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Marias Pass

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Marias Pass ( elevation 5,213 feet (1,589 m)) is a mountain pass in the Rocky Mountains in the western US state of Montana . Lying on the southern border of Glacier National Park , it is traversed by US Highway 2 and by the BNSF Hi-Line Subdivision . The pass is the lowest crossing of the Continental Divide between Canada and central New Mexico , and is the northernmost pass in the US open to automobile traffic year-round.

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22-1017: Marias Pass traverses the Continental Divide in the Lewis Range , along the boundary between the Lewis and Clark National Forest and the Flathead National Forest . The pass forms the southern limit of the Continental Ranges , a major grouping of the Rocky Mountains which extends as far north as McGregor Pass in the Northern Rockies of the Canadian province of British Columbia . The Great Bear Wilderness in Lewis and Clark National Forest

44-461: A gap 15 miles wide, and along which was an old Indian trail, and followed it up on the trail for thirty miles to the southwest, finding no obstruction, except from trees; and at that distance, ascending a lofty hill, saw no mountains in the direction of the stream. On each side the mountains were lofty and rugged, showing, generally, perpendicular rock from within 300 feet of their summits, which were covered with snow; and snow banks were also found on

66-665: A good and practicable pass leading from some branch of the Marias; and at this time I was sanguine that we should find there the best solution of the question of the railroad practicability of the Rocky Mountain range. Governor Stevens’ confident entry for September 5 (written years later) could have been colored by the events of a few days later: From the Little Dog, a prominent chief of the Piegan tribe [of Blackfeet ], and

88-675: A man of character and probity, I got a very particular description of the Marias Pass we were in search of. From some superstition of the Blackfeet, it has not been used for many years, but formerly it was almost the only thoroughfare made use of by the Indians in passing from one side of the mountains to the other. It is a broad, wide open valley, with scarcely a hill or obstruction on the road, excepting here and there some fallen timber. Undoubtedly feeling pressured by his duty to organize

110-556: A railroad, because its approach was broad and open, within a valley ranging from one to six miles wide, and at a gentle grade that would not require extensive excavation or rockwork. Construction of the railroad through the pass began on August 1, 1890, starting east from Fort Assinniboine toward Marias Pass. The railroad followed the Middle Fork of the Flathead River west of the Continental Divide. Stevens also discovered

132-506: A transcontinental railroad. The project was known as the Pacific Railroad Survey , and Isaac Stevens (who had just been appointed as the first governor of Washington Territory ) was chosen to lead the survey of the northernmost of the four candidate routes. Stevens’ voluminous report of that survey, published six years after the expedition, provides detailed insights. Of September 5, 1853, Stevens writes: Mr. Lander

154-691: Is 2,337 feet (712 m) lower than the south pass of Fremont . Marias Pass was finally explored and charted in December 1889 by John Frank Stevens , principal engineer of the Great Northern Railway (GN). The location of the pass had been rumored for decades beforehand, but it took Stevens and a Flathead guide named Coonsah, who had been hiding out with the Blackfoot in Browning , to discover it. The pass proved ideal for

176-487: Is south of the pass and Glacier National Park is to the north. As a low pass through the Rocky Mountains, Marias Pass was undoubtedly known to Native Americans for countless years. And while the pass was likely known by early fur trappers , its potential for use beyond foot traffic wasn’t recognized until the middle of the nineteenth century. In 1853 Congress approved funding to survey possible routes for

198-588: The Bob Marshall Wilderness is a 1,000 ft (300 m) high feature that runs for 40 miles (64 km). Major passes include Marias Pass and Logan Pass which bisects Glacier National Park east to west. Formed by the Lewis Overthrust beginning 170 million years ago, an enormous slab of Precambrian rocks 3 miles (4.8 km) thick, 50 miles (80 km) wide and 160 miles (260 km) long faulted and slid over newer rocks of

220-876: The Bob Marshall Wilderness Complex in Montana , United States. The highest peak is Mount Cleveland at 10,479 ft (3,194 m). The Lewis Range is within Waterton Lakes National Park in Canada, and in Glacier National Park and the Bob Marshall Wilderness Complex located in Flathead and Lewis and Clark National Forests in Montana. The Continental Divide spans much of the uppermost sections of

242-538: The Cretaceous period. In this relatively rare occurrence, older rocks are now positioned above newer ones. James G. Swan James Gilchrist Swan (January 11, 1818 – May 18, 1900) was an American Indian agent in what is now the U.S. state of Washington , who was known as an authority on the indigenous peoples of the Pacific Northwest Coast , an Indian artifact collector on behalf of

