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161-521: The aqueduct is the sole water supply for about 1.4 million people in the East Bay. Under present water rights agreements, EBMUD can withdraw up to 325 million gallons (1,230,000 m) per day, or 364,000 acre-feet (0.449 km) per year, from the Mokelumne River. In addition, up to 98 million gallons (371,000 m) per day or 110,000 acre-feet (0.14 km) per year can be supplied via a branch from

322-414: A breach may experience flooding similar to a natural event, while damage near a breach can be catastrophic, including carving out deep holes and channels in the nearby landscape. Under natural conditions, floodwaters return quickly to the river channel as water-levels drop. During a levee breach, water pours out into the floodplain and moves down-slope where it is blocked from return to the river. Flooding

483-589: A canyon for about 60 miles (97 km), past Dunsmuir and Castella , before emptying into Shasta Lake near Lakehead in Shasta County . The McCloud River rises on the east slope of Mount Shasta and flows south for 77 miles (124 km) through the southern Cascade Range , roughly parallel to the Upper Sacramento, eventually to reach the McCloud Arm of Shasta Lake. The Pit River, by far

644-574: A chance to return for spawning. According to UC Davis Center for Watershed Sciences these rice fields adjacent to the Sacramento River will serve as potential nurseries for salmon. UC Davis also concluded from past experimental releases of salmon, that the Yolo Bypass floodway could have up to 57,000 acres of a productive breeding habitat with almost no cost to farmers. The Nigiri project has demonstrated off-season agriculture fields such as

805-539: A combined storage capacity of 155,150 acre-feet (0.19137 km). The water is treated at the San Pablo, Sobrante and Upper San Leandro Treatment Plants before passing through the Claremont Tunnel, which emerges on the western side of the range between Berkeley and Oakland . Water not immediately put into the municipal system is stored in the reservoirs for use in times of low delivery or drought. Most of

966-612: A distance of some 610 km (380 mi). The scope and scale of the Mississippi levees has often been compared to the Great Wall of China . The United States Army Corps of Engineers (USACE) recommends and supports cellular confinement technology (geocells) as a best management practice. Particular attention is given to the matter of surface erosion, overtopping prevention and protection of levee crest and downstream slope. Reinforcement with geocells provides tensile force to

1127-553: A dyke may be a field wall, generally made with dry stone . The main purpose of artificial levees is to prevent flooding of the adjoining countryside and to slow natural course changes in a waterway to provide reliable shipping lanes for maritime commerce over time; they also confine the flow of the river, resulting in higher and faster water flow. Levees can be mainly found along the sea, where dunes are not strong enough, along rivers for protection against high floods, along lakes or along polders . Furthermore, levees have been built for

1288-677: A flood emergency. Some of the earliest levees were constructed by the Indus Valley civilization (in Pakistan and North India from c.  2600 BCE ) on which the agrarian life of the Harappan peoples depended. Levees were also constructed over 3,000 years ago in ancient Egypt , where a system of levees was built along the left bank of the River Nile for more than 1,000 kilometers (600 miles), stretching from modern Aswan to

1449-629: A great network of pumps and canals that would take water from the Sacramento River in the north, and transport it to drought-prone central and southern California, especially the San Joaquin Valley. The Sacramento River basin receives "two-thirds to three-quarters of northern California's precipitation though it has only one-third to one-quarter of the land. The San Joaquin River watershed occupies two-thirds to three-quarters of northern California's land, but only collects one-third to one-quarter of

1610-419: A height of 400 feet (120 m). This would expand the reservoir surface by 33 to 46 feet (10 to 14 m). The enlarged reservoir would cover 3,400 acres (1,400 ha), an increase of 62 percent, and the capacity would be about 300,000 acre-feet (0.37 km), a roughly 50 percent increase. It would allow for more water to be provided during the dry season that would otherwise have been spilled over

1771-444: A high suspended sediment fraction and thus are intimately associated with meandering channels, which also are more likely to occur where a river carries large fractions of suspended sediment. For similar reasons, they are also common in tidal creeks, where tides bring in large amounts of coastal silts and muds. High spring tides will cause flooding, and result in the building up of levees. Both natural and man-made levees can fail in

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1932-413: A large portion of the habitat currently used by migrating birds. Native bird populations have been declining steadily since the 19th century. Species that were once common but now are endangered or gone include the southwestern willow flycatcher , western yellow-billed cuckoo , least Bell's vireo , and warbling vireo . Another reason for dropping numbers are the introduction of non-native species, such as

2093-578: A large proportion of their population within a few decades of the arrival of Sutter and the following settlers, the start of the gold rush , not to mention the numerous battles fought between the settlers and native bands as well as the forced relocation of some of the tribes to Indian reservations in several places scattered around the Sacramento Valley, mainly in the Coast Ranges. In the early 1850s, several treaties were signed between

2254-428: A number of ways. Factors that cause levee failure include overtopping, erosion, structural failures, and levee saturation. The most frequent (and dangerous) is a levee breach . Here, a part of the levee actually breaks or is eroded away, leaving a large opening for water to flood land otherwise protected by the levee. A breach can be a sudden or gradual failure, caused either by surface erosion or by subsurface weakness in

2415-659: A part in the formation of the 300-mile (480 km) Monterey Submarine Canyon when sea levels were lower during the Ice Ages. The Monterey Bay outlet of the Sacramento and San Joaquin rivers was blocked off by uplift about 2 million years ago, and runoff from the Sierra began to transform the Central Valley into a gigantic lake, called Lake Clyde . This lake stretched 500 miles (800 km) north to south and

2576-403: A plethora of massive changes to the environment beginning in the 20th century. An early project was undertaken to raise the entire city of Sacramento about 11 feet (3.4 m) above its original elevation. This was followed by much bigger engineering projects to control and store the floodwaters of the Sacramento River; the building of these public works would radically transform the river during

2737-412: A shorter route to the ocean and begin building a new delta. Wave action and ocean currents redistribute some of the sediment to build beaches along the coast. When levees are constructed all the way to the ocean, sediments from flooding events are cut off, the river never migrates, and elevated river velocity delivers sediment to deep water where wave action and ocean currents cannot redistribute. Instead of

2898-421: A shorter time interval means higher river stage (height). As more levees are built upstream, the recurrence interval for high-water events in the river increases, often requiring increases in levee height. During natural flooding, water spilling over banks rises slowly. When a levee fails, a wall of water held back by the levee suddenly pours out over the landscape, much like a dam break. Impacted areas far from

