NoeFlandre/osm-polygon-wikidata-only huggingface dataset:
Ток-Джанкшен

Аэропорт Ток-Джанкшен (англ. Tok Junction Airport), (ИКАО: PFTO, FAA LID: 6K8) — государственный гражданский аэропорт, расположенный в 1,8 километрах к востоку от центрального делового района города Ток (Аляска), США. Операционная деятельность Аэропорт Ток-Джанкшен расположен на высоте 500 метров над уровнем моря и эксплуатирует одну взлётно-посадочную полосу : 7/25 размерами 765 x 15 метров с асфальтовым покрытием. За период с 31 декабря 2004 года по 31 декабря 2005 года Аэропорт Ток-Джанкшен обработал 2 700 операций взлётов и посадок самолётов (в среднем 225 операций ежемесячно), из них 56 % пришлось на рейсы аэротакси и 44 % — на авиацию общего назначения. В данный период в аэропорту базировалось 39 воздушных судов, из которых 90 % — однодвигательные самолёты, 8 % — многодвигательные и 3 % — вертолёты. Авиакомпании и пункты назначения Примечания Ссылки FAA Alaska airport diagram (GIF)
Matanuska (ledovec)

Matanuska je údolní ledovec ve státě Aljaška v USA. Se svou délkou 43 km a šířkou 6,4 km se ve Spojených státech jedná o největší ledovec dostupný automobilem. Čelo ledovce napájí řeku Matanuska. Ledovec Matanuska se nachází poblíž silnice Glenn Highway, přibližně 160 km severovýchodně od Anchorage. Ledovec se pohybuje rychlostí 30 cm/den. Kvůli tání spodního ledovce se za posledních 30 let poněkud změnilo umístění čela ledovce. Po ledovci je pojmenován trajekt MV Matanuska společnosti Alaska Marine Highway. Odkazy Reference V tomto článku byl použit překlad textu z článku Matanuska Glacier na anglické Wikipedii. Související články Matanuska Externí odkazy Obrázky, zvuky či videa k tématu Matanuska na Wikimedia Commons
Matanuska-Gletscher

Der Matanuska-Gletscher (von russisch: Матануска) ist ein 39 km langer, an seinem Ende sechs Kilometer breiter Gletscher im südlichen Alaska an der Nordflanke der Chugach Mountains, nördlich des Mount Marcus Baker. Seine Westflanke bildet der Mount Wickersham. Das Schmelzwasser des Gletschers fließt über den Matanuska River in das Cook Inlet. In den vergangenen 400 Jahren hat er kaum an Größe verloren, reichte jedoch früher bis in die Gegend des heutigen, 90 km westlich gelegenen Palmer. Die Gletscherzunge reichte bis nahe an den Glenn Highway. In den letzten 13 Jahren ist er allerdings sehr stark abgeschmolzen, sodass er heute nicht mehr bis an den Highway herankommt. Weblinks Matanuska Glacier. In: Geographic Names Information System. United States Geological Survey, United States Department of the Interior; abgerufen im 1. Januar 1 (englisch). Interaktives Panorama: Matanuska-Gletscher
Matanuska Glacier

Matanuska Glacier is a valley glacier in the US state of Alaska. At 27 miles (43 km) long by 4 miles (6.4 km) wide, it is the largest glacier accessible by car in the United States. Its terminus feeds the Matanuska River. It lies near the Glenn Highway about 100 miles (160 km) northeast of Anchorage in Glacier View. The glacier flows about 1 foot (30 cm) per day. Due to ablation of the lower glacier, as of 2007, the location of the glacier terminus has changed little over the previous three decades. Ownership and access The glacier is located in Matanuska Glacier State Recreation Site, an Alaska State Park with trails and a small campground. Although the park is public, a private entity affiliated with Cook Inlet Region, Inc. charges a toll on the only bridge connecting the park to Alaska Route 1. Name The glacier is the eponym of the Alaska Marine Highway ferry MV Matanuska. Gallery See also Matanuska Formation Glacier National Park List of glaciers References
Glaciar Matanuska

