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Located on the east side of the park, Going-to-the-Sun Road parallels the lake along its north shore. At an elevation of 4,484 feet (1,367 m), Saint Mary Lake's waters are colder and lie almost 1,500 feet (460 m) higher in elevation than Lake McDonald, the largest lake in the park, which is located on the west side of the Continental Divide.
North of Going-to-the-Sun Rd. at St. Mary Lake in Glacier National Park 48°41′39″N 113°31′13″W / 48.694167°N 113.520278°W / 48.694167; -113.520278 ( Roes Creek Campground Camptender
St. Mary or Saint Mary [2] (Blackfeet: Natoaki, "Holy Woman") is an unincorporated community on the western border of the Blackfeet Indian Reservation adjacent to Glacier National Park in Glacier County, Montana, United States.
[2] [3] [4] The view of the "St. Mary" webcam on the Glacier National Park official website is broadcast from the center and shows the westward-facing view over St. Mary Lake, which includes a distant view of Logan's Pass.
The St. Mary Utility Area Historic District comprises a support area of Glacier National Park with employee housing and support buildings in the prevailing National Park Service Rustic style. [2] The complex was built by Civilian Conservation Corps labor to replace the administrative facilities at East Glacier Ranger Station in a location more ...
The Saint Mary Ranger Station (or St. Mary) is a ranger station in Glacier National Park in the U.S. state of Montana. The log cabin was built in 1913 [2] on the east side of the park overlooking Upper Saint Mary Lake. The oldest administrative structures in the park., [3] it features an architecture that foreshadows the National Park Service ...
Going-to-the-Sun Mountain is a 9,647-foot (2,940 m) mountain peak located in Glacier National Park in the U.S. state of Montana. It rises dramatically above St. Mary Valley just north of the Going-to-the-Sun Road. [3] The mountain was named by James Willard Schultz in 1888.
The St. Mary River Formation is a geologic formation of Late Cretaceous (71.9-67 Ma [3]) age of the Western Canada Sedimentary Basin in southwestern Alberta and northwesternmost Montana. [ 4 ] [ 5 ] It was first described from outcrops along the St. Mary River by George Mercer Dawson in 1883, and it takes its name from the river.