3059-535: A single pipeline, were completed. The first deliveries to the Bay Area were made on June 23, 1929. At the time of completion, Pardee Dam was the tallest in the world (this record was surpassed one year later by Diablo Dam in Washington State). In 1949, a second pipeline was built and in 1963 the third pipeline was constructed, bringing the aqueduct to its present capacity. In 1964, the second major dam of

3220-626: A total of over 3,000 cubic feet per second (85 m /s) of water to irrigate some 150,000 acres (610 km ). In 1960, construction began on the State Water Project, whose primary purpose was to deliver water to Los Angeles and the San Francisco Bay Area. Oroville Dam – the tallest dam in the U.S. – was built on the Sacramento's largest tributary, the Feather River. A series of channels were enlarged in

3381-480: A turning point in the history of the Sacramento Valley, and California as a whole. In 1841, Sutter and his men built a fortress at the confluence of the Sacramento and American Rivers and the Mexican government granted him almost 50,000 acres (200 km ) of land surrounding the two rivers. Naming it New Helvetia, he created an agricultural empire in the lower Sacramento Valley, attracting several hundred settlers to

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3542-472: A vast tidal estuary and inverted river delta of over 1,000 square miles (2,600 km ) which receives the entire run-off of the Central Valley, a region covering a third of California. The Sacramento is by far the largest contributor of fresh water to the Delta; in an average year, it accounts for more than 80 percent of the fresh water inflow. At Walnut Grove , the manmade Delta Cross Channel connects

3703-537: Is electrical resistivity tomography (ERT). This non-destructive geophysical method can detect in advance critical saturation areas in embankments. ERT can thus be used in monitoring of seepage phenomena in earth structures and act as an early warning system, e.g., in critical parts of levees or embankments. Large scale structures designed to modify natural processes inevitably have some drawbacks or negative impacts. Levees interrupt floodplain ecosystems that developed under conditions of seasonal flooding. In many cases,

3864-424: Is 43 miles (69 km) long and is maintained to a depth of 30 feet (9.1 m). The Sacramento River and its drainage basin once supported extensive riparian habitat and marshes , in both the Sacramento Valley and the Delta, home to a diverse array of flora and fauna. Due to the reclamation of land for agriculture and the regulation of seasonal flooding, the amount of water-based habitat declined greatly during

4025-546: Is below mean sea level. These typically man-made hydraulic structures are situated to protect against erosion. They are typically placed in alluvial rivers perpendicular, or at an angle, to the bank of the channel or the revetment , and are used widely along coastlines. There are two common types of spur dyke, permeable and impermeable, depending on the materials used to construct them. Natural levees commonly form around lowland rivers and creeks without human intervention. They are elongated ridges of mud and/or silt that form on

4186-420: Is important in order to design stable levee and floodwalls . There have been numerous studies to investigate the erodibility of soils. Briaud et al. (2008) used Erosion Function Apparatus (EFA) test to measure the erodibility of the soils and afterwards by using Chen 3D software, numerical simulations were performed on the levee to find out the velocity vectors in the overtopping water and the generated scour when

4347-508: Is located in a seismically active zone and is considered vulnerable to earthquakes, especially the 15-mile (24 km) stretch where it crosses the Sacramento–San Joaquin Delta, where an earthquake or storm-induced levee failure could damage the pipelines or any of three major river crossings here. A large earthquake (100 year return period or more) could put the aqueduct out of service from 18 months to three years, depending on

4508-451: Is permanently diverted through the gap. Sometimes levees are said to fail when water overtops the crest of the levee. This will cause flooding on the floodplains, but because it does not damage the levee, it has fewer consequences for future flooding. Among various failure mechanisms that cause levee breaches, soil erosion is found to be one of the most important factors. Predicting soil erosion and scour generation when overtopping happens

4669-573: Is prolonged over such areas, waiting for floodwater to slowly infiltrate and evaporate. Natural flooding adds a layer of sediment to the floodplain. The added weight of such layers over many centuries makes the crust sink deeper into the mantle , much like a floating block of wood is pushed deeper into the water if another board is added on top. The momentum of downward movement does not immediately stop when new sediment layers stop being added, resulting in subsidence (sinking of land surface). In coastal areas, this results in land dipping below sea level,

4830-532: Is the only part of the Sacramento River basin extending into another state. Unlike most California rivers, the Pit and the McCloud Rivers are predominantly spring-fed, ensuring a large and consistent flow in even the driest of summers. At the lower end of Shasta Lake is Shasta Dam , which impounds the Sacramento River for flood control, irrigation and hydropower generation. Before the construction of Shasta Dam,

4991-459: Is used heavily for irrigation and serves much of Central and Southern California through the canals of giant state and federal water projects. While it is now providing water to over half of California's population and supporting the most productive agricultural area in the nation, these changes have left the Sacramento greatly modified from its natural state and have caused the decline of its once-abundant fisheries. The Sacramento River originates in

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5152-452: Is used to flood the fields for most of this experiment adjacent to the Sacramento River. The water is eventually flushed back into the Delta ecosystem through agricultural canals. Levee A levee ( / ˈ l ɛ v i / or / ˈ l ɛ v eɪ / ), dike ( American English ), dyke ( British English ; see spelling differences ), embankment , floodbank , or stop bank is an elevated ridge , natural or artificial, alongside

5313-490: The Blessed Sacrament ". In the following years, two more Spanish expeditions traversed the lower part of the river, the last one in 1817. The next visitors were Hudson's Bay Company (HBC) fur trappers exploring southwards from the disputed Oregon Country , starting in the 1820s. The first organized expedition, led by Peter Skene Ogden , arrived in the area of Mount Shasta in 1826. By this time, California

5474-624: The California Coast Ranges , enclosing the Sacramento Valley and forcing the streams within to flow south instead of west, forming the ancestral Sacramento River. (The Klamath Mountains , which enclose the northwest part of the Sacramento Basin, were formed in the same way but are much older, dating back 7.5 million years.) It is possible that the river once had its outlet in Monterey Bay , and may have played

5635-677: The Carquinez Strait into San Pablo Bay and San Francisco Bay , joining the Pacific at the Golden Gate . Following the Columbia River , the Sacramento is the largest river by discharge on the Pacific coast of the continental United States. The natural runoff of the river is 22 million acre-feet (27 km ) per year, or about 30,000 cubic feet per second (850 m /s). Before dams were built on its tributaries,

