NoeFlandre/osm-polygon-wikidata-only huggingface dataset:
Форт-Белнап

Форт-Белнап (англ. Fort Belknap) — индейская резервация, расположенная в центральной части штата Монтана. История Резервация была основана в 1888 году для двух индейских народов — гровантров и ассинибойнов. Своё название она получила от форта Белнапа, который в свою очередь был наречён в честь Уильяма Уорта Белнапа, американского генерала и военного министра в кабинете Улисса Гранта. Гровантры до 1861 года входили в конфедерацию черноногих и враждовали с ассинибойнами, но после одного инцидента они порвали со своими союзниками и объединились с бывшими врагами. В 1869 году гровантры и ближайшие к ним группы верхних ассинибойнов заключили мир. В марте 2012 года индейцы Форт-Белнапа от Йеллоустонского национального парка получили стадо чистокровных равнинных бизонов. Спустя столетие эти животные вновь появились на территории гровантров и ассинибойнов. В 2014 году на территории резервации начала действовать компания 4Finance US Holding Inc., оказывающая услуги по быстрому кредитованию, одним из владельцев которой является российский олигарх Олег Викторович Бойко. География Резервация расположена в северо-центральной части штата Монтана и включает часть округов Блейн и Филлипс. Общая площадь Форт-Белнап, включая трастовые земли (117,723 км²), составляет 2 638,174 км², из них 2 628,311 км² приходится на сушу и 9,863 км² — на воду. Административным центром резервации и штаб-квартирой племени является город Харлем. Демография По данным федеральной переписи населения 2010 года, в резервации проживал 2 851 человек. Согласно федеральной переписи населения 2020 года в резервации проживало 3 382 человека, насчитывалось 879 домашних хозяйств и 1 075 жилых домов. Средний доход на одно домашнее хозяйство в индейской резервации составлял 41 042 доллара США. Около 39,5 % всего населения находились за чертой бедности, в том числе 49,3 % тех, кому ещё не исполнилось 18 лет, и 18,3 % старше 65 лет. Расовый состав распределился следующим образом: белые — 132 чел., афроамериканцы — 8 чел., коренные американцы (индейцы США) — 3 142 чел., азиаты — 4 чел., океанийцы — 0 чел., представители других рас — 7 чел., представители двух или более рас — 89 человек; испаноязычные или латиноамериканцы любой расы составили 76 человек. Плотность населения составляла 1,28 чел./км². Комментарии Примечания Ссылки Official Fort Belknap Indian Community Website
Fort Missoula

Fort Missoula est un poste militaire de la United States Army établi le 25 juin 1877 le long de la Bitterroot, près de la ville de Missoula dans le Montana, afin de protéger les colons des attaques possibles d'Amérindiens. Durant la Seconde Guerre mondiale, le fort abrita un camp de prisonniers de guerre italiens et japonais. Depuis 1987, le fort est inscrit au Registre national des lieux historiques. Notes et références Annexes Bibliographie (en) Robert Walter Frazer, Forts of the West : military forts and presidios, and posts commonly called forts, west of the Mississippi River to 1898, Norman, University of Oklahoma Press, 1972 (1re éd. 1965), 246 p. (ISBN 978-0-8061-1250-3, OCLC 898938526, lire en ligne), p. 83. (en) Carol Van Valkenburg, An alien place : the Fort Missoula, Montana, Detention Camp, 1941-1944, Missoula, Pictorial Histories Pub., 2009, 130 p. (ISBN 978-0-929521-99-2, OCLC 601767928). Liens externes Ressource relative à l'architecture : Registre national des lieux historiques (en) « Historical Museum at Fort Missoula », sur fortmissoulamuseum.org. Portail du Registre national des lieux historiques Portail des forces armées des États-Unis Portail du Montana
Fort William Henry Harrison