El glaciar Matanuska es un valle glaciar en los EE. UU. en el estado de Alaska. De menos de 43 kilómetros de largo por 6,4 km de ancho, es el glaciar más grande accesible en coche en los Estados Unidos. Su terminal es la fuente del río Matanuska. Se encuentra cerca de la carretera de Glenn cerca de 160 kilómetros al noreste de Anchorage. El glaciar Matanuska fluye alrededor de 1 pie (30 cm) por día. Debido a la ablación del glaciar inferior, a partir de 2007, la ubicación de la terminal del glaciar ha cambiado poco durante los últimos tres decenios.​ El glaciar es el epónimo del ferry de la Carretera Marítima de Alaska M / V Matanuska . Galería de imágenes Referencias Enlaces externos Wikimedia Commons alberga una galería multimedia sobre Glaciar Matanuska.
Glacier Matanuska

Le glacier Matanuska, en anglais Matanuska Glacier, est un glacier d'Alaska aux États-Unis, de 39 kilomètres de longueur et de 6,4 kilomètres de largeur. C'est le plus grand glacier accessible en voiture des États-Unis. Il se termine par la rivière Matanuska qui se jette dans le golfe de Cook. Il longe la Glenn Highway à 160 kilomètres au nord-est d'Anchorage. Le Matanuska est un glacier actif qui avance d'environ trente centimètres par jour. Il est accessible au public de mars à fin octobre. Notes et références (en) Cet article est partiellement ou en totalité issu de l’article de Wikipédia en anglais intitulé « Matanuska Glacier » (voir la liste des auteurs). Annexes Articles connexes Liste des glaciers de l'Alaska Liens externes Ressource relative à la géographie : Geographic Names Information System Portail de la montagne Portail des lacs et cours d'eau Portail de l’Alaska
Ghiacciaio Matanuska

Matanuska Glacier è un ghiacciaio dell'Alaska centro-meridionale che si origina nel gruppo dei monti Chugach (Chugach Mountains). Etimologia Il nome deriva da un termine russo (Matanooski o Mednoviska) derivato a sua volta dalla parola indigena 'Ch'atanhtnu Li'a' con cui ci si riferisce invece al ghiacciaio. Li'a nella lingua locale significa ghiacciaio o ghiaccio. La valle del ghiacciaio è chiamata anche Mat-Su Valley. Dati fisici Il ghiacciaio Matanuska, lungo 43 km e largo 6,4 km è il più grande ghiacciaio accessibile in auto negli Stati Uniti d'America. Si trova vicino all'autostrada Glenn (Glenn Highway), parte dell'autostrada statale Alaska Route 1 a circa 160 km a nord di Anchorage. Il ghiacciaio scorre di circa 30 cm al giorno. A causa dell'inferiore ablazione del ghiacciaio la posizione del fronte negli ultimi tre decenni è rimasta più o meno uguale. Più o meno 18.000 anni fa percorreva per tutta la lunghezza la valle Matanuska (Matanuska Valley) fino a Palmer. Circa 10.000 anni fa ha incominciato a ritirarsi fino ad arrivare nella posizione attuale. Accessi e turismo Al miglio 101 (chilometro 162,5) della Glenn Highway si trova la Matanuska Glacier State Recreation Area. Un posto di sosta e di ristoro in vista del ghiacciaio. Qualche chilometro più avanti una stradina sterrata scende la valle, attraversa il fiume Matanuska e porta ad un parcheggio privato dal quale a piedi si può raggiungere il ghiacciaio (è previsto un pedaggio). Alcune immagini Note Bibliografia Jim Dufresne, Alaska, in Lonely planet, Torino, EDT srl, Ottobre 2009, ISBN 978-88-6040-464-0. Voci correlate Autostrada Glenn Monti Chugach Matanuska Valle Matanuska Altri progetti Wikimedia Commons contiene immagini o altri file su ghiacciaio Matanuska Collegamenti esterni (EN) Ghiacciaio Matanuska, su Geographic Names Information System, USGS.
Matanuska-gletsjer