5796-794: The Central Valley along the Calaveras River before crossing the Sacramento–San Joaquin River Delta . Near Lodi , the aqueduct is joined by an extension of the Folsom South Canal, which supplements the Mokelumne River supply. Once the water reaches the Berkeley Hills above the East Bay, it is channeled into a complex distribution system consisting of six terminal reservoirs ( Briones , Chabot , Lafayette , San Pablo and Upper San Leandro) with

5957-603: The Gulf of California just south of the US-Mexico border near the southeast part of the state, is far larger than the Sacramento in terms of length and drainage area but has a slightly smaller flow. The Sacramento, when combined with the Pit, is also one of the longest rivers in the United States entirely within one state—after Alaska 's Kuskokwim and Texas ' Trinity . The major drainage basins bordering that of

6118-535: The Indus Valley , ancient Egypt, Mesopotamia and China all built levees. Today, levees can be found around the world, and failures of levees due to erosion or other causes can be major disasters, such as the catastrophic 2005 levee failures in Greater New Orleans that occurred as a result of Hurricane Katrina . Speakers of American English use the word levee , from the French word levée (from

6279-716: The Klamath Diversion , proposed to send the entire flow of the Klamath River into the Sacramento River through a system of large reservoirs, canals, pumping stations and tunnels. Similarly, the Dos Rios Dam project would have diverted a considerable portion of the Eel River to the Sacramento. Both projects were defeated by local resistance, opposition from environmentalists, as well as the high capital cost. The Sacramento River Deep Water Ship Channel

6440-525: The Nile Delta on the shores of the Mediterranean . The Mesopotamian civilizations and ancient China also built large levee systems. Because a levee is only as strong as its weakest point, the height and standards of construction have to be consistent along its length. Some authorities have argued that this requires a strong governing authority to guide the work and may have been a catalyst for

6601-679: The Sacramento River . However, this supply is expected only to be used in the driest 35% of years. In the early 20th century, due to a lack of reliable local water, Bay Area cities began to look to rivers in the Sierra Nevada , about 100 miles (160 km) east, as a potential new source. Although the city of San Francisco was already extending an aqueduct to the Tuolumne River , East Bay communities wanted to build an independent water system, fearing future " hegemony " of

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6762-730: The Shasta , Modoc , and Achomawi /Pit River Tribes of the volcanic plateaus in the north; the Wintu and Hupa in the northern Klamath and Trinity mountains; the Nomlaki , Yuki , Patwin , and Pomo of the Coast Ranges; the Yana , Atsugewi , Maidu , Konkow , and Nisenan in the Sierra and their western foothills; and the Miwok in the south. Most of the Sacramento Valley's native peoples relied on hunting, gathering and fishing, although agriculture

6923-533: The Snake – Columbia River systems; geologic evidence indicates that the two were connected by a series of wetlands and channels about 4-5 million years ago. Located along the Pacific Flyway , the sprawling wetlands of the Sacramento Valley are an important stop for migratory birds; however, only a fraction of the historic wetlands remain. Seasonally flooded rice paddies in the Sacramento Valley comprise

7084-548: The Tehachapi Mountains via four large pumping stations. The project irrigates 750,000 acres (300,000 ha) of land in the San Joaquin Valley and serves 22 million people in Central and Southern California. Over the years, several other plans materialized to divert rivers from California's North Coast into the Sacramento watershed, as future demand was projected to exceed supply. The only one to be built

7245-457: The bank . It closely parallels the English verb to dig . In Anglo-Saxon , the word dic already existed and was pronounced as dick in northern England and as ditch in the south. Similar to Dutch, the English origins of the word lie in digging a trench and forming the upcast soil into a bank alongside it. This practice has meant that the name may be given to either the excavation or to

7406-631: The banks of a river , often intended to protect against flooding of the area adjoining the river. It is usually earthen and often runs parallel to the course of a river in its floodplain or along low-lying coastlines. Naturally occuring levees form on river floodplains following flooding, where sediment and alluvium is deposited and settles, forming a ridge and increasing the river channel's capacity. Alternatively, levees can be artificially constructed from fill , designed to regulate water levels. In some circumstances, artificial levees can be environmentally damaging . Ancient civilizations in

7567-791: The catchwater drain , Car Dyke, to the South Forty Foot Drain in Lincolnshire (TF1427). The Weir Dike is a soak dike in Bourne North Fen , near Twenty and alongside the River Glen , Lincolnshire . In the Norfolk and Suffolk Broads , a dyke may be a drainage ditch or a narrow artificial channel off a river or broad for access or mooring, some longer dykes being named, e.g., Candle Dyke. In parts of Britain , particularly Scotland and Northern England ,

7728-437: The foothill yellow-legged frog and western spadefoot are listed as endangered species. Riparian and wetlands areas along the Sacramento once totaled more than 500,000 acres (2,000 km ); today only about 10,000 acres (40 km ) remains. Much of this consists of restored stretches and artificially constructed wetlands. Levee construction has prevented the river from changing course during winter and spring floods, which

7889-611: The 19th century, gold was discovered on a tributary of the Sacramento River, starting the California Gold Rush and an enormous population influx to the state. Overland trails such as the California Trail and Siskiyou Trail guided hundreds of thousands of people to the gold fields. By the late part of the century mining had ceased to be a major part of the economy, and many immigrants turned to farming and ranching. Many populous communities were established along

8050-417: The 20th century. From the late 19th century through the 20th century, California experienced an economic boom that led to the rapid expansion of both agriculture and urban areas. The Central Valley was becoming a heavily developed irrigation farming region, and cities along the state's Pacific coast and the Sacramento and San Joaquin rivers were growing rapidly, requiring river control to prevent flooding on

8211-419: The 20th century. Other human impacts include the heavy water consumption for agriculture and urban areas, and pollution caused by pesticides , nitrates , mine tailings , acid mine drainage and urban runoff . The Sacramento supports 40–60 species of fish, and 218 species of birds. The basin also has a number of endemic amphibian and fish species. Many Sacramento River fish species are similar to those in

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8372-672: The Cascades; its headwaters rise on the western extreme of the Basin and Range Province , east of major Cascade volcanoes such as Mount Shasta and Lassen Peak . The other two are the Klamath River and Columbia River . By discharge, it is the second-largest contiguous U.S. river draining into the Pacific, after only the Columbia River, which has almost ten times the flow of the Sacramento. The Colorado River , which reaches