Fort William Henry Harrison is the Montana National Guard’s training facility, located near Helena, Montana. It is also home to the Fort Harrison VA Medical Center and Montana State Veterans Cemetery, located adjacent to the military installation. History Fort William Henry Harrison (1895–1913) was authorized by a Congressional act of 12 May 1892 which was intended to establish, as a part of a greater consolidation program, concentrations of troops in a few larger installations so that smaller installations could be abandoned. The post was first named Fort Harrison after the sitting President of the United States, Benjamin Harrison, on 13 December 1892. Some years later on 16 February 1906, the name was changed to Fort William Henry Harrison because it was discovered that there had already been an Army fort named for Benjamin Harrison in Indianapolis, Indiana. Fort William Henry Harrison was first garrisoned with troops from Fort Assinniboine near Havre, Montana 23 September 1895. These initial troops were withdrawn in 1913. Fort William Henry Harrison's most famous contribution during the 20th century was its 1942 use as the organization and training area for the U. S. Army's 1st Special Service Force, a joint World War II American-Canadian light infantry brigade made famous by the 1966 book, The Devil's Brigade, co-written by Robert H. Adleman and George Walton, and The Devil's Brigade, the 1968 American war film. Current operations The post is now home of the Montana National Guard's Joint Forces Headquarters, 95th Troop Command, 208th Regional Training Institute, Training Center Headquarters, 190th Chemical Reconnaissance Detachment, Montana Medical Readiness Detachment, 83rd Civil Support Team, 1049th Fire Fighting Detachment, and I Company 145th Forward Support Element. Additionally, there is as an Army Reserve training facility and Veterans Affairs Hospital. See also List of military installations in Montana References
Brice Apartments

The Brice Apartments, located at 228 2nd Ave. E. in Kalispell, Montana, were built in 1936. They were listed on the National Register of Historic Places in 1994. They were designed by architect Fred Brinkman and built by contractor B. Brice Gilliland in the Starved Classical architecture style. Gilliland built them "for his daughter Gussie to manage for income after her retirement from teaching." The complex is "the only surviving brick apartment house built in Kalispell during the pre-World War II period." References
Fresno Dam

Fresno Dam is a dam on the Milk River, a tributary of the Missouri River, upstream of Havre, Montana. The dam is part of the Milk River Project, owned by the U.S. Bureau of Reclamation. It serves mainly to provide irrigation water and some of its capacity is also reserved for flood control. The dam was built between 1937 and 1939, and raised and overhauled in 1943 and 1951. References
Gem Glacier

This is Gem Glacier is the smallest glacier in Glacier National Park (U.S.). Located on the east (Glacier County) side of the Continental Divide arête known as the Garden Wall, the glacier is situated on the cliff face above the better known Grinnell Glacier. Gem Glacier is a hanging glacier, and drapes down from the north face of the steep arete to which it is attached. Gem Glacier is only 5 acres (0.020 km2) in area and is far below the 25 acres (0.10 km2) threshold often cited as qualifying as an active glacier. Between 1966 and 2005, Gem Glacier lost 30 percent of its acreage and Grinnell Glacier lost 40 percent. See also List of glaciers in the United States Glaciers in Glacier National Park (U.S.) References
Giant Springs

Giant Springs er en stor kilde i Cascade County i staten Montana, USA. Kilden ligger i Giant Springs State Park, lidt nordøst for byen Great Falls på den østlige bred af Missouri-floden. Kilden blev opdaget af Lewis og Clark i 1805 under deres ekspedition, der blandt andet skulle kortlægge det landområde, som USA havde købt af Frankrig i forbindelse med Louisiana-købet i 1803. Kilden, der ligger i en højde af 1.010 meter over havet, udleder omkring 7 m3 vand i sekundet eller omkring 25 millioner liter vand i timen (252 milliarder liter pr. år) fra sit udløb, der er ca. 65 meter i diameter. Dette betyder at den er klassificeret i den højeste kategori af kilder (kræver en udledning på mere end 2.800 liter i sekundet). Vandet, der er ca., 12o grader varmt kommer fra afsmeltet sne i bjergkæden Little Belt Mountains, knap 100 km fra kilden. Datering med radioistopi viser at det tager vandet ca. 2.900 år, at bevæge sig under jorden fra bjergene til kildens udspring. De vandledende lag mellem bjergene og kilden består af såkaldt Madison Kalksten. Giant Springs er dannet af en åbning i et stort grundvandsmagasin (Madison Aquifer), der ligger under 5 af USA's stater og 3 canadiske provinser. Selv om en del af vandet fra Little Belt Mountains udledes i Giant Springs, forbliver en del under jorden, og fortsætter til floder i Black Hills, Big Horn Mountains og andre steder. Selve grundvandsbassinet når overfladen i Canada. I dag aftappes en del af kildevandet og sælges som kildevand på flasker. En del af udledningen bruges til udklækning af ørredyngel og Roe River fører overskudsvandet fra kilden til Missouri-floden. Giant Springs State Park er den mest besøgte statspark i Montana. Noter Eksterne links Om Giant Springs Statepark fra Go West Travel Guide (engelsk)
Giant Springs

