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60-744: The Loup River (pronounced /lup/) is a tributary of the Platte River , approximately 68 miles (109 km) long, in central Nebraska in the United States . The river drains a sparsely populated rural agricultural area on the eastern edge of the Great Plains southeast of the Sandhills . The name of the river means "wolf" in French , named by early French trappers after the Skidi band of

120-406: A meandering river , which has a single sinuous channel. It is also distinct from an anastomosing river , which consist of multiple interweaving semi-permanent channels which are separated by floodplain rather than channel bars; these channels may themselves be braided. The physical processes that determine whether a river will be braided or meandering are not fully understood. However, there

180-542: A meandering profile. A stream with cohesive banks that are resistant to erosion will form narrow, deep, meandering channels, whereas a stream with highly erodible banks will form wide, shallow channels, preventing the helical flow of the water necessary for meandering and resulting in the formation of braided channels. Braided rivers occur in many environments, but are most common in wide valleys associated with mountainous regions or their piedmonts or in areas of coarse-grained sediments and limited growth of vegetation near

240-772: A Spanish scout and explorer in the Southwest , was a war captain of the Spanish Indian auxiliaries. By 1714 (the same year the French explorers reached the Platte), he and a small exploration group from the south had reportedly already reached the Platte three times. He later guided the 1720 Villasur expedition to the area in a Spanish effort to stop French expansion onto the Great Plains. Naranjo and Villasur's party made

300-525: A U.S. Army officer on leave, led an expedition to the west financed by John Jacob Astor . They took wagons along the Platte, North Platte and Sweetwater River trail to the Green River in present-day Wyoming. The notable author Washington Irving wrote an account of Bonneville's explorations in the west that made him well known in the US. Following the fur traders, the major emigration trails established along

360-560: A canoe to travel far. The Platte River valley provided an easily passable wagon corridor; it sloped gradually up in height as it went almost due west from the Missouri. The Platte route had access to water, grass, buffalo and buffalo 'chips,' which the Indians and emigrants used as fuel for fires. Long Native American use had created trails on both sides of the muddy, about 1 mile (1.6 km) wide and shallow Platte River. The Platte's water

420-404: A dendritic system, or of cohesive sediments with no bedload transport. Meanders fully develop only when the river banks are sufficiently stabilized to limit lateral flow. An increase in suspended sediment relative to bedload allows the deposition of fine erosion -resistant material on the inside of a curve, which accentuated the curve and in some instances, causes a river to shift from a braided to

480-938: A number of Nebraska stakeholders embarked upon the Platte River Cooperative Hydrology Study (COHYST). Conducted with assistance from the United States Geological Survey and the Natural Resources Conservation Service , this study attempts to arrive at a better understanding of the geology and hydrology of the Platte River basin from the Colorado and Wyoming borders to Columbus, including the Loup basin. This improved understanding could be used to develop policies for management of

540-405: A previously adopted closure of part of such river basin, subbasin, or reach to the issuance of additional water well permits, or to temporarily suspend or continue in effect a temporary suspension previously adopted on the drilling of new water wells in all or part of such river basin, subbasin, or reach. Most of the Platte River basin is currently considered as overappropriated. Beginning in 2004,

600-406: A river basin, subbasin, or reach shall be deemed overappropriated if it is subject to an interstate cooperative agreement among more states and if, prior to such date, the state has declared a moratorium on the issuance of new surface water appropriations in such river, subbasin, or reach, and has requested each natural resources district jurisdiction in the affected area to close or continue in effect

660-622: A slow flowing, shallow braided stream . The North Platte River has been dammed about eight times for water storage and irrigation purposes in Wyoming and Nebraska as it flows to its confluence with the South Platte River. The upper reaches of the river in the Rockies in Colorado and Wyoming are popular for recreation rafting and lure and fly fishing for rainbow , brown , cutthroat trout and other sport fish. In western Nebraska,

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720-426: A straight channel. Also important to channel development is the proportion of suspended load sediment to bed load . An increase in suspended sediment allowed for the deposition of fine erosion -resistant material on the inside of a curve, which accentuated the curve and in some instances, caused a river to shift from a braided to a meandering profile. These experimental results were expressed in formulas relating

780-402: A variation in sediment load, provided the amount of water carried by the river is unchanged. A threshold slope was experimentally determined to be 0.016 (ft/ft) for a 0.15 cu ft/s (0.0042 m /s) stream with poorly sorted coarse sand. Any slope over this threshold created a braided stream, while any slope under the threshold created a meandering stream or – for very low slopes –