8533-577: The Delta to facilitate water flow from the Sacramento to the Banks Pumping Plant and the California Aqueduct , which can carry as much as 4.2 million acre-feet (5.2 km ) of water each year. From its origin at the Delta the canal runs 444 miles (715 km) southwards through the west side of the San Joaquin Valley, providing irrigation water to farmlands along its length, and lifted almost 3,000 feet (910 m) over

8694-515: The Knaggs Ranch property within the Yolo Bypass by Sacramento River for four consecutive winters. UC Davis shares their results produced the fastest growth of juvenile Chinook salmon in the Central Valley to ever be recorded. The Nigiri project attempted to see if these floodplains as surrogate wetlands which can be controlled to copy the Sacramento River system's annual natural flooding cycle the native fish depend on. Runoff water from agriculture

8855-596: The McCloud River emptied into the Pit River, which joined the Sacramento near the former mining town of Kennett , submerged when Shasta Lake was filled. The Pit River Bridge , which carries Interstate 5 and the Union Pacific Railroad over the reservoir, is structurally the highest double-decked bridge in the United States (although most of the bridge piers are submerged under Shasta Lake when

9016-638: The Mississippi, stretching from Cape Girardeau , Missouri , to the Mississippi delta . They were begun by French settlers in Louisiana in the 18th century to protect the city of New Orleans . The first Louisiana levees were about 90 cm (3 ft) high and covered a distance of about 80 km (50 mi) along the riverside. The U.S. Army Corps of Engineers, in conjunction with the Mississippi River Commission, extended

9177-552: The Pit and McCloud Rivers provided the majority of river flow in dry summers when the Upper Sacramento and other tributaries slowed to a trickle. Monthly combined discharge of Sacramento River at Freeport and Yolo Bypass near Woodland (cfs) The Sacramento River's watershed is the largest entirely in California, covering much of the northern part of the state. The endorheic (closed) Goose Lake drainage basin in southern Oregon , however, has been known to overflow into

9338-521: The Sacramento River system during particularly wet years. The Sacramento River basin generally lies between the Sierra Nevada and Cascade Range on the east and the Coast Ranges and Klamath Mountains in the west, although the part of the basin drained by the Pit River extends east of the Cascades. The Pit River, has the distinction of being one of three rivers that cut through the main crest of

9499-484: The Sacramento River system is the Pit River, which is by far the largest of the three rivers flowing into Shasta Lake. At the USGS Montgomery Creek gauge, the average flow of the Pit River was 4,760 cu ft/s (135 m /s) for the period 1966–2013. By comparison, the Sacramento River at Delta gauge, a few miles above Shasta Lake, recorded an average of 1,191 cu ft/s (33.7 m /s) for

9660-527: The Sacramento River, although not all of them are currently operational. The ones currently in operation are at Delta, California (near the source at Mount Shasta), at Keswick (near Redding), Colusa (about halfway down the river), Verona , and Freeport . The Freeport gauge, which sits just downstream of Sacramento, provides a relatively good metric of the annual outflow from the Sacramento River Basin. The average flow between 1949 and 2013

9821-436: The Sacramento River, including the state capital of Sacramento . Intensive agriculture and mining contributed to pollution in the Sacramento River, and significant changes to the river's hydrology and environment. Since the 1950s the watershed has been intensely developed for water supply and the generation of hydroelectric power . Today, large dams impound the river and almost all of its major tributaries. The Sacramento River

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9982-512: The Sacramento Valley is below 300 feet (91 m) in elevation; in its lower course, the Sacramento River drops only about 1 foot (0.30 m) per mile. Between the bajadas or alluvial slopes extending from the foothills of the Sierra Nevada and Coast Ranges, are the low floodplains of the Sacramento River. The river flows at an elevation somewhat higher than the surrounding terrain due to deposits of sediment over millennia that created raised banks (essentially natural levees ). The banks separate

10143-525: The Sacramento and Feather Rivers into the Yolo Bypass , which parallels the Sacramento River down the west side of the valley. Cache Creek and Putah Creek , two major tributaries which formerly joined the Sacramento River from the west, are now intercepted by the Yolo Bypass via man-made channels. The main channel of the Sacramento flows south, forming the Yolo– Sacramento County line. As

10304-682: The Sacramento are that of the Klamath in the north, the San Joaquin and Mokelumne to the south and the Eel River in the west. The Russian River also lies to the west and the endorheic (closed) Honey Lake and Eagle Lake basins to the north. On the east side are many endorheic watersheds of the Great Basin including the Truckee River and Carson River . Parts of the Sacramento watershed come very close to, but do not extend past,

10465-465: The Sacramento to the Mokelumne River channel, allowing a portion of the water to be pumped south toward Clifton Court Forebay , the receiving reservoir for the main CVP and State Water Project aqueducts which irrigate millions of acres and supply water to over 23 million people in the San Joaquin Valley , the San Francisco Bay Area and Greater Los Angeles . Although river levels are tidally influenced here and occasionally as far north as Verona,

10626-421: The Sacramento with a portion of its historic flood plain, which it would have naturally flooded had the levee system not been in place. During the Great Depression in the 1930s, the first concrete proposals for a statewide water engineering project emerged, but when the state government could not sell the necessary bonds to fund the project, the federal government took over. The Central Valley Project , one of

10787-411: The Sacramento's main tributaries, enabling the regulation of water for irrigation and hydroelectric power. Starting in the late 1950s, two major canals were extended to irrigate the western side of the Sacramento Valley – the Tehama-Colusa and Corning Canals . Starting at the Red Bluff Diversion Dam on the Sacramento, the canals are 111 and 21 mi (179 and 34 km) long respectively, and divert

10948-529: The Sierra Nevada. The watershed also has Lassen Volcanic National Park , which covers 106,000 acres (430 km ) centered on Lassen Peak, the southernmost Cascade volcano. Whiskeytown-Shasta-Trinity National Recreation Area , which is over 200,000 acres (810 km ) in size, straddles much of the upper Sacramento and Trinity Rivers, and is named for the three local reservoirs (Shasta Lake, Trinity Lake and Whiskeytown Lake ) which are popular tourist areas. Many other state parks and recreation areas lie within