Giant Springs is a large first-magnitude spring located near Great Falls, Montana and is the central feature of Giant Springs State Park. Its water has a constant temperature of 54 °F (12 °C) and originates from snowmelt in the Little Belt Mountains, 60 miles (97 km) away. According to chlorofluorocarbon dating, the water takes about 3,000 years to travel underground before returning to the surface at the springs. Giant Springs is formed by an opening in a part of the Madison aquifer, a vast aquifer underlying 5 U.S. States and 3 Canadian Provinces. The conduit between the mountains and the spring is the geological stratum found in parts of the northwest United States called the Madison Limestone. Although some of the underground water from the Little Belt Mountains escapes to form Giant Springs, some stays underground and continues flowing, joining sources from losing streams in the Black Hills, Big Horn Mountains and other areas. The aquifer eventually surfaces in Canada. Giant Springs has an average discharge of 242 cubic feet (6.9 m3) of water per second or 150 million gallons per day. The spring outlet is located in Giant Springs State Park, just downstream and northeast of Great Falls, Montana on the east bank of the Missouri River. Giant Springs was first described by Lewis and Clark during their exploration of the Louisiana Purchase in 1805. Before that, the Blackfeet people utilized the springs as an easy-to-access water source in the winter. The springs were mostly ignored by settlers until 1884 when the town of Great Falls was established and the springs became the place for Sunday recreational activities. In the mid-1970s the park was established as a Montana State Park. Today, some of the spring water is bottled annually for human consumption and some of the discharge is used for a trout hatchery. The hatchery is a Montana state trout hatchery named Giant Springs Trout Hatchery and raises mostly rainbow trout. The spring serves as the headwaters of the 200-foot (61 m)-long Roe River, once listed as the shortest river in the world according to Guinness Book of World Records. The river flows into the Missouri River which is near the spring and borders its state park. See also Spring (hydrosphere) References External links Media related to Giant Springs State Park at Wikimedia Commons State of Montana: Official Giant Springs State Park website Youtube: Giant Springs 1 Youtube: Giant Springs 2 Youtube: Giant Springs 3
Giant Springs

Giant Springs är en första magnituds vattenkälla som ligger nära Great Falls, Montana och den är huvudattraktionen i Giant Springs State Park. Dess vatten som har en konstant temperatur på 12 ° C härstammar från snösmältningen i Little Belt Mountains, 97 km bort. Enligt klorfluorkarbon datering, tar det 26 år att för vattnet att förflytta sig från bergen Giant Springs har bildats genom en öppning i en del av Madison akvifern, en stor akvifer som ligger under 5 amerikanska delstater och 3 Kanadensiska provinser.Vattnet leds mellan bergen och källan av det geologiska skikt som finns i delar av nordvästra USA och som kallas Madison Limestone. Även om en del av det underjordiska vattnet från Little Belt Mountains flödar ut för att bilda Giant Springs, stannar en del under jord och fortsätter flöda, tillsammans med strömmar från Black Hills, Big Horn Mountains och andra området. Akvifern når ytan i Kanada. Källan ligger på en höjd 1.010 meter över havet. Utflödet från den är ca 6,9 kubikmeter vatten i sekunden eller omkring 25 miljoner liter vatten i timmen, Den har en diameter på ca 65 meter. Det betyder att den är klassificerad i den högsta klassen när det gäller källor (det kräver ett utflöde på mer än 2.800 liter i sekunden). Källan beskrevs första gången under Lewis och Clarks expedition 1805 då man bland annat kartlade de landområden USA köpt av Frankrike i samband med Louisianaköpet 1803. Innan dess hade svartfotsindianerna utnyttjat källan då dess vatten var lättåtkomligt på vintern. Källan ignorerades till största delen av nybyggarna fram till 1884 då staden Great Falls bildades och källan blev platsen för söndagsutflykter och rekreation. I mitten av 1970-talet blev källan och en del av omgivningarna en delstatspark (Montana State Park). På 1980-talet döptes den om till Giant Springs Heritage State Park. Idag tappas en del av källvattnet och säljs på flaska, en del av används till fiskuppfödning vid Giant Springs Trout Hatchery och Roe River för resten av vattnet till Missourifloden. Roe River hade fram till 2006, då kategorin blev avskaffad, rekordet som värdens kortaste flod (61 meter) i Guinness Rekordbok. Giant Springs Heritage State Park är den mest besökta parken i Montana. Källor Den här artikeln är helt eller delvis baserad på material från engelskspråkiga Wikipedia, tidigare version. Den här artikeln är helt eller delvis baserad på material från danskspråkiga Wikipedia, tidigare version. Noter Externa länkar Giant Springs Statepark i Go West Travel Guide Source Giant Springs Inc hemsida
Gibson Reservoir

