Glacier National Park Hotels - Unofficial review
Hotels in Glacier Park are often required dor tourists who require short term accommodation. Some may want to stay at high quality hotels. Some may wqant to stay at old or new hotels. Some may want to stay well known hotels. Some may want to stay at hotels with access to entertainment and to culture.
Hotels in Glacier Park, USA, are often required for tourists who need a place to stay. Some may want to stay at high quality hotels in the region that have access to culture and to entertainment.
Glacier National Park is located in the U.S. state of Montana, bordering the Canadian provinces of Alberta and British Columbia. Glacier National Park contains two mountain ranges, sometimes referred to as the southern extension of the Canadian Rockies mountain ranges, with over 130 named lakes, more than 1,000 different species of plants and hundreds of species of animals. This vast pristine ecosystem, spread across 1,584 mi², is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 mi². The famed Going-to-the-Sun Road, a National Historic Civil Engineering Landmark, traverses through the heart of the park and crosses the Continental Divide, allowing visitors breathtaking views of the rugged Lewis and Livingston mountain ranges, as well as dense forests, alpine tundra, waterfalls and two large lakes.
The earliest
occupants with lineage to current tribes were the Salish, Flathead, Shoshone and
Cheyenne. The Blackfeet arrived around the beginning of the 18th century and soon
dominated the eastern slopes of what later became the park, as well as the Great
Plains immediately to the east. The park region provided the Blackfeet shelter
from the harsh winter winds of the plains, and supplemented their traditional
bison hunts with other game meat. Today, the Blackfeet Indian Reservation borders
the park in the east, while the Flathead Indian Reservation is located west and
south of the park. When the Blackfeet Reservation was first established in 1855
by the Lame Bull Treaty, it included the eastern area of the current park up to
the Continental Divide. To the Blackfeet, the mountains of this area, especially
Chief Mountain and the region in the southeast at Two Medicine, were considered
the Backbone of the World and were frequented during vision quests. In 1895, Chief
White Calf of the Blackfeet authorized the sale of the mountain area, some 800,000
acres, to the U.S. government for $1.5 million. This established the current boundary
between the park and the reservation.
While exploring the Marias River in 1806, the Lewis and Clark Expedition came within 50 miles of the area that is now the park. A series of explorations after 1850 helped to shape the understanding of the area that later became the park. George Bird Grinnell came to the region in the late 1880s and was so inspired by the scenery that he spent the next two decades working to establish a national park. In 1901, Grinnell wrote a description of the region, in which he referred to it as the "Crown of the Continent", and his efforts to protect the land make him the premier contributor to this cause. A few years after Grinnell first visited, Henry L. Stimson and two companions, including a Blackfeet Indian, climbed the steep east face of Chief Mountain in 1892.
In 1891, the Great Northern Railway crossed the Continental Divide at Marias Pass (5,213 ft), which is along the southern boundary of the park. In an effort to stimulate use of the railroad, the Great Northern soon advertised the splendors of the region to the public. The company lobbied the United States Congress, and in 1900, the park was designated as a forest preserve. Under the forest designation mining was still allowed, but was not commercially successful. Meanwhile, proponents of protecting the region kept up their efforts, and in 1910, under the influence of George Bird Grinnell, Henry L. Stimson and the railroad, a bill was introduced into the U.S. Congress which redesignated the region from a forest reserve to a national park. This bill was signed into law by President William Howard Taft on May 11, 1910. From May until August, the forest reserve supervisor, Fremont Nathan Haines, managed the Park's resources as the first acting superintendent. In August 1910, William Logan was appointed the Park's first superintendent.
The Great Northern Railway, under the supervision of president Louis W. Hill, built a number of hotels and chalets throughout the park in the 1910s to promote tourism. These buildings, constructed and operated by a Great Northern subsidiary called the Glacier Park Company, were modeled on Swiss architecture as part of Hill's plan to portray Glacier as "America's Switzerland". Vacationers commonly took pack trips on horseback between the lodges or utilized the seasonal stagecoach routes to gain access to the Many Glacier area in the northeast.