11109-432: The U.S. government and the Native Americans involving their relocation onto a reservation in the Sierra foothills; this promise was broken. Therefore, in 1863, the tribes from the area surrounding the middle Sacramento and Feather rivers , the Konkow group, were removed and marched forcibly to the Round Valley Indian Reservation near the Eel River . A total of 461 people were forced from their homes, but only 277 made it to

11270-411: The United States, Sutter and other large landholders in California held on to their properties. In 1848 Sutter assigned James W. Marshall to build a sawmill on the South Fork American River at Coloma , where Marshall discovered gold. Although Sutter and Marshall originally intended to keep the find a secret, news soon broke attracting three hundred thousand hopefuls from all over North America, and even

11431-421: The Yolo Bypass in the rice field floodplains adjacent to the Sacramento River. The name comes from a form of Japanese sushi which contains a slice of fish on top of a compressed wedge of vinegared rice. Salmon migrate from the Central Valley rivers to the ocean where they increase in size for one to three years then return to rivers to spawn, if a young fish is larger when they enter the ocean, they will have more of

11592-602: The ancient path of the Siskiyou Trail, in the 1880s and 1890s. Many parts of the railroad were treacherous, especially in the mountainous areas north of Dunsmuir . It was not long after Sacramento surpassed a population of 10,000, then the Great Flood of 1862 swept away much of it (and almost everything else along the Sacramento River) and put the rest under water. The flood waters were exacerbated by

11753-451: The aqueduct consists of three separate buried steel pipelines, although there are also some aboveground segments. The pipelines, also known as Aqueducts No. 1, 2 and 3, have diameters of 61 inches (1.5 m), 67 inches (1.7 m) and 87 inches (2.2 m), respectively. Aside from the main facilities, the distribution system includes 4,000 miles (6,400 km) of pipes, 125 pump plants, and 168 local reservoirs/storage tanks. The aqueduct

11914-415: The aqueduct. However, Camanche allows for greater diversions into the aqueduct by storing winter floodwaters spilled from Pardee. During the dry season, water is released from Camanche in order to satisfy local water-rights holders, eliminating the need to draw water from Pardee. The aqueduct travels southwest for 95 miles (153 km) through the western foothills of the Sierra Nevada and then west across

12075-557: The area, and relied on Native American labor to maintain his domain. Sutter had something of a two-faced relationship with the many Native American groups in the area. He was friendly with some of the tribes, and paid their leaders handsomely for supplying workers, but others he seized by force to labor in the fields. After the Bear Flag Revolt of 1846 and the Mexican–American War , in which California became part of

12236-551: The bank. Thus Offa's Dyke is a combined structure and Car Dyke is a trench – though it once had raised banks as well. In the English Midlands and East Anglia , and in the United States, a dike is what a ditch is in the south of England, a property-boundary marker or drainage channel. Where it carries a stream, it may be called a running dike as in Rippingale Running Dike , which leads water from

12397-548: The base of the Montezuma Hills , forming the border of Solano and Sacramento Counties. This part of the river is dredged for navigation by large oceangoing vessels and averages three-quarters of a mile (1.2 km) across. North of Antioch and Pittsburg , the Sacramento and San Joaquin Rivers join at the head of Suisun Bay , marking the official end of both rivers. The combined waters flow west through Suisun Bay and

12558-577: The border of California and Nevada . The basin's diverse geography ranges from the glacier-carved, snowcapped peaks of the Sierra Nevada to the sea-level (and often lower) marshes and farmlands of the Sacramento-San Joaquin Delta. The highest point is 14,104 feet (4,299 m) at Mount Shasta , a dormant stratovolcano near the headwaters of the Sacramento River. The Sierra Nevada peaks generally decrease in height from south to north—from over 10,000 feet (3,000 m) in

12719-430: The bypass recorded an average throughput of 4,809 cubic feet per second (136.2 m /s) between 1939 and 2013, mostly from December–March. The highest recorded flow was 374,000 cubic feet per second (10,600 m /s) on February 20, 1986. During the dry season of July through September, the bypass carries low to zero flow. Although the Sacramento River nominally begins near Mount Shasta, the true hydrological source of

12880-512: The center of an agricultural empire that provided food to feed the thousands of miners working in the hills as well as a place of financial exchange of all the gold that was mined. Sacramento was officially established in 1850 and was recognized as the state capital in 1854. As the economy of the Sacramento Valley grew, the Southern Pacific Railroad established tracks along the river to connect California with Oregon following

13041-637: The city of Vancouver , British Columbia , there are levees (known locally as dikes, and also referred to as "the sea wall") to protect low-lying land in the Fraser River delta, particularly the city of Richmond on Lulu Island . There are also dikes to protect other locations which have flooded in the past, such as the Pitt Polder, land adjacent to the Pitt River , and other tributary rivers. Coastal flood prevention levees are also common along

13202-407: The construction of dikes well attested as early as the 11th century. The 126-kilometer-long (78 mi) Westfriese Omringdijk , completed by 1250, was formed by connecting existing older dikes. The Roman chronicler Tacitus mentions that the rebellious Batavi pierced dikes to flood their land and to protect their retreat (70  CE ). The word dijk originally indicated both the trench and

13363-512: The counties. Many of the mountainous regions of the watershed are administered by the U.S. Forest Service . The Sacramento River watershed includes large areas of coniferous forests in the Mendocino and Trinity National Forests in the Coast Ranges, Shasta and Lassen National Forests in the southern Cascades and the Plumas , Tahoe and Eldorado National Forests on the western slopes of

13524-489: The dam during the winter. This project would have flooded between 2 and 3 miles (3.2 and 4.8 km) of the Mokelumne River. Due to environmental concerns, the project was shelved in 2011. Sacramento River The Sacramento River ( Spanish : Río Sacramento ) is the principal river of Northern California in the United States and is the largest river in California. Rising in the Klamath Mountains ,

13685-500: The delta of the Sacramento and San Joaquin Rivers. However, due to their vantage point, neither Fages nor any of his men saw the Sacramento clearly. They assumed that the San Joaquin, coming from the south, was the largest of the merging rivers they saw. In 1808, explorer Gabriel Moraga , on a journey to find suitable sites for the construction of missions, became the first foreigner to see the river clearly. Judging its huge breadth and power he named it Rio de los Sacramentos , or "River of