Gibson Reservoir is a man-made body of water located just south of the Bob Marshall Wilderness, 20 miles (32 km) northwest of Augusta, Montana. It forms part of the county line between Teton and Lewis & Clark counties. The reservoir is formed by the concrete arch Gibson Dam and backs water up between a hilly pass for about 3 miles. The water in the dam is initially provided by spring snow runoff and carried there via the North Fork Sun River and the South Fork Sun River right after the two join. The reservoir is mainly used for irrigation control. References External links Gibson Reservoir Bathymetric Map Archived 2020-07-07 at the Wayback Machine Montana Fish, Wildlife & Parks
Gibson Reservoir

Gibson Reservoir est un plan d'eau artificiel situé juste au sud de Bob Marshall Wilderness, à 20 milles (32 kilomètres) au nord-ouest d'Augusta (en), dans le Montana. Il fait partie de la ligne de comté entre les comtés de Teton et Lewis & Clark. Le réservoir est formé par l'arche en béton du barrage Gibson et soutient l'eau entre un col vallonné sur environ 3 miles. L'eau du barrage est initialement fournie par le ruissellement printanier de la neige acheminée par la rivière North Fork Sun et la rivière South Fork Sun juste après la jonction des deux. Le réservoir est principalement utilisé pour le contrôle de l'irrigation . Liens externes « Gibson Reservoir », Montana Fish, Wildlife & Parks (consulté le 6 juillet 2020) « Gibson Dam », Bureau of Reclamation (consulté le 6 juillet 2020) Gibson Reservoir Bathymetric Map Montana Fish, Wildlife & Parks Notes st références Ressource relative à la géographie : Geographic Names Information System Portail des lacs et cours d'eau Portail du Montana
Glasgow station (Montana)

Glasgow station is a train station in Glasgow, Montana. The station is served by Amtrak's daily Empire Builder line. The station, platform, and parking are owned by BNSF Railway. In 2005, Glasgow saw 4.5% of Montana's twelve passenger stations’ total traffic. Bibliography Allen, W.F. (1893). Travelers Official Guide of the Railway and Steam Navigation Lines in the United States and Canada. New York, New York: National Railway Publication Company. Retrieved November 22, 2021. References External links Glasgow, MT – Amtrak Glasgow, MT – Station history at Great American Stations (Amtrak) Glasgow Amtrak Station (USA RailGuide – Train Web)
Goat Lake (Glacier County, Montana)

Goat Lake is located in Glacier National Park, in the U. S. state of Montana. Goat Lake is in a cirque below Goat Mountain which looms almost 3,400 feet (1,000 m) above the lake immediately to the northwest. The lake is a 3 miles (4.8 km) hike by trail from the Rising Sun Auto Camp. See also List of lakes in Glacier County, Montana References
Grace Lutheran Church of Barber

Grace Lutheran Church of Barber is a site on the National Register of Historic Places in Golden Valley County, Montana. The church was added to the Register on February 1, 1982. Grace Lutheran Church is located on U.S. Route 12 approximately seven miles west of the town of Ryegate. Grace Lutheran of Barber was organized in 1911. Methodists built the church at Barber in 1917. The wooden structure was shared by both Methodist and Lutheran congregations for many years. In 1927, the Lutheran congregation purchased the church and the Methodist congregation relocated to Ryegate. The church is still being used for religious services. References External links Media related to Grace Lutheran Church (Barber, Montana) at Wikimedia Commons Grace Lutheran ELCA (Montana Church Directory) Archived 2016-03-03 at the Wayback Machine
Grasshopper Glacier (Montana)

Grasshopper Glacier is in the Beartooth Mountains, Custer National Forest, Montana, U.S. The glacier is within the Absaroka-Beartooth Wilderness, a part of the Greater Yellowstone Ecosystem. Grasshopper Glacier is approximately 0.20 miles (0.32 km) long and 0.25 mi (0.40 km) wide. Starting at a point more than 11,300 feet (3,400 m) above sea level, the glacier originally was more than 5 mi (8.0 km) long but has receded significantly since first researched in the early 20th century. As of 2007, the glacier consists of several smaller glaciers, each occupying a different north-facing cirque. Grasshopper Glacier was named for the tens of millions of grasshoppers (locusts) that have been found entombed in the ice, some for hundreds and perhaps thousands of years. Many of the grasshoppers are of species that are now extinct, and their high level of preservation allowed early researchers to send some specimens to entomologists for identification. During this research it was discovered that some of the grasshoppers were of the extinct species Melanoplus spretus (Rocky Mountain locust), known to have existed at least up to the beginning of the 20th century. Known to travel in swarms numbering in the trillions in some years, it is believed that the grasshoppers found in the glacier may have been caught in severe storms and perished. Until the late 20th century, the grasshopper remains were quite common; however, lower snowfall rates since the late 1980s and higher temperatures have contributed to a higher melting rate of the glacier and many specimens decompose before they can be retrieved. Access to the glacier is difficult due to poor weather conditions and the requirement to travel via off road vehicle and then hike on foot several miles to the base of the glacier. The road is impassable for up to 10 months of the year. The Beartooth Highway (U.S. 212) is one of the closest access roads. Two smaller glaciers in the immediate region also have the same species of grasshoppers entombed in their ice; one is also named Grasshopper Glacier, the other simply Hopper Glacier. Other glaciers also bear the name for the same reason, including one in the Crazy Mountains north/northwest of the Beartooths, and Grasshopper Glacier in the Shoshone National Forest in Wyoming. See also List of glaciers in the United States References
Graves Hotel

