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The Snake River is a major river of the greater Pacific Northwest region in the United States. At 1,078 miles (1,735 km) long, it is the largest tributary of the Columbia River, in turn, the largest North American river that empties into the Pacific Ocean. The Snake River rises in western Wyoming, then flows through the Snake River Plain of southern Idaho, the rugged Hells Canyon on the Oregon–Idaho border and the rolling Palouse Hills of Washington, emptying into the Columbia River at the Tri-Cities in the Columbia Basin of Eastern Washington.
Castleford is a city in Twin Falls County, Idaho, United States. The population was 226 at the 2010 census. It is part of the Twin Falls, Idaho Micropolitan Statistical Area.
Hells Canyon is a ten-mile-wide (16 km) canyon in the Western United States, located along the border of eastern Oregon, a small section of eastern Washington and western Idaho. It is part of the Hells Canyon National Recreation Area which is also located in part of the Wallowa-Whitman National Forest. It is North America's deepest river gorge at 7,993 feet (2,436 m), running deeper than the Grand Canyon in Arizona.
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Carp River is a 40.2-mile-long (64.7 km) river in Chippewa and Mackinac counties in the U.S. state of Michigan. 21.7 miles (34.9 km) of the river were added to the National Wild and Scenic Rivers System in 1992.
The Jarbidge River is a 51.8-mile-long (83.4 km), high elevation river in Elko County, Nevada and Owyhee County, Idaho in the United States. The Jarbidge originates as two main forks in the Jarbidge Mountains of northeastern Nevada and then flows through basalt and rhyolite canyons on the high plateau of the Owyhee Desert before joining the Bruneau River.
Black River is a 4.2-mile-long (6.8 km) river in the southwest part of the U.S. state of Michigan that empties into Lake Michigan in South Haven at 42°24′08″N86°17′04″W, where it discharges past the South Pier Lighthouse. The river takes its name from the dark brown color of its water, which is caused by suspended sediments and organic materials picked up along its course. The river supports a variety of wildlife including trout, snapping turtles, leeches, and many other varieties of flora and fauna. The Black River watershed encompasses 287 square miles (740 km2) across two counties and 13 townships.
The Sebasticook River is a 76-mile-long (122 km) river in the central part of Maine, in the United States. From its source in Dexter, the upper "Main Stream" section flows generally west and south 30 miles (48 km) to Great Moose Lake. From the outlet of the lake in Hartland, the Sebasticook flows 41 miles (66 km) south to the Kennebec River in Winslow.
The Priest River is a 68-mile (109 km) long tributary of the Pend Oreille River in the U.S. state of Idaho. It is part of the Columbia River basin, as the Pend Oreille River is a tributary of the Columbia River. The river's drainage basin is 980 square miles (2,500 km2) in area.
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Salmon Falls Creek is a tributary of the Snake River, flowing from northern Nevada into Idaho in the United States. Formed in high mountains at the northern edge of the Great Basin, Salmon Falls Creek flows northwards 121 miles (195 km), draining an arid and mountainous basin of 2,103 square miles (5,450 km2). The Salmon Falls Creek valley served as a trade route between the Native American groups of the Snake River Plain and Great Basin. Today, most of its water is used for irrigation.
Fall River rises on the Madison and Pitchstone Plateaus in the southwest corner of Yellowstone National Park, Wyoming and flows approximately 64 miles (103 km) to its confluence with the Henrys Fork of the Snake River near Ashton, Idaho. Historically, the river was referred to as the Middle Fork of the Snake River or as Fall River or the Falls River by trappers and prospectors as early as the 1830s. It was officially named the Falls River by 1872 Hayden Geological Survey, but was always called Fall River by the locals and so the U.S. Board on Geographic Names changed the official name to Fall River in 1997 at the request of Idaho authorities. The river is home to numerous waterfalls and cascades in its upper reaches.
Lower Salmon Falls Dam is a concrete gravity-type hydroelectric dam on the Lower Salmon Falls of the Snake River, in the U.S. state of Idaho. The dam is located 5 miles downstream from Upper Salmon Falls, between Gooding County and Twin Falls County, Idaho.
References
- ↑ U.S. Geological Survey Geographic Names Information System: Upper Salmon Falls
- ↑ Commission, United States Federal Energy Regulatory (2004). Federal Energy Regulatory Commission Reports. Vol. 108. Federal Energy Regulatory Commission. pp. 61–642.
- ↑ Camp, Charles L.; Clyman, James (1925-12-01). "James Clyman: His Diaries and Reminiscences (Continued)". California Historical Society Quarterly. 4 (4): 307–360. doi:10.2307/25177782. ISSN 0008-1175. JSTOR 25177782.
- ↑ U.S. Geological Survey Geographic Names Information System: Upper Salmon Falls
- ↑ Commission, United States Fish (1896). Bulletin of the United States Fish Commission. U.S. Government Printing Office. p. 258.
- ↑ U.S. Geological Survey Geographic Names Information System: Lower Salmon Falls
- ↑ U.S. Geological Survey Geographic Names Information System: Salmon Falls
- ↑ U.S. Geological Survey Geographic Names Information System: Lower Salmon Falls Dam
- ↑ Waterfalls in Idaho from www.ultimateidaho.com accessed on September 26, 2013
- ↑ Lower Salmon Falls from worldwaterfalldatabase.com accessed on September 26, 2013
- ↑ "Salmon Falls". Geographic Names Information System. United States Geological Survey. Retrieved 2013-12-30.
- ↑ "Upper Salmon Falls". Geographic Names Information System. United States Geological Survey. Retrieved 2013-12-30.
- ↑ "Lower Salmon Falls". Geographic Names Information System. United States Geological Survey. Retrieved 2013-12-30.
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