13846-488: The development of systems of governance in early civilizations. However, others point to evidence of large-scale water-control earthen works such as canals and/or levees dating from before King Scorpion in Predynastic Egypt , during which governance was far less centralized. Another example of a historical levee that protected the growing city-state of Mēxihco-Tenōchtitlan and the neighboring city of Tlatelōlco,

14007-479: The earth together. On the land side of high levees, a low terrace of earth known as a banquette is usually added as another anti-erosion measure. On the river side, erosion from strong waves or currents presents an even greater threat to the integrity of the levee. The effects of erosion are countered by planting suitable vegetation or installing stones, boulders, weighted matting, or concrete revetments . Separate ditches or drainage tiles are constructed to ensure that

14168-553: The east at Colusa . Below Colusa the river flows south-southeast, forming the border of Colusa County and Sutter County to the east. About 20 miles (32 km) further downstream, the Sacramento River reaches the Tisdale Weir. During floods, water overtops the weir and flows east into the Sutter Bypass , the first of two major bypass channels that temporarily store and move floodwaters downstream to reduce pressure on

14329-467: The eastern boundary of the Yolo Bypass . The manually operated Sacramento Weir, located across from downtown Sacramento on the west side of the river, serves to relieve floodwater pressure from the American River by allowing it to drain west into the Yolo Bypass instead of continuing down the Sacramento River. Downstream of Sacramento, the river enters the Sacramento–San Joaquin River Delta ,

14490-503: The extent of the damage. Levee failures in 1980 and 2004 (not caused by earthquakes) on Jones Tract have threatened the aqueduct. An aqueduct joint at the crossing of the Middle River also failed in 1992, nearly causing a washout of the levee. The aqueduct was shut down in time before an actual levee breach could occur. Because Pardee Reservoir is relatively small among California reservoirs, EBMUD has pursued to raise Pardee Dam to

14651-579: The feminine past participle of the French verb lever , 'to raise'). It originated in New Orleans a few years after the city's founding in 1718 and was later adopted by English speakers. The name derives from the trait of the levee's ridges being raised higher than both the channel and the surrounding floodplains. The modern word dike or dyke most likely derives from the Dutch word dijk , with

14812-938: The foundation does not become waterlogged. Prominent levee systems have been built along the Mississippi River and Sacramento River in the United States , and the Po , Rhine , Meuse River , Rhône , Loire , Vistula , the delta formed by the Rhine, Maas/Meuse and Scheldt in the Netherlands and the Danube in Europe . During the Chinese Warring States period , the Dujiangyan irrigation system

14973-529: The geographically similar Colusa Basin is located to the west. The Sutter Bypass begins at Colusa and runs parallel to the east side of the Sacramento River until reaching the confluence with the Feather River . The Yolo Bypass, located on the west side of the river, starts at the confluence of the Feather and rejoins the Sacramento in the Delta. Although termed "bypasses", the system essentially reconnects

15134-425: The gold fields. As the miners expanded their diggings deeper into the Sierra Nevada and Klamath Mountains, Native Americans were pushed off their land and a long series of skirmishes and fights began that continued until intervention by the state and national governments. The influx of migrants brought foreign diseases like malaria and smallpox , which American Indians had no immunity to. These diseases killed off

15295-611: The headwaters of the American River near Lake Tahoe , to 5,000 to 7,000 feet (1,500 to 2,100 m) in Lassen County where they adjoin the Cascade Range. On the west side, the Coast Ranges are the opposite, increasing in height to almost 10,000 feet (3,000 m) in the north. The arid volcanic plateaus in the northeast, which are characterized by alternating hills and large sedimentary basins, typically lie at elevations of 3,000 to 5,000 feet (910 to 1,520 m). Most of

15456-450: The impact is two-fold, as reduced recurrence of flooding also facilitates land-use change from forested floodplain to farms. In a natural watershed, floodwaters spread over a landscape and slowly return to the river. Downstream, the delivery of water from the area of flooding is spread out in time. If levees keep the floodwaters inside a narrow channel, the water is delivered downstream over a shorter time period. The same volume of water over

15617-462: The inland coastline behind the Wadden Sea , an area devastated by many historic floods. Thus the peoples and governments have erected increasingly large and complex flood protection levee systems to stop the sea even during storm floods. The biggest of these are the huge levees in the Netherlands , which have gone beyond just defending against floods, as they have aggressively taken back land that

15778-549: The laboratory tests, empirical correlations related to average overtopping discharge were derived to analyze the resistance of levee against erosion. These equations could only fit to the situation, similar to the experimental tests, while they can give a reasonable estimation if applied to other conditions. Osouli et al. (2014) and Karimpour et al. (2015) conducted lab scale physical modeling of levees to evaluate score characterization of different levees due to floodwall overtopping. Another approach applied to prevent levee failures

15939-1100: The land in the delta to gradually sink since the late 19th century. Many of the delta islands would be underwater if not for the maintenance of the levees and pumps that keep them dry. Some of the "islands" are now up to 25 feet (7.6 m) below the adjacent channels and sloughs. The Sacramento River watershed is home to about 2.8 million people; more than two-thirds live within the Sacramento metropolitan area . Other important cities are Chico , Redding , Davis and Woodland . The Sacramento River watershed covers all or most of Shasta , Tehama , Glenn , Butte , Plumas , Yuba , Sutter , Lake and Yolo Counties. It also extends into portions of Siskiyou , Modoc , Lassen , Lake (in Oregon), Sierra , Nevada , Placer , El Dorado , Sacramento , Solano and Contra Costa Counties. The river itself flows through Siskiyou, Shasta, Tehama, Butte, Glenn, Colusa, Sutter, Yolo, Sacramento, Solano and Contra Costa, often forming boundaries between

16100-550: The land was probably submerged under the Pacific), they were worn by erosion , and the present-day range only formed about 4 million years ago. The northern part of the Sacramento watershed is more ancient, and was formed by intense volcanic activity over 25 million years ago, resulting in lava flows that covered and created the Modoc Plateau, through which the Pit River flows. Mount Shasta and Lassen Peak are among

16261-471: The land. Most of the villages were small. Although it was once commonly believed that the original natives lived as tribes , they actually lived as bands , family groups as small as twenty to thirty people. The Sacramento Valley was first settled by humans about 12,000 years ago, but permanent villages were not established until about 8,000 years ago. Historians have organized the numerous separate original native groups into several "tribes". These are known as