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264-549: The Smithsonian Institution , and for writing the first ethnography of the Makah tribal group , among whom he lived. A curious and creative man, his imaginative ambitions included a fantasy of making paper from Puget Sound seaweed. This Washington (state) biographical article is a stub . You can help Misplaced Pages by expanding it . This biographical article about an Indigenous person of North America

286-597: The Survey results, James G. Swan , early resident of Washington Territory, wrote in The Northwest Coast , In 1853, Governor Isaac I. Stevens, the first Governor of the Territory, surveyed a route for a Northern Pacific Rail-road and discovered a pass near the sources of Maria’s River suitable for a rail-road, estimated to be 2500 feet lower than the south pass of Fremont. By modern measurements, Marias Pass

308-402: The determined Isaac Stevens made one final attempt to locate the elusive pass, requesting survey party member James Doty , left behind at Fort Benton , attempt to find it from the east. Stevens dutifully reported Doty’s not-quite-successful results in the Survey report: Turning back on the 8th of June [1854], Mr. Doty retraced his route as far as the Marias, already referred to as issuing from

330-638: The newly-formed Washington Territory, Governor Stevens pressed on across the Rockies without locating Marias Pass. After crossing the Continental Divide at Cadotte Pass (elevation 6,073 feet (1,851 m)), Stevens sent the civilian engineer Abiel Tinkham back to look for the pass. But approaching from the steeper western side of the divide, Tinkham missed Marias Pass, and instead crossed at today’s Cut Bank Pass (elevation 7,850 feet (2,390 m)), roughly 12 miles (19 km) northwest of Marias Pass. Upon hearing Tinkham’s report, and realizing Tinkham’s error,

352-590: The north side of many hills. It is to be regretted that Mr. Doty did not continue on, and ascertain where the trail issued on the western side of the mountains. This is the true Marias Pass, described to me by the Little Dog at Fort Benton in September, 1853, and formerly used by the Indians in crossing the mountains. News of such a pass, even unexplored, was too important to wait for publication. Ever self-confident, Isaac Stevens must have spread word of Marias Pass by mouth: in 1857, three years before publication of

374-464: The pass across the Cascades in central Washington which bears his name . A memorial to President Theodore Roosevelt was constructed along the Continental Divide at the top of the pass. Designs for the memorial were made by Kimball , Steele & Sandham of Omaha, Nebraska. Construction began in 1930, with the original intent to produce a granite archway across the highway, and a cornerstone

396-614: The range. Major peaks in the range include Mount Cleveland (10,479 ft; 3,194 m), which is the highest peak in the range and in Glacier National Park. Other prominent peaks include Mount Stimson (10,142 ft; 3,091 m), Mount Jackson (10,052 ft; 3,064 m), Mount Siyeh (10,014 ft; 3,052 m), Going to the Sun Mountain , (9,642 ft; 2,939 m) and the isolated Chief Mountain (9,080 ft; 2,770 m). The Chinese Wall in

418-534: The summit of Marias Pass. Lewis Range The Lewis Range is a mountain range located in the Rocky Mountains of northern Montana , United States and extreme southern Alberta , Canada. It was formed as a result of the Lewis Overthrust , a geologic thrust fault resulted in the overlying of younger Cretaceous rocks by older Proterozoic rocks. The range is located within Waterton Lakes National Park in Alberta , Canada and Glacier National Park and

440-410: Was busily occupied to-day in fitting out his party for the survey of Marias Pass, in reference to which I also gained some general information that satisfied me of the existence of a pass in that quarter. Since I have given my attention to the passes of these mountains, I have been greatly impressed with the fact, from the course of the streams and the general deportment of the country, that there must be

462-632: Was later decided to build an obelisk instead of an archway; it was completed 93 years ago in 1931. Today, U.S. Route 2 uses the pass, along with the BNSF Railway , a successor to the Great Northern Railway. The railway line, which sees freight traffic, as well as Amtrak 's Empire Builder , is part of BNSF's Northern Transcon line linking Chicago and the Pacific Northwest . A statue of Stevens stands at

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484-471: Was placed to the southeast of the highway. Eleanor Roosevelt was later on hand to place a small copper box filled with a copy of the bill that appropriated funds for the memorial as well as some other documents into the cornerstone. The obelisk is sixty feet (18 m) in height and extends nineteen feet (5.8 m) into the ground. It has a tapering cement core covered on all sides with seven-inch (18 cm) slabs of Montana granite quarried near Helena . It

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