De Matanuska-gletsjer is een gletsjer in een vallei in de Amerikaanse staat Alaska. De gletsjer is 43 kilometer lang en 6,4 kilometer breed en is daarmee de langste gletsjer die bereikbaar is met de auto in de Verenigde Staten. De gletsjertong is de bron van de rivier de Matanuska. De gletsjer ligt nabij de Glenn Highway op ongeveer 160 kilometer ten noordoosten van Anchorage. De Matanuska-gletsjer stroomt met ongeveer 30 centimeter per dag. Als gevolg van ablatie van de lagere gletsjer, is de locatie van de gletsjertong licht veranderd in de afgelopen drie decennia.
Матануска (ледник)

Матануска (англ. Matanuska Glacier) — ледник на Аляске. Официальное наименование настоящего ледника дано в 1898 году Томасом Меденхоллом по наименованию одноимённой реки. Ледник расположен в долине в Чугачских горах на территории боро Матануска-Суситна. Размеры ледника — примерно 43 км X 6 км. Наблюдения последних 30 лет показали, что площадь уменьшилась. Ледник двигается со скоростью около 30 см в день. Летом температура у ледника может превышать +20 °C. Граница ледника является истоком одноимённой реки. Матануска интересен тем, что это крупнейший из ледников США, к которому можно подъехать на автомобиле. Примечания
Матануска (льодовик)

Льодовик Матануска (англ. Matanuska Glacier) — долинний льодовик в американському штаті Аляска. Маючи 46 кілометрів у довжину і 6,4 — в ширину, він є найбільшим льодовиком в Сполучених Штатах, до якого можна дістатися на авто. З його закінчення бере витоки річка Матануска. Льодовик розташований біля Шосе Ґленн приблизно 160 км на північний схід від Анкориджа. Швидкість льодовика Матануска близько 30 см на день. Через абляцію нижнього льодовика на 2007 рік місце закінчення льодовика змінилось за три останні декади. Джерела
Martin-River-Gletscher

Der Martin-River-Gletscher ist ein 45 km langer Gletscher im US-Bundesstaat Alaska, 80 km östlich von Cordova. Benannt wurde der Martin-River-Gletscher 1905 vom U.S. Geological Survey (USGS). Geografie Das 1500 m hoch gelegene Nährgebiet des Gletschers befindet sich an der Südwestflanke des Mount Hawkins, einem östlichen Nebengipfel des Mount Tom White, in den östlichen Chugach Mountains. Der im Mittel etwa 2,2 km breite Gletscher strömt in westsüdwestlicher Richtung durch die Chugach Mountains und endet auf einer Höhe von etwa 120 m. Der Hauptgletscher besitzt mehrere Tributärgletscher. Die gesamte Gletscherfläche umfasst ungefähr 250 km². Im unteren Bereich verbreitert sich der Gletscher auf eine Breite von 10 km. Unterhalb der Haupt-Gletscherzunge hat sich ein Gletscherrandsee gebildet, der den Martin River speist. Weiter südlich befindet sich mit dem Lake Charlotte ein weiterer Gletscherrandsee. Der Kushtaka-Gletscher bildet eine Gletscherzunge, die nach Süden abzweigt. Einen weiteren Abfluss bildet der Canyon Creek, der am südöstlichen Rand der Gletscherzunge gespeist wird und zum Bering River abfließt. Weblinks Martin River Glacier. In: Geographic Names Information System. United States Geological Survey, United States Department of the Interior; abgerufen im 1. Januar 1 (englisch). Einzelnachweise
Mat-Su Regional Medical Center

Mat-Su Regional Medical Center is a 125-bed general hospital in the U.S. state of Alaska. The hospital is owned by Community Health Systems (CHS). Located in the Gateway census-designated place, between Palmer and Wasilla, it is the principal hospital for the Matanuska-Susitna Borough. Owing to its location a short distance from the interchange of the Glenn and Parks Highways, Mat-Su Regional (along with the hospital on Joint Base Elmendorf-Richardson for those eligible to receive care there) serves as a principal hospital for many of the Glenn Highway communities in northern Anchorage, such as Chugiak, Eagle River, Eklutna and Peters Creek. Built at a cost of $87,700,000 to replace the aging Valley Hospital in downtown Palmer, construction on the hospital began in spring 2004. The hospital opened on January 27, 2006. The three-story, 197,690 square feet (18,366 m2) facility contains fifty medical/surgical beds and eight each of intensive care, progressive care, and obstetric beds, all in private rooms. There are four operating rooms, plus a fifth designated for Caesarean sections. The unfinished third floor provides room for a sixth operating room and 52 more general beds. Mat-Su Regional also operates a large outpatient clinic on the edge of downtown Wasilla, next to Wasilla High School. References
Matanuska–Susitna College