16422-600: The largest city of the Shasta Cascade region, and turns southeast, entering Tehama County . East of Cottonwood it receives Cottonwood Creek – the largest undammed tributary – from the west, then Battle Creek a short distance downstream. Below Battle Creek it carves its last gorge, Iron Canyon, emerging from the hills at Red Bluff , where a pumping station (which replaced the Red Bluff Diversion Dam ) removes water for irrigation. Beyond Red Bluff

16583-481: The largest irrigation projects in the world, was constructed by the U.S. Bureau of Reclamation beginning in 1935. Ultimately, the system would distribute 7 million acre-feet (8.6 km ) to irrigate 3 million acres (1.2 million ha) of land in the Sacramento and San Joaquin Valleys. Construction of Shasta Dam, the principal water storage facility in the Sacramento River system, started in 1938 and

16744-553: The largest of the three, begins in Modoc County in the northeastern corner of California. Draining a vast and remote volcanic highlands area, it flows southwest for nearly 300 miles (480 km) before emptying into Shasta Lake near Montgomery Creek . Goose Lake , straddling the Oregon –California border, occasionally overflows into the Pit River during wet years, although this has not happened since 1881. The Goose Lake watershed

16905-528: The levee system beginning in 1882 to cover the riverbanks from Cairo, Illinois to the mouth of the Mississippi delta in Louisiana. By the mid-1980s, they had reached their present extent and averaged 7.3 m (24 ft) in height; some Mississippi levees are as high as 15 m (50 ft). The Mississippi levees also include some of the longest continuous individual levees in the world. One such levee extends southwards from Pine Bluff , Arkansas , for

17066-420: The levee. A breach can leave a fan-shaped deposit of sediment radiating away from the breach, described as a crevasse splay . In natural levees, once a breach has occurred, the gap in the levee will remain until it is again filled in by levee building processes. This increases the chances of future breaches occurring in the same location. Breaches can be the location of meander cutoffs if the river flow direction

17227-475: The levees in the area, created for the purpose of farming the fertile tidal marshlands. These levees are referred to as dykes. They are constructed with hinged sluice gates that open on the falling tide to drain freshwater from the agricultural marshlands and close on the rising tide to prevent seawater from entering behind the dyke. These sluice gates are called " aboiteaux ". In the Lower Mainland around

17388-542: The main channel of the Sacramento. The Sacramento River and the Sutter Bypass flow parallel for over 40 miles (64 km), rejoining on the border of Sutter County and Yolo County near Knights Landing . The Feather River , the largest tributary of the Sacramento, joins from the east at Verona directly below the Sutter Bypass. A second flood control structure, the Fremont Weir, diverts flood waters from both

17549-543: The main channel, this will make levee overtopping more likely again, and the levees can continue to build up. In some cases, this can result in the channel bed eventually rising above the surrounding floodplains, penned in only by the levees around it; an example is the Yellow River in China near the sea, where oceangoing ships appear to sail high above the plain on the elevated river. Levees are common in any river with

17710-445: The majority of The Lake being drained in the 17th century. Levees are usually built by piling earth on a cleared, level surface. Broad at the base, they taper to a level top, where temporary embankments or sandbags can be placed. Because flood discharge intensity increases in levees on both river banks , and because silt deposits raise the level of riverbeds , planning and auxiliary measures are vital. Sections are often set back from

17871-413: The most recent being the Great Flood of 1862 . Dams, levees and floodways constructed during the 20th century have thus far prevented this phenomenon from re-occurring. The Sacramento River and its valley were one of the major Native American population centers of California. The river's abundant flow and the valley's fertile soil and mild climate provided enough resources for hundreds of groups to share

18032-561: The mountains and plateaus of far northern California as three major waterways that flow into Shasta Lake : the Upper Sacramento River, McCloud River and Pit River . The Upper Sacramento begins near Mount Shasta , at the confluence of North, Middle and South Forks in the Trinity Mountains of Siskiyou County . It flows east into a small reservoir, Lake Siskiyou , before turning south. The river flows through

18193-489: The now, primarily, endorheic (closed) Goose Lake rarely experiences southerly outflow into the Pit River , the most northerly tributary of the Sacramento. The Sacramento and its wide natural floodplain were once abundant in fish and other aquatic creatures, notably one of the southernmost large runs of chinook salmon in North America. For about 12,000 years, humans have depended on the vast natural resources of

18354-599: The numerous Cascade Range volcanoes that still stand in the area. As the Sierra rose, water erosion and glaciation carved deep canyons, depositing massive amounts of sediment to form a coastal plain between the mountains and the Pacific Ocean. About 3 million years ago, multiple terranes were formed and smashed into the North American Plate from the Pacific Plate, causing the uplift of

18515-399: The ocean migrating inland, and salt-water intruding into freshwater aquifers. Where a large river spills out into the ocean, the velocity of the water suddenly slows and its ability to transport sand and silt decreases. Sediments begin to settle out, eventually forming a delta and extending to the coastline seaward. During subsequent flood events, water spilling out of the channel will find

18676-520: The one hand, and to ensure a consistent supply of water on the other. The U.S. Army Corps of Engineers and the State of California completed reports as early as the 1870s and 1880s which outlined future development of the Sacramento, Feather, Yuba and Bear rivers. In 1873, Colonel B.S. Alexander of the Army Corps of Engineers surveyed the Central Valley's hydrology and irrigation systems and proposed

18837-484: The overtopping water impinges the levee. By analyzing the results from EFA test, an erosion chart to categorize erodibility of the soils was developed. Hughes and Nadal in 2009 studied the effect of combination of wave overtopping and storm surge overflow on the erosion and scour generation in levees. The study included hydraulic parameters and flow characteristics such as flow thickness, wave intervals, surge level above levee crown in analyzing scour development. According to

18998-626: The parasitic cowbird , which lays its eggs in the nests of other bird species causing its hatchlings to compete with the others for food. There were once 9 species of amphibians that used the Sacramento River, but some have become extinct and most other populations are declining due to habitat loss caused by agriculture and urban development. Amphibians originally thrived in the marshes, sloughs, side-channels and oxbow lakes because of their warmer water, abundance of vegetation and nutrients, lower predator populations and slower current. This population once included several species of frogs and salamanders;

19159-410: The period 1945–2013. The McCloud River had an average discharge of 775 cu ft/s (21.9 m /s) for the 1967–2013 period. Since the 1960s, the McCloud River flow has been reduced and the Pit River flow increased due to diversion of water for hydropower generation; however the total volume of water entering Shasta Lake remains the same. Before Shasta Dam was built, the volcanic springs feeding