The Graves Hotel was a historic hotel located at 106 South Central Avenue in Harlowton, Montana. A. C. Graves, a leading figure in Harlowton's early development, had the hotel built in 1909; it was one of the first businesses to be built after a fire destroyed much of downtown Harlowton in 1907. The hotel was the first sandstone building in Harlowton, though the stone eventually became a common building material; its design featured a projecting corner oriel window topped by a metal cupola. In addition to hosting visitors and railroad travelers, the hotel also served as a community meeting place and business center. The hotel was added to the National Register of Historic Places on August 6, 1980. The hotel was destroyed by a fire on February 12, 2023. References
Grinnell Lake

Grinnell Lake is located in Glacier National Park, in the U. S. state of Montana. Named after George Bird Grinnell, the lake has an opaque turquoise appearance from the rock flour (silt) which is transported to the lake from Grinnell Glacier. Grinnell Lake is accessible via the Grinnell Glacier Trail and is 3.2 miles (5.1 km) from the Many Glacier Hotel. It lies below the north face of Angel Wing. Gallery See also List of lakes in Glacier County, Montana References
Hamilton High School (Montana)

Hamilton High School is located in the Bitterroot Valley in Hamilton, Montana, United States. As of the 2019–20 school year there were 474 students in grades 9–12 with a student to teacher ratio of 14.74 to 1. Graduating classes are generally around 125 students. The school mascot is the Bronc. Hamilton High School was rebuilt in the year 2000. The old Hamilton High School now serves as the Hamilton Middle School. The 700-seat Hamilton Performing Arts Center is located in Hamilton High School. Hamilton High School classifies as a Class "A" school in the Montana High School Association. It is a member of the Southwestern "A" conference for most sports. References External links Official website localschooldirectory.com overview of Hamilton High School
Harris Glacier

Harris Glacier is located in the US state of Montana in Glacier National Park. The glacier is situated in a cirque immediately to the northeast of Parke Peak at an elevation between 7,000 ft (2,100 m) and 6,600 ft (2,000 m) above sea level. The glacier covers an area of approximately 8 acres (0.032 km2) and does not meet the threshold of 25 acres (0.10 km2) often cited as being the minimum size to qualify as an active glacier. Between 1966 and 2005, the glacier lost 77 percent of its acreage. See also List of glaciers in the United States Glaciers in Glacier National Park (U.S.) References
Lac Harrison (États-Unis)

Le lac Harrison (en anglais : Harrison Lake) est un lac américain dans le comté de Flathead, au Montana. Il est situé à 1 127 mètres d'altitude au sein du parc national de Glacier. Liens externes Ressource relative à la géographie : Geographic Names Information System (en) Lac Harrison sur Natural Atlas Portail des lacs et cours d'eau Portail du Montana
Heaven's Peak Fire Lookout

The Heaven's Peak Fire Lookout is a historic fire lookout post located in Glacier National Park, Montana, USA. It is significant as one of a chain of staffed fire lookout posts within the park. The one-story timber-construction with a flat roof was built in 1945. The flat, overhanging roof is anchored to the stone foundation with cables. The lookout was to be built in 1940 by local contractor Ole Norden as part of a Public Works Administration project. However, Norden was unable to perform the work and it was completed in 1945 under a different contract. References
Heaven's Peak Fire Lookout

Le Heaven's Peak Fire Lookout est une tour de guet du comté de Flathead, dans le Montana, aux États-Unis. Protégé au sein du parc national de Glacier, il est inscrit au Registre national des lieux historiques depuis le 19 décembre 1986. Liens externes Ressource relative à l'architecture : Registre national des lieux historiques Portail des tours de guet Portail du Registre national des lieux historiques Portail du Montana