Matanuska–Susitna College, commonly known as Mat-Su College, is a community college in Palmer, Alaska serving the Matanuska-Susitna Valley that is part of the University of Alaska Anchorage system.. The college began in 1958 as Palmer Community College, changing its name in 1963 to correspond to the Matanuska-Susitna Borough where it is located. Total enrollment is about 1,100 students per semester. Dr. Marie Gardner is the college director. References
McCarty-Gletscher (Alaska)

Der McCarty-Gletscher ist ein etwa 12,5 km langer vom Harding Icefield gespeister Gletscher an der Ostküste der Kenai-Halbinsel in Alaska. Der McCarty-Gletscher liegt 60 km südwestlich von Seward im Kenai-Fjords-Nationalpark. Der 2 km breite Gletscher strömt in südsüdwestlicher Richtung und mündet in das Kopfende des McCarty-Fjords. Im Osten wird der Gletscher vom 1951 m hohen McCarty Peak flankiert. Der Gletscher ist im Rückzug begriffen. Benannt wurde der Gletscher vom U.S. Geological Survey im Jahr 1911 nach William McCarty, der in Seward ansässig war. Weblinks McCarty Glacier. In: Geographic Names Information System. United States Geological Survey, United States Department of the Interior; abgerufen im 1. Januar 1 (englisch). Einzelnachweise
McCarty Glacier

The McCarty Glacier is a tidewater glacier located in the Harding Icefield in the Kenai Mountains of the Kenai Peninsula, Alaska. The glacier is named for William McCarty, a former resident of Seward. The glacier has been severely affected by global warming and since the early 1900s its terminus has receded 15 km from the mouth of the bay. See also List of glaciers and icefields References External links U.S. Geological Survey Geographic Names Information System: McCarty Glacier Photo gallery including many pictures of the McCarty Glacier Excerpt from an article of the Geographical Review on the McCarty Glacier
Mendenhall Valley, Juneau

The Mendenhall Valley (colloquially The Valley) [Lingít: Áakʼw Táak] is the drainage area of the Mendenhall River in the U.S. state of Alaska. The valley contains a series of neighborhoods, comprising the largest populated place within the corporate limits of the City and Borough of Juneau, Alaska's capital. The valley was formed by Mendenhall Glacier over the course of roughly 3,000 years. It was named for the American physicist and meteorologist Thomas Corwin Mendenhall. The Mendenhall Valley begins ten miles from the downtown area, at the intersection of Egan Drive and Glacier Highway, and ends ten miles further west at the intersection of Glacier Highway and Mendenhall Loop Road at Auke Bay. The Valley comprises an area stretching from the wetlands along Fritz Cove and Auke Bay back to the Mendenhall Glacier as well as Mendenhall Lake and the Mendenhall River, which for the most part drains the Valley. The Valley forms the core of Alaska's 34th election (or state House) district, which is represented in the Alaska House of Representatives by Andi Story. Along with the rest of Juneau and adjoining communities, it is part of Senate District Q, represented in the Alaska Senate by Jesse Kiehl. There are four elementary schools (Auke Bay, Glacier Valley, Mendenhall River, and Riverbend), one middle school (Floyd Dryden), and one high school (Thunder Mountain) located in Mendenhall Valley. Most of Juneau's churches are located in the Valley. Points of interest Adair-Kennedy Memorial Park Fritz Cove Heintzleman Ridge Juneau International Airport Mendenhall Glacier Mendenhall Lake Mendenhall Mall Mendenhall River Brotherhood Bridge Mendenhall Wetlands State Game Refuge Nugget Mall Diamond park Mendenhall Glacier Visitor Center References
Mission Church (Arctic Village, Alaska)