840-477: Is estimated at 3,240 cu ft/s (92 m /s). The Platte drains one of the most arid areas of the Great Plains with a flow that is considerably lower than rivers of comparable length in North America. For much of its length, it is a classic wide, muddy and shallow braided stream which in the lower reaches flows in a floodplain bordered by bluffs. During pioneer days, the common humorous description

900-424: Is joined from the north by the about 70-mile-long (110 km) Loup River about 2 miles (3 km) southeast of Columbus. During pioneer days, a Loup River ferry crossed the river. From Columbus, the Platte flows almost due east about 50 miles (80 km) past North Bend and then on to Fremont . Near Fremont, the Platte bends south and then east around the location of Omaha in a large "L" turn. Near Fremont

960-735: Is very close to the French words "rivière platte" ("flat river"), the probable origin of the name Platte River. The Platte River is formed in western Nebraska east of the city of North Platte, Nebraska by the confluence of the North Platte and the South Platte Rivers , which both arise from snowmelt in the eastern Rockies east of the Continental Divide . In central north Colorado is the North Park valley, ringed by mountains of 12,000 feet (3,700 m) height; this

1020-554: Is where the North Platte River originates. The head of the North Platte River is essentially all of Jackson County ; its boundaries are the continental divide on the west and south and the mountain drainage peaks on the east—the north boundary is the state of Wyoming. The nearest Colorado town is Walden , the county seat. The rugged Rocky Mountains Continental Divide surrounding Jackson County have at least twelve peaks over 11,000 feet (3,400 m) in height. From Jackson County,

1080-403: Is wide agreement that a river becomes braided when it carries an abundant supply of sediments. Experiments with flumes suggest that a river becomes braided when a threshold level of sediment load or slope is reached. On timescales long enough for the river to evolve, a sustained increase in sediment load will increase the bed slope of the river, so that a variation of slope is equivalent to

1140-476: The Central Flyway . Fossil evidence in the Platte River valley indicates this crane stopover has been active for over 10 million years. Since the mid-20th century, this river has shrunk significantly. This reduction in size is attributed in part to its waters being used for irrigation, and to a much greater extent to the waters diverted and used by the growing population of Colorado, which has outstripped

1200-745: The Loup Canal to hydroelectric facilities in Monroe and then in Columbus . The canal then runs into the Platte a short distance below its confluence with the Loup. Platte River The Platte is one of the most significant tributary systems in the watershed of the Missouri, draining a large portion of the central Great Plains in Nebraska and the eastern Rocky Mountains in Colorado and Wyoming . The river valley played an important role in

1260-613: The Mormon Trail north of the Platte River and had to ferry across the Elkhorn. After the Union Pacific railroad was constructed west from Omaha in 1866, it had to build a major bridge across the Elkhorn. After the confluence of the Elkhorn and the Platte River, the Platte continues southward, about 7 miles (11 km) before it turns sharply and heads almost due East for about 20 miles (32 km) before its confluence with

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1320-541: The Nebraskier , after its Oto name, meaning "flat water". The French later applied the French word plate (meaning flat, and pronounced plat , or platte ) to the river. Occupied by various Indian tribes for part of each year, the Platte River territory had been claimed by both Spanish and French explorers trying to rule the Great Plains. Spain had claimed all of the Great Plains after Coronado's 1541–42 expedition. Jose Naranjo, an African - Hopi who served as

1380-619: The Oregon boundary dispute with Britain in 1846, the conclusion of the Mexican–American War in 1848, and the California Gold Rush in 1849 and other gold and silver strikes rapidly attracted increased emigrant traffic west. The Platte River in the future state of Nebraska and the North Platte River in Wyoming typically had many channels and islands. The waterways were often too shallow, crooked, muddy and unpredictable for

1440-631: The Pawnee , whose name means "Wolf People," and who lived along its banks. The river and its tributaries, including the North Loup, Middle Loup, and South Loup, are known colloquially as "the Loups", comprising over 1800 mi (2900 km) of streams and draining approximately one-fifth of Nebraska. The river is formed in eastern Howard County , approximately 5 miles (8 km) northeast of St. Paul and 20 miles (32 km) north of Grand Island , by

1500-583: The Rakaia and Waitaki Rivers of New Zealand are not aggrading, due to retreating shorelines, but are nonetheless braided rivers. Variable discharge has also been identified as important in braided rivers, but this may be primarily due to the tendency for frequent floods to reduce bank vegetation and destabilize the banks, rather than because variable discharge is an essential part of braided river formation. Numerical models suggest that bedload transport (movement of sediment particles by rolling or bouncing along

