Snake river where is it




















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Brooks, Karl Boyd. Seattle: University of Washington, Fiege, Mark. Azevedo, ed. Washington, D. Palmer, Tim. Snake River: Window to the Wes t. Petersen, Keith. Barlow who had explored that area in The group thought that Harebell Creek was the Snake River's main channel, an interpretation of the stream that was changed by the Hague surveys during the s. The Snake name comes from sign language—a serpentine movement of the hand with the index finger extended—that referred to the weaving of baskets or grass lodges of the Snake or Shoshone Indians.

The source of the Snake River was debated for a long time. The problem was to find the longest branch in the Two Ocean Plateau, which is thoroughly crisscrossed with streams.

Current maps show the head of the Snake to be about 3 miles north of Phelps Pass, at a point on the Continental Divide inside Yellowstone National Park. In , John G. White showed a photo in his hand-typed book Souvenir of Wyoming of the "true source of the Snake," writing that "it is near the Continental Divide upon two ocean plateau. More than two million wild salmon and steelhead once returned to spawn in the Snake and its tributaries each year.

Today, these species are either extinct or threatened with extinction, as the most extensive freshwater salmon habitat in the lower 48 states is upstream of the four dams on the lower Snake. They then head out to sea, and after several years return to their natal rivers to spawn, an inland journey of more than miles.

Four U. Army Corps of Engineers dams and miles of slack water reservoirs prevent salmon from migrating to and from the high-elevation spawning and rearing habitat in central Idaho, northeast Oregon, and southwest Washington. The system of dams and reservoirs kills 50 to 80 percent of juvenile salmon and steelhead as the fish make their way downstream to the ocean. Climate change is already affecting runoff patterns in the Columbia basin, causing mountain snow to melt earlier in the spring, which leads to lower summertime flows and higher summer water temperatures.

In the late nineteenth century, the military drove the Native Americans out and settlers began ranching and mining in the canyon. Today, boaters can explore archaeological sites and old homesteads, all part of the canyon's rich, colorful history. Hells Canyon is one of the most imposing river gorges in the West. Until a million years ago, the Owyhee Mountains acted as a dam between the Snake River and its current confluence with the Columbia River, creating a vast lake in what is now southwestern Idaho.

When the mountains were finally breached, the Snake roared northward, cutting a giant chasm through the volcanic rock. The resulting canyon, roughly ten miles across, is not as dramatic as the Grand Canyon. However, when the surrounding peaks are visible from the river, the sense of depth is tremendous.

The adjacent ridges average 5,' above the river.



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