loop and ballast siding remain. See also List of rivers of New Zealand References External links Google Street View from SH1 bridge 1923 flood damage to road bridge 1940 views of railway bridge construction [1] [2] Aerial view of river mouth Map of 2016 earthquake slip and photo of the slip and lake
Río Hapuku

El río Hāpuku nace en la cordillera Kaikōura de Nueva Zelanda y fluye hacia el sureste para adentrarse en el Pacífico Sur en Hapuka, entre Clarence y Kaikōura.​ El nombre proviene de la palabra maorí hāpuku o hāpuka, un pez marino de aguas profundas (Polyprion oxygeneios).​ Su principal afluente es el río Puhi Puhi. El Hāpuku se salva con un puente de 460 m de 1940 con 23 vanos de 20 m en la Main North Line​ y con un puente en la SH1 de 1983 de 11 vanos, 227 m de largo y 8,6 m de ancho.​ El primer puente se terminó de construir en 1915 con cimientos de 7,9 m de profundidad, aunque los accesos fueron algo posteriores.​ Mientras que otros ríos se vieron afectados por graves inundaciones en 1953, el Hāpuku sólo se elevó 2,0 m en el puente del ferrocarril,​ probablemente debido a su corta cuenca, al levantamiento tectónico de su cabecera y a la anchura del lecho trenzado del río, que es una fuente de balasto para el ferrocarril.​ Sin embargo, una inundación de 1868 tuvo un mayor impacto río arriba, dejando una orilla de 9,1 m y una inundación de 1941 dañó el ferrocarril.​ La fauna asociada a la zona incluye salamanquesas de ojos negros, que se encuentran cerca de la cabecera del brazo norte del río Hāpuku, y bluff wetas. Las especies introducidas incluyen ciervos rojos, cabras (mantenidas en niveles bajos por el sacrificio), cerdos y gamuzas.​ Había dos refugios en el valle; Hapuku Hut y Barratts Bivvy, unidos por senderos. Sin embargo, un deslizamiento provocado por el terremoto de Kaikōura de 2016 bloqueó el río, acumulándose agua detrás del deslizamiento y destruyendo Barratts Hut y Bivvy.​ La estación de tren de Hapuka estuvo abierta desde el 13 de marzo de 1944 hasta el 29 de marzo de 1981. Se conservan un bucle de paso y un apartadero de balasto.​ Referencias Enlaces externos Vista del río desde en puente SH1 en Google Street View Vistas de 1940 de la construcción del puente ferroviario sobre el río [1] Vista aérea de la desembocadura del río
Hapuku (fleuve)

Le fleuve Hapuku (en anglais : Hapuku River) est un cours d’eau de l’île du Sud de la Nouvelle-Zélande. Toponymie Le nom vient du mot Māori Hapuku ou Hapuka, un poisson marin des profondeurs . Géographie Il prend naissance au niveau de la chaîne de Seaward Kaikoura et s’écoule vers le sud-est, pour se jeter dans l’océan Pacifique au niveau de la ville de Hapuka entre les villes de Clarence et Kaikoura . Les affluents les plus élevés prennent naissance à environ 2,000 m d’altitude. Son principal affluent est la rivière Puhi Puhi. Ponts La rivière Hapuku est franchie par un pont de 1 500 pieds, datant de 1940 portant sur 23 portées de 67 pieds sur la ligne principale nord de l'île du sud (en) et de 11 portées de 227 m de long, de 8,6 m de large en 1983 pour supporter la State Highway 1/SH1 . Le premier pont fut terminé en 1915, avec des fondations de plus de 26 pi (7,9248 m) de profondeur bien que l’approche fut un peu plus tardive . Effets des inondations Alors que d’autres rivières furent affectées d’inondations sévères en 1953, le fleuve Hapuku grimpa de seulement 6,5 pieds au niveau du pont du chemin de fer . Probablement que ceci était dû au peu de captage de l’eau, de la surélévation tectonique de ses sources et de la largeur du lit de son secteur de cours d'eau en tresses, qui est une source du ballast du chemin de fer. Toutefois en 1868, une inondation a eu plus d’impact en amont, emportant 30 pieds de la berge et une inondation de 1941 a endommagé la ligne de chemin de fer Faune La vie sauvage associée au secteur comprend la présence de Mokopirirakau kahutarae (lézards aux yeux noirs), retrouvés près de la source de la branche nord de la rivière Hapuku, et le bluff wetas (en) . Des Pluvier à double collier (Banded dotterels) nichent dans la vallée du fleuve Hapuku. Les espèces introduites comprennent le Cerf élaphe, (en anglais red deer), les chèvres (maintenues à un nombre limité par l’organisation de battues périodiques), des cochons et des chamois . Installations Il y avait deux huttes du DoC ans la vallée : Hapuku Hut et Barratts Bivvy, reliées par un chemin de randonnée . Toutefois, un glissement de terrain déclenché par le séisme de 2016 à Kaikoura bloqua la rivière, avec de l’eau s’accumulant en amont du glissement de terrain et détruisant les refuges de Barratts Hut et Bivvy. Transport La station de chemin de fer d’Hapuka fut ouverte le 13 mars 1944 et fonctionna jusqu’au 29 mars 1981, bien qu’un passage à niveau et le ballast restent en place depuis lors . Voir aussi liste des cours d'eau de la Nouvelle-Zélande Notes et références (en) Cet article est partiellement ou en totalité issu de l’article de Wikipédia en anglais intitulé « Hapuku River » (voir la liste des auteurs). liens externes 1923 flood damage to road bridge 1940 views of railway bridge construction [1] [2] Aerial view of river mouth Map of 2016 earthquake slip and photo of the slip and lake Ressource relative à la géographie : New Zealand Gazetteer Portail des lacs et cours d'eau Portail de la Nouvelle-Zélande
Wellington Opera House