1560-585: The interior least tern are birds using the flyway which have been classified as endangered and are protected under the Platte River Endangered Species Partnership. Common plants in the Platte River area are big and little bluestem, switch grass, and cottonwood trees. White-tail deer, many types of catfish, Canada geese, and bald eagles attract fans. The Platte River area has long supported many animals but recently, due to urbanization and farming causing loss of habitat,

1620-479: The 1540s, dramatically changed life in the Great Plains. Indian tribes could more easily follow the buffalo herds as they migrated from north to south and back. Before 1870, herds of several hundred thousand bison (buffalo) periodically migrated across the Platte in following seasonal grazing. The animals often waded or swam across the Platte. The first-known European to see the Platte was the French explorer Étienne de Veniard, sieur de Bourgmont in 1714, who named it

1680-626: The Mississippi River to the British. The Spanish took over lands west of the Mississippi River. Since there were few fur-bearing animals on the Platte of interest to the fur traders , the French and British explorers and fur trappers ignored the Platte territory for some time. During the course of the Napoleonic Wars (1803–1815), France briefly reacquired the land west of the Mississippi River from Spain. In 1804, Napoleon sold

1740-541: The Missouri River. Sarpy County is shaped like a crescent, being bounded on the east by the Missouri River, on the south and west by the Platte, and on the north by Douglas County which contains Omaha. The Platte-Missouri River confluence is about 10 miles (16 km) south of Omaha. Including the North Platte River, the Platte River stretches over 850 miles (1,400 km), with a drainage basin of about 90,000 square miles (230,000 km ). The mean annual flow

1800-561: The North Platte flows north about 200 miles (320 km) out of the Routt National Forest and North Park near what is now Walden to Casper, Wyoming . Shortly after passing Casper, the North Platte turns to the east-southeast and flows about 350 miles (560 km) to the city of North Platte, Nebraska. In Colorado and Wyoming, the North Platte is narrower and much swifter flowing than it is in Nebraska, where it becomes

1860-551: The Platte is joined from the north by the Elkhorn River . The Elkhorn, a 290-mile-long (470 km) river, originates in the eastern Sandhills of Nebraska and is one of the largest tributaries of the Platte River. The Elkhorn joins the Platte on its south-bound path just southwest of Omaha, approximately 1 mile (2 km) south and 3 miles (5 km) west of Gretna . The pioneers leaving from near Omaha (established 1854) or Council Bluffs, Iowa (established 1846) used

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1920-467: The Platte turns sharply and flows south-southeast about 10 miles (16 km) to about Waterloo, Nebraska —located about 20 miles (32 km) west of Omaha. Near Waterloo the Platte turns even more and heads almost due south for about 10 miles (16 km). About 30 miles (48 km) east-southeast of Waterloo and about 30 miles (48 km) from the Platte's confluence with the Missouri River ,

1980-592: The Platte, North Platte River and Sweetwater River was first written about after its discovery in 1811 by Wilson Price Hunt of the Astor Expedition . He was returning to the Missouri River posts from the newly established Fort Astoria on the Columbia River near the Pacific Ocean. Because few American trappers and settlers were then in the contested Oregon Territory , his trail discovery

2040-583: The South Platte River trail into Colorado. After the North Platte and the South Platte rivers join to form the Platte River, over most of its length it is a sandy, broad, shallow, braided river. Its many shallow channels and islands and ever-changing sandbars made navigation difficult; it was never used as a major water transportation route. The Platte flows in a large arc, east-southeast to near Fort Kearny and then east-northeast, across Nebraska south of Grand Island and on to Columbus . The Platte River

2100-503: The South Platte turns east and flows about 200 miles (320 km) to its confluence with the North Platte River near the city of North Platte, Nebraska. The South Platte River has been dammed about 20 times for water storage, drinking water and irrigation purposes in Colorado as it flows to its confluence with the North Platte River. The total number of dams in the South Platte drainage may exceed 1,000 as nearly all major streams have at least one dam on them. The South Platte River serves as

2160-446: The US initially had little interest in settling the land on the plains. The next "good" land was believed to be in Oregon or California , especially the coastal areas, and those were the destinations of most emigrant traffic. The Mormons settled Utah , largely due to religious persecution in eastern areas. Various gold and silver strikes attracted further emigration to nearly all western states. The Native American trail west along