The chalets, built between 1910 and 1913, included Belton, St. Mary, Going-to-the-Sun, Many Glacier, Two Medicine, Sperry, Granite Park, Cut Bank, and Gunsight Lake. The railway also built Glacier Park Lodge, adjacent to the park on its east side, and the Many Glacier Hotel on the east shore of Swiftcurrent Lake. Louis Hill personally selected the sites for all of these buildings, choosing each for their dramatic scenic backdrops and views. Another developer, John Lewis, built the Lewis Glacier Hotel on Lake McDonald in 1913–1914. The Great Northern Railway bought the hotel in 1930, and it was later renamed Lake McDonald Lodge. Some of the chalets were in remote backcountry locations accessible only by trail. Today, only Sperry, Granite Park, and Belton Chalets are still in operation, while a building formerly belonging to Two Medicine Chalet is now Two Medicine Store. The surviving chalet and hotel buildings within the park are now designated as National Historic Landmarks. In total, 350 buildings and structures within the park are listed on the National Register of Historic Places, including ranger stations, backcountry patrol cabins, fire lookouts, and concession facilities.
After the park was well established and visitors began to rely more on automobiles, work was begun on the 53 mile ong Going-to-the-Sun Road, completed in 1932. Also known simply as the Sun Road, the road bisects the park and is the only route that ventures deep into the park, going over the Continental Divide at Logan Pass (6,646 feet, 2025 m) at the midway point. The Sun Road is also listed on the National Register of Historic Places, and in 1985 was designated a National Historic Civil Engineering Landmark. Another route, along the southern boundary between the park and National Forests is U.S. Route 2, which crosses the Continental Divide at Marias Pass and connects the towns of West Glacier and East Glacier. During the 1930s, the Civilian Conservation Corps assisted in the development of many of the park's trails and campgrounds. The increase in motor vehicle traffic through the park during the 1930s also resulted in the construction of new concession facilities at Swiftcurrent and Rising Sun, both designed for automobile-based tourism. These early "auto camps" are now also listed on the National Register.
The park is bordered on the north by Waterton Lakes National Park in Alberta, and the Flathead Provincial Forest and Akamina-Kishinena Provincial Park in British Columbia. To the west, the north fork of the Flathead River forms the western boundary, while its middle fork is part of the southern boundary. The Blackfeet Indian Reservation provides most of the eastern boundary, and the Lewis and Clark and the Flathead National Forests form the southern and western boundary. The remote Bob Marshall Wilderness Complex is located in the two forests immediately to the south.
The park contains a dozen large lakes and 700 smaller ones, but only 131 lakes have been named. Lake McDonald, St. Mary Lake, Bowman Lake and Kintla Lake are the four largest lakes. Numerous smaller lakes, known as tarns, are located in cirques formed by glacial erosion. Some of these lakes, like Avalanche Lake and Cracker Lake, are colored an opaque turquoise by suspended glacial silt, which also causes a number of streams to run milky white. The lack of plankton, however, lowers the rate of pollution filtration, and pollutants have a tendency to linger longer. Consequently, the lakes are considered environmental bellwethers as they can be quickly affected by even minor increases in pollutants.
Two hundred waterfalls are scattered throughout the park, however, during dryer times of the year, many of these are reduced to a trickle. The largest falls include those in the Two Medicine region, McDonald Falls in the McDonald Valley and Swiftcurrent Falls in the Many Glacier area, which is easily observable and close to the Many Glacier Hotel. One of the tallest waterfalls is Bird Woman Falls, which drops 492 feet from a hanging valley beneath the north slope of Mount Oberlin.[ Bird Woman Falls can be easily seen from the Going-to-the-Sun Road.
Montana is a state in the Western United States. The western third of the state contains numerous mountain ranges; other 'island' ranges are found in the central third of the state, for a total of 77 named ranges of the Rocky Mountains. This geographic and geographical fact is reflected in the state's name, derived from the Spanish word montaña 'mountain', from Latin. The economy is primarily based on ranching and wheat farming in the east, lumber and tourism in the west, oil and coal in the east, and hard rock mining in the west. Millions of tourists annually visit Glacier National Park, the Battle of Little Bighorn site, and three of the five entrances to Yellowstone National Park.
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