The Wellington Opera House is a proscenium theatre in Wellington, New Zealand, located on Manners Street opposite Te Aro Park. History The present Opera House replaced earlier buildings on Manners Street. The Imperial Opera House opened in 1878, but burnt down a year later. Construction work on the present building began in 1911. It was named The Grand Opera House in May 1913 with a plan to open early on Boxing Night that year. The principal architect William Pitt was based in Melbourne, Australia, and much of the work was overseen by Wellington architect Albert Liddy. The opera house finally opened on Easter Saturday of 12 April 1914 to an evening performance by the American Burlesque Company, with a full seating capacity of 2141 in three levels of stalls, dress circle and gallery, including 50 box seats. The original seating upholstery was made and installed by the Wellington company Kirkcaldie & Stains, and the interior features fine plaster mouldings and an ornate dome. The building was designed with brick masonry outer walls with wooden floors and a timber-framed roof. It is registered by Heritage New Zealand as a Category 1 Historic Place. A photo hanging in the dress circle foyer alcove is of Phyllis Porter a dancer in the J.C. Williamson Peep Show Company in 1923 who died in Wellington Hospital after her costume caught fire. In 1977 it was restored with funding from the New Zealand insurance company State Insurance, and for many years it was known as the State Opera House. In the 1990s and early 2000s the building was operated by the St James Theatre Trust, which ran the nearby St James Theatre. In July 2011 Positively Wellington Venues, an integration between the Wellington Convention Centre and the St James Theatre Trust, began managing the theatre under the new name of The Opera House along with five other venues in the capital city. In October 2012 it was announced that the Opera House was an earthquake risk and would possibly have to close. By the end of 2016, funding from Wellington City Council and the Performing Arts Foundation of Wellington enabled the building to be strengthened and restored to sufficient code to continue to be open to the public. The refit also included an award-winning restoration of its original interior features, by a local architect and 14 painters and artists. The Opera House was used for the theatre scenes in Peter Jackson's 2005 film King Kong. References Kernohoran, David, Wellington's Old Buildings, Victoria University Press, 1994, ISBN 0-86473-267-8 (page 131) "Opera House". New Zealand Heritage List/Rārangi Kōrero. Heritage New Zealand. External links Media related to Opera House, Wellington at Wikimedia Commons Official website
Ópera de Wellington

La Ópera de Wellington (en inglés: Opera House, Wellington) es un teatro de proscenio en Wellington, Nueva Zelanda​​ ubicado en la calle frente al Parque de Te Aro. William Pitt, el arquitecto que lo diseño se basó en el modelo de Melbourne, Australia, y gran parte de la obra fue supervisada por el arquitecto Albert Liddy. Originalmente conocido como la "Gran ópera" (Grand Opera House), su construcción comenzó en 1911. Se trata de un edificio de ladrillo, con suelos de madera. En 1977, fue restaurado por la compañía de Seguros del Estado, y durante muchos años fue conocido como la Casa estatal de la Ópera o la ópera estatal. Hoy en día, es simplemente "La Casa de la Ópera". Véase también Cultura de Nueva Zelanda Teatro Referencias
Opera House (Wellington)

Opera House – teatr w Wellington, stolicy Nowej Zelandii, usytuowany na ulicy Manners Street, naprzeciwko parku Te Aro. Mimo tego, że szkic rysunku wykonał australijski architekt William Pitt, to z powodu trudności technicznych (Pitt mieszkał w Melbourne) prace nad projektem kończył lokalny architekt Albert Liddy. Jest to ceglany budynek z drewnianymi podłogami. Ma trzy poziomy.
Opera House (Wellington)

A Opera House é um teatro em Wellington, Nova Zelândia. Foi desenhada por William Pitt. Originalmente conhecida por Grand Opera House, a construção começou em 1911. É um edifício de tijolo, com chãos de madeira. Em 1977 foi restaurado pela State Insurance Tower, e por muitos anos ficou conhecida por State Opera House. Actualmente é simplesmente conhecida por Opera House. Ligações externas (em inglês) Sítios Históricos da Nova Zelândia - Opera House
Веллингтонский оперный театр