2220-450: The ability of its groundwater to sustain them. Varying cultures of indigenous peoples lived intermittently along the Platte for thousands of years before European exploration. Historical tribes claimed various territories in the region. The Indian tribes typically visited different areas in different seasons, as they followed the bison herds for hunting periods. The introduction of horses, which had escaped from early Spanish explorers in

2280-437: The amount of water they carry, i.e., with " flashy " rivers, and with rivers with weak banks . Braided channels are found in a variety of environments all over the world, including gravelly mountain streams, sand bed rivers, on alluvial fans , on river deltas , and across depositional plains. A braided river consists of a network of multiple shallow channels that diverge and rejoin around ephemeral braid bars . This gives

2340-556: The area west of the Mississippi River to the US in the Louisiana Purchase ; the US roughly doubled its area at a cost of about $ 15,000,000. In 1820 the U.S. Army ordered Major Stephen H. Long to explore and map the area around the Platte. Long reported the area as a great American desert, despite its native inhabitants and wildlife, due to a lack of easily-cultivated land. As a result of his and other reports,

2400-500: The banks and riverbed of the North Platte provide a green oasis amid an otherwise semi-arid region of North America. Today, by the time the North Platte reaches Paxton, Nebraska it is much smaller due to the extensive water taken from it for irrigation. Historically, the North Platte River was up to a mile wide (1.6 km) in many places, as evidenced by the old streambed and historic written records. The South Platte River drainage includes about 28,000 square miles (73,000 km ) in

2460-508: The confluence of the North Loup and Middle Loup rivers. It flows east-northeast, past Fullerton , where it is joined from the north by the Cedar River . It continues east-northeast roughly parallel to the Platte, past Genoa , separated from the Platte by approximately 15 mi (24 km). It joins the Platte from the northwest approximately 4 miles (6 km) southeast of Columbus . A diversion dam southwest of Genoa diverts water to

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2520-643: The continental divide. It is formed by the confluence of the South Fork South Platte River and Middle Fork South Platte River , approximately 15 miles (24 km) southeast of Fairplay, Colorado . After the South and Middle fork join, the South Platte flows east-southeast till it exits Elevenmile Reservoir; it turns almost ninety degrees to skirt the west side of Pikes Peak and flows roughly east-northeast about 100 miles (160 km) through Denver and on to Greeley, Colorado . From Greeley,

2580-426: The critical slope for braiding to the discharge and grain size. The higher the discharge, the lower the critical slope, while larger grain size yields a higher critical slope. However, these give only an incomplete picture, and numerical simulations have become increasingly important for understanding braided rivers. Aggradation (net deposition of sediments) favors braided rivers, but is not essential. For example,

2640-474: The first irrigation ditch to divert water from the Platte for farming. In March 1924, the U.S. Army Air Corps conducted a three-day bombing campaign on an ice gorge that threatened bridges near the town of North Bend. The Platte is in the middle of the Central Flyway, a primary north–south corridor for migratory birds from their summer nesting grounds in the north ( Alaska and Canada ), south for

2700-649: The most northern of Spanish exploration trips into the central plains. A Pawnee and Otoe Indian attack defeated the Spanish forces; the survivors returned to Santa Fe, New Mexico , and the Spanish left the Great Plains to the American Indians. As a result of the Seven Years' War (1756–1763) (called the French and Indian War in America), the French ceded all of their lands in North America east of

2760-729: The north and south banks of the Platte and North Platte River were the Oregon (1843–1869), California (1843–1869), Mormon (1847–1869) and the Bozeman (1863–68) trails. This network of trails, sometimes called the Emigrant Trails or the Great Platte River Road , all went west along both sides of the Platte River. The route along the Platte River included all these emigration trails and was developed as an important trail route used by migrant wagon trains for westward United States expansion after 1841. The settlement of

2820-612: The north east corner of Colorado, parts of southeastern Wyoming in the vicinity of the city of Cheyenne and a small part of the southwest corner of Nebraska. The South Platte drains a large part of the Front Range mountains east of the continental divide. The part of the river labeled the South Platte is formed in Park County, Colorado , located southwest of Denver , in the South Park grassland basin and mountains east of

2880-419: The numbers have declined. Canada geese have adapted to the farm fields and scavenge a large part of their fare from unharvested grain. Many have taken up residence at suburban office parks and stopped seasonal migrations. The Platte River flowing through an arid part of the mid-west has been widely overused. The claims on the Platte River water have exceeded the supply of water in drier years. Under Nebraska law,