The Mission Church is a historic Episcopal log church building on the eastern fork of the Chandalar River in Arctic Village, Alaska, inside the Arctic National Wildlife Refuge. Known also as Old Missionary Church and as Old Log Church, it was built in 1917. It was one of numerous mission churches established in Alaska by the Episcopal Church in the early 20th century. The building is significant as a mission church and for association with Reverend Albert E. Tritt. A native of Arctic Village, Tritt was converted to Christianity by gospel preaching of Episcopal missionaries at Fort Yukon, about 100 miles (160 km) to the south. He returned with a Takudh-language Bible and sought to bring others into the Episcopal church. He became a deacon of the Episcopal Church in 1925. He helped with the building of a newer church in the village in 1939. The church was added to the National Register of Historic Places in 1977. See also National Register of Historic Places listings in Yukon–Koyukuk Census Area, Alaska References
Monroe Catholic High School

Monroe Catholic High School is a private, Roman Catholic high school in Fairbanks, Alaska. It is the only Catholic high school in the Roman Catholic Diocese of Fairbanks. It is the northernmost Roman Catholic high school in the Americas. Background Monroe High School, as it was known at that time, was founded in 1955. For the first academic year, classes were held in the Immaculate Conception Church basement for the nine freshman students. The next year, another class was added when the new modern school building was opened adjacent to the grade school. Each year another class was added until the class of 1959, comprising six by that time, graduated. Notable alumni Suzanne Jackson, visual artist, poet, dancer Mike Kelly, Alaska politician Pete Kelly, Alaska politician Lisa Murkowski, U.S. Senator Kirsten Powers, journalist Stephen Sundborg, Jesuit priest, president of Seattle University External links School website References
Mulcahy Stadium

Mulcahy Stadium is a 3,500-capacity baseball park in Anchorage, Alaska. Opened in 1963, although the grass of the playing surface was seeded in 1962, it is home to two teams of the Alaska Baseball League: the Anchorage Glacier Pilots and Anchorage Bucs. In addition to the Glacier Pilots and Bucs, high school and American Legion games are played at Mulcahy. About The ballpark is named after former Alaska Railroad station auditor assistant William Mulcahy. It is located west of the Sullivan Arena across a parking lot. It has a natural grass outfield and an infield of FieldTurf. It has one of the largest capacities of any outdoor sports facility in Alaska. In 1999, five sections of aluminum bleachers were removed so that the Bucs' 3rd base clubhouse could be built. There are two rows of seating in front of the Bucs' clubhouse containing seats that were formerly used at the Oakland–Alameda County Coliseum. The OF dimensions are as follows, LF 325 CF 398 RF 325 backstop 60 The San Diego Chicken, the "Clown Prince of Baseball" Max Patkin and "Morganna the Kissing Bandit" have made appearances at Mulcahy. The annual 4th of July doubleheader between the Glacier Pilots and Bucs routinely draws crowds in excess of 4,000. On July 31, 2003, a Cessna 207 Skywagon plane carrying the pilot and three passengers made an emergency crash landing, rolling just behind the left field fence as a game between the Bucs and the Alaska Goldpanners was on at Mulcahy, and a soccer game was being played at the field behind it (Anchorage Football Stadium). Players and spectators rushed to the wreckage to help. Three aboard the plane walked away with minor injuries while one received substantial injuries. The field received a new scoreboard, new exterior fencing, new gray box seats, and the press box and grandstand were repainted for the 2007 season. In 2008, four sections of aluminum bleachers were replaced with the Home Brew Alley expansion, a wooden multi-tiered beer garden, that was installed on the first base line. After the 2009 season, the dugouts were expanded, the bullpens were relocated out-of-play, and FieldTurf was installed in the infield and foul territory. References External links Detailed Story of the 2003 Skywagon Crash - Check-Six.com
NANA Regional Corporation

NANA Regional Corporation é uma da treze empresas conhecidas como Alaska Native Regional Corporations, tendo sido criada por meio do Alaska Native Claims Settlement Act, que em 1971 pôs fim às reclamações feitas pelos povos originários do Alasca. A empresa foi fundada em 7 de junho de 1972. Sendo uma empresa ANCSA, suas ações não podem ser comercializadas, devedo ser detidas por povos originários do Alasca. Ligações externas NANA Regional Corporation
Nativity of Our Lord Chapel