Веллингтонский оперный театр (англ. Opera House, Wellington) — театр с авансценой в Веллингтоне (Новая Зеландия), расположенный на улице Мэннерс-стрит. История До действующего оперного театра функционировал Императорский оперный театр, который открылся в 1878 году, но сгорел год спустя. Строительные работы над зданием оперного театра начались в 1911 году. В мае 1913 года здание получило наименование — Большой оперный театр. Главный архитектор Уильям Питт работал в Мельбурне, Австралия, и большую часть работ курировал архитектор из Веллингтона Альберт Лидди. Оперный театр открылся 12 апреля 1914 года вечерним представлением с полной вместимостью 2141 человек на трёх уровнях партера, бельэтажа и галереи, включая 50 мест в ложе. Оригинальная обивка сидений была изготовлена и установлена веллингтонской компанией Kirkcaldie & Stains, а интерьер отличается гипсовыми молдингами и богато украшенным куполом. Здание было спроектировано с кирпичными внешними стенами с деревянными полами и крышей с деревянным каркасом. Зарегистрировано Фондом по охране исторических мест Новой Зеландии как историческое место категории 1. На фотографии, висящей в нише фойе бельэтажа, запечатлена Филлис Портер, танцовщица в J.C. Williamson Peep Show Company в 1923 году, которая умерла в больнице Веллингтона после того, как её костюм загорелся. В 1977 году здание было отремонтировано при финансовой поддержке новозеландской страховой компании State Insurance, и в течение многих лет оно было известно как Государственный оперный театр. В 1990-х и начале 2000-х годов зданием управлял St James Theatre Trust. В июле 2011 года Positively Wellington Venues, объединение Wellington Convention Centre и St James Theatre Trust, начали управлять театром под новым названием The Opera House вместе с пятью другими площадками в столице. В октябре 2012 года было объявлено, что оперный театр, возможно, придётся закрыть. К концу 2016 года финансирование от городского совета Веллингтона и Фонда исполнительских искусств Веллингтона позволило укрепить здание и восстановить его до достаточного уровня, чтобы оно оставалось открытым для публики. Реконструкция также включала отмеченную наградами реставрацию его оригинальных внутренних деталей местным архитектором и 14 художниками и артистами. Оперный театр использовался для сцен в фильме Питера Джексона 2005 года «Кинг-Конг». Примечания
Teatro St. James

El Teatro St. James (en inglés:St. James Theatre; acortado a "St. James" por los lugareños) es un teatro ubicado en el corazón de la ciudad capital de Nueva Zelanda, Wellington. El teatro actual fue diseñado en 1912 por el australiano Henry Eli White. El teatro se encuentra al frente de Courtenay Place, la calle principal del distrito de entretenimiento de Wellington, frente al complejo de cines Reading. El edificio es el número 83.​​ El edificio está clasificado como "Categoría I" ("lugares de especial importancia patrimonial o excepcional valor histórico o cultural"), y lugar histórico por el New Zealand Historic Places Trust.​ Véase también Cultura de Nueva Zelanda Teatro Referencias
St. James Theatre (Wellington)

St. James Theatre, we wcześniejszych latach również Westpac St. James Theatre, później skrócone do St. James – teatr znajdujący się w Wellington, zbudowany w 1912 roku (zaprojektował go Henry Eli White) oraz otwarty 26 grudnia 1912. Teatr jest zlokalizowany w samym centrum stolicy Nowej Zelandii, w rozrywkowej dzielnicy miasta. Budynek ma numer 83. Przypisy
Harry Barker Reserve

Harry Barker Reserve is a cricket and hockey ground in Te Hāpara, Gisborne, New Zealand. It occupies 9.3 hectares and includes six cricket fields and nine hockey pitches. Establishment The Gisborne City Council purchased the Turanganui Golf Course in 1962, and developed it into a housing estate on the Pacific Coast Highway. The houses surround a substantial recreational area, which the council named the Harry Barker Reserve after a former mayor of Gisborne. Cricket Harry Barker Reserve held its first first-class match when Northern Districts played Otago in the 1974–75 Plunket Shield. As of April 2025 the ground has held 28 first-class matches, the most recent in January 2014. The first List A match there was in the 1981–82 Shell Cup when Northern Districts played Wellington. As of April 2025 the ground has held 11 List A matches, the most recent in January 2015. A three-day match between a New Zealand XI and the touring Zimbabwean team was played at the ground in January 2012. As well as the main cricket ground there are several other pitches spread out across the reserve. The Poverty Bay Cricket Association often holds an entire senior three-match round of club cricket on the reserve simultaneously. It is the headquarters and main home ground of the Association. Hockey The Harry Barker Reserve hockey stadium with blue Polytan synthetic turf was completed in 2015. On 7 April 2015 an international match was played there between the New Zealand and Argentina women's teams. New Zealand won 1–0. It was the first time an international sporting fixture had been held in Gisborne. The two teams returned for another match the next day, when Argentina beat New Zealand 7–1. References External links Harry Barker Reserve at ESPNcricinfo Harry Barker Reserve at CricketArchive Harry Barker Reserve at Gisborne District Council website Archived 2018-01-29 at the Wayback Machine