2940-530: The principal source of water for arid eastern Colorado. The South Platte River valley provided a major emigration path to Denver. The wagon trails followed the south side of the Platte/North Platte River. Wagon trains were ferried or waded in low water years across the swampy-bottomed South Platte River in several places to stay on the south side of the North Platte River where the trails were located. Miners who later went on to Denver followed

3000-546: The river a fancied resemblance to the interwoven strands of a braid . The braid bars, also known as channel bars, branch islands, or accreting islands, are usually unstable and may be completely covered at times of high water. The channels and braid bars are usually highly mobile, with the river layout often changing significantly during flood events. When the islets separating channels are stabilized by vegetation, so that they are more permanent features, they are sometimes called aits or eyots. A braided river differs from

3060-414: The river bottom) is essential to formation of braided rivers, with net erosion of sediments at channel divergences and net deposition at convergences. Braiding is reliably reproduced in simulations whenever there is little lateral constraint on flow and there is significant bedload transport. Braiding is not observed in simulations of the extreme cases of pure scour (no deposition taking place), which produces

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3120-732: The river system, both for human use and for the sake of the basin's endangered species. As of October 2009, the study is still ongoing. Braided stream A braided river (also called braided channel or braided stream ) consists of a network of river channels separated by small, often temporary, islands called braid bars or, in British English usage, aits or eyots . Braided streams tend to occur in rivers with high sediment loads or coarse grain sizes, and in rivers with steeper slopes than typical rivers with straight or meandering channel patterns. They are also associated with rivers with rapid and frequent variation in

3180-613: The trail. On their return trip, the fur traders carried out furs destined for eastern markets. The fur trade route was used to about 1840. By about 1832, the fur traders had improved the trail along the Platte, North Platte, and Sweetwater rivers to a rough wagon trail from the Missouri River to the Green River in Wyoming, where most of the Rocky Mountain Rendezvous were held. In 1834 Benjamin Bonneville ,

3240-549: The trails along the Platte. The Pony Express , operational from 1860–61, and the First Transcontinental Telegraph , completed in 1861, both followed the earlier emigrant trails along the Platte. The completion of the telegraph put the Pony Express out of business as it could provide much faster east–west communication. In 1866 the Union Pacific portion of the first Transcontinental Railroad

3300-518: The westward expansion of the United States, providing the route for several major emigrant trails, including the Oregon , California , Mormon and Bozeman trails. The first Europeans to see the Platte were French explorers and fur trappers about 1714; they first called it the Nebraskier (Nebraska), a transliteration of the name given by the Otoe people, meaning "flat water". This expression

3360-413: The winter, and the return in the spring. The Central Flyway bird species include trumpeter swans , tundra swans , over one million Canada geese , greater white-fronted geese , sandhill cranes, canvasback ducks and others. Other species such as bald eagles , herons and several species of ducks migrate through the Platte River area but over shorter distances. The whooping crane, piping plover , and

3420-581: Was constructed along the Platte River as it started west from Omaha. In the 20th century, the Lincoln Highway and later Interstate 80 were constructed through the Platte valley. The highways parallel the Platte and the North Platte through much of Nebraska. Many of Nebraska’s larger cities originated on or near the Platte River, as it was the first path of transportation. These include Omaha (est. 1854), Fort Kearny (est. 1848), Grand Island (est. 1857) and North Platte (est. 1869). In 1859 settlers built

3480-485: Was little used and nearly forgotten. In 1823 Jedediah Smith and several trappers "rediscovered" the route. The trail along the Platte, North Platte and Sweetwater rivers became a major route of fur traders to their summer Rocky Mountain Rendezvous . In 1824 fur trappers and traders directing mule trains carrying trade goods and supplies for the mountain men were some of the first European-American parties to use

3540-533: Was silty and bad tasting, but it was usable if no other water was available. Emigrants learned to let it sit in a bucket for an hour or so to settle most of the silt. The trail(s) through the Platte River Valley extended about 450 miles (720 km) in the present state of Nebraska. Nearly all the trails from the Missouri converged on the Platte River at or before Fort Kearny in mid-state Nebraska. Historians have estimated about 400,000 emigrants followed

3600-434: Was that the Platte was "a mile wide at the mouth, but only six inches deep." 49ers said it was "too thick to drink, too thin to plow". In western Nebraska, the banks and riverbed of the Platte provide a green oasis amid an otherwise semi-arid region of North America. The central Platte River valley is an important stopover for migratory water birds, such as the whooping crane and sandhill crane , in their yearly traversal of

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