The Nativity of Our Lord Chapel (Russian: Церковь Рождества Христова) is a historic Russian Orthodox church located in Church Street, Ouzinkie, Alaska. It is now under the Diocese of Alaska of the Orthodox Church in America. The current building was built in 1906 as a replacement to an older, adjacent building from 1849 or 1855 that was left to deteriorate. Its design was based on that of the 1888 Russian Orthodox church at Karluk, which itself was based upon the church at Belkofski. This church has a relatively larger onion dome, though the onion dome is still small. It was added to the National Register of Historic Places in 1980. See also National Register of Historic Places listings in Kodiak Island Borough, Alaska References
Nikolai Airport

Nikolai Airport (IATA: NIB, ICAO: PAFS, FAA LID: FSP) is a state-owned public-use airport located one nautical mile (1.85 km) northeast of the central business district of Nikolai, a city in the Yukon-Koyukuk Census Area of the U.S. state of Alaska. As per Federal Aviation Administration records, the airport had 364 passenger boardings (enplanements) in calendar year 2008, a decrease of 21% from the 459 enplanements in 2007. This airport is included in the FAA's National Plan of Integrated Airport Systems for 2009–2013, which categorized it as a general aviation facility. Although many U.S. airports use the same three-letter location identifier for the FAA and IATA, this airport is assigned FSP by the FAA and NIB by the IATA (which assigned FSP to Saint Pierre Airport in Saint Pierre and Miquelon). Facilities Nikolai Airport covers an area of 76 acres (31 ha) at an elevation of 441 feet (134 m) above mean sea level. It has one runway designated 4/22 with a gravel surface measuring 4,003 by 75 feet (1,220 x 23 m). Airlines and destinations See also List of airports in Alaska References External links FAA Terminal Procedures for FSP, effective July 9, 2026 Resources for this airport: FAA airport information for FSP AirNav airport information for PAFS ASN accident history for NIB FlightAware airport information and live flight tracker NOAA/NWS latest weather observations for PAFS SkyVector aeronautical chart for FSP
Aeroportul Nikolai

Aeroportul Nikolai (IATA: NIB, ICAO: PAFS, FAA LID: FSP) este un aeroport din Alaska, Statele Unite ale Americii ce deservește zona Nikolai⁠(d)[[Nikolai (city in Alaska, USA)|​]]. Aeroportul a fost tranzitat în 2019 de 60 de pasageri. A fost numit după zona deservită. Situat la o altitudine de 134 m, aeroportul dispune de 1 pistă. Este operat de Alaska Department of Transportation & Public Facilities⁠(d). Infrastructură Piste Aeroportul dispune de o singură pistă. Pista 04/22 are suprafața de pietriș și dimensiunile 4.021 picioare × 75 picioare. Terminale Note Vezi și
Lake Grouse

Lake Grouse (or Grouse Lake) is a small lake of glacial origin located on the Kenai Peninsula in the U.S. state of Alaska, approximately 10 km (6.2 mi) north of Seward. The name first appeared in a 1906 United States Geological Survey record reported (from a local name) by cartographer Moffit. Salvelinus malma (Dolly Varden) trout can be fished in this lake. Ice fishing is possible from December to April. References Further reading Haugen, Scott (2006). Flyfisher's Guide to Alaska. Wilderness Adventures Press. p. 65. ISBN 1-932098-02-X. External links Media related to Grouse Lake at Wikimedia Commons "Grouse Lake". alaska.org. Retrieved January 29, 2025.
Lac Grouse (Alaska)

Le Grouse Lake (ou lac Grouse) est un petit lac d'origine glaciaire situé sur la péninsule de Kenai dans l'État américain de l'Alaska, à environ 10 km au nord de Seward. Le nom apparaît pour la première fois dans un document de l'United States Geological Survey de 1906 rapporté (à partir d'un nom local) par le cartographe Moffit. La truite Salvelinus malma peut être pêchée dans ce lac. La pêche sur glace est possible de décembre à avril. Source de traduction Références Liens Ressource relative à la géographie : Geographic Names Information System Lectures complémentaires Scott Haugen, Flyfisher's Guide to Alaska, Wilderness Adventures Press, 2006, 65 p. (ISBN 1-932098-02-X) Portail des lacs et cours d'eau Portail de l’Alaska