19320-411: The precipitation." The topography of the Sacramento River watershed makes it particularly prone to flooding. Storm water runs quickly off the steep mountains flanking the Sacramento Valley, but with few exceptions the alluvial valley floor is strikingly flat, slowing down the runoff and causing it to overflow the river banks. Before flood control works were built, the winter floods frequently transformed

19481-484: The pressure of floodwaters on the main channel. The bypasses are then allowed to drain slowly once flood crests have passed. For most of the year, the bypasses remain dry and are used for annual crops such as rice. Some of the principal features are the Butte Basin, Colusa Basin, Sutter Bypass and the Yolo Bypass. The Butte Basin is a large lowland area on the east side of the river between Hamilton City and Colusa ;

19642-598: The project, Camanche Dam , was completed below Pardee. In 1970, EBMUD signed a contract with the U.S. Bureau of Reclamation (USBR) for supplemental water from the Folsom South Canal , which draws water from the American River near Sacramento . The USBR supply was delayed for nearly 40 years in part due to minimum flow requirements in the American River to protect salmon and steelhead populations. The Folsom South Canal Connection (FSCC), which links

19803-458: The purpose of impoldering, or as a boundary for an inundation area. The latter can be a controlled inundation by the military or a measure to prevent inundation of a larger area surrounded by levees. Levees have also been built as field boundaries and as military defences . More on this type of levee can be found in the article on dry-stone walls . Levees can be permanent earthworks or emergency constructions (often of sandbags ) built hastily in

19964-436: The reservation; the others perished of disease, starvation or exhaustion. As mining developed from simple methods such as panning and sluicing to a new form of commercialized extraction, hydraulic mining , profits from the petering gold rush made a second leap, earning more profits than placer miners in the early years had ever made. The city of Sacramento , founded on the original site of Sutter's fort, began to flourish as

20125-515: The reservoir is full). The Upper Sacramento River canyon also provides the route for I-5 and the railroad between Lakehead and Mount Shasta. Below Shasta Dam the Sacramento River enters the foothills region of the northern Sacramento Valley. It flows through Keswick Dam , where it receives about 1,200,000 acre⋅ft (1.5 × 10  million km ) of water per year diverted from the Trinity River . It then swings east through Redding ,

20286-473: The rice fields under the Yolo Bypass next to Sacramento River can serve as an important floodplain habitat and feeding ground for juvenile or endangered fish. UC Davis noted juveniles grew much bigger and faster within the flooded rice fields when compared to those released in the Sacramento River. Public agencies, conservation groups and landowners have all been working together and conducting experiments since 2011. Experiments conducted on rice fields took place at

20447-497: The rich valley bottom and marsh lands. Before European contact, the indigenous population of the Sacramento Valley has been estimated at 76,000 people. The first outsiders to see the river were probably the members of a Spanish colonial-exploratory venture to Northern California in 1772, led by Captain Pedro Fages . The group ascended a mountain, likely in the hills north of Suisun Bay , and found themselves looking down at

20608-403: The river after use) are about 4.72 million acre-feet (5.82 km ) for irrigation and 491,000 acre-feet (0.606 km ) for urban use. An additional 7.61 million acre-feet (9.39 km ) is reserved for environmental uses, primarily to maintain a minimum fresh water outflow in the Delta to combat salinity. The U.S. Geological Survey (USGS) has stream gauges on 25 locations along

20769-444: The river continues south it approaches the Sacramento metro area, the largest population center in the watershed. Sacramento International Airport is located on the east bank of the river near Fremont. Near downtown Sacramento it receives the American River from the east, then passes under the historic Tower Bridge and Interstate 80 Business . The California State Capitol sits less than zero point five miles (0.80 km) east of

20930-404: The river flooded up to 650,000 cubic feet per second (18,000 m /s) during the rainy season, equal to the flow of the Mississippi River . Late summers of particularly dry years could see flows drop below 1,000 cubic feet per second (28 m /s). Large volumes of water are withdrawn from the Sacramento River for irrigation, industry and urban supplies. Annual depletions (water not returned to

21091-413: The river floodplains immediately adjacent to the cut banks. Like artificial levees, they act to reduce the likelihood of floodplain inundation. Deposition of levees is a natural consequence of the flooding of meandering rivers which carry high proportions of suspended sediment in the form of fine sands, silts, and muds. Because the carrying capacity of a river depends in part on its depth, the sediment in

21252-642: The river flows south for 400 miles (640 km) before reaching the Sacramento–San Joaquin River Delta and San Francisco Bay . The river drains about 26,500 square miles (69,000 km ) in 19 California counties , mostly within the fertile agricultural region bounded by the Coast Ranges and Sierra Nevada known as the Sacramento Valley , but also extending as far as the volcanic plateaus of Northeastern California. Historically, its watershed has reached as far north as south-central Oregon where

21413-415: The river from the lowlands to the east and west that once served as vast overflow basins during winter storms, creating large areas of seasonal wetlands . Since the 19th century, artificial levee systems have been constructed to enable farming in the fertile flood plain. Today there are 2,000,000 acres (8,100 km ) of irrigated farmland in the Sacramento Valley. Due to the reduction of the floodplain area,

21574-402: The river reaches the low floodplain of the Sacramento Valley, receiving Mill Creek from the east and Thomes Creek from the west near Los Molinos , then Deer Creek from the east near Vina . Southeast of Corning , the Sacramento forms the boundary of Tehama County to the west and Butte County to the east. A few miles downstream it forms the border of Butte County and Glenn County to

21735-440: The river to form a wider channel, and flood valley basins are divided by multiple levees to prevent a single breach from flooding a large area. A levee made from stones laid in horizontal rows with a bed of thin turf between each of them is known as a spetchel . Artificial levees require substantial engineering. Their surface must be protected from erosion, so they are planted with vegetation such as Bermuda grass in order to bind

21896-531: The river where the Tower Bridge crosses it. Shortly downstream, the Port of Sacramento is located on the west side of the Sacramento, connected to the river by a lock. The Sacramento River Deep Water Ship Channel provides access to the port from the Pacific, bypassing about 42 miles (68 km) of the winding lower Sacramento. The channel runs parallel to the Sacramento several miles to the west, and also forms

22057-575: The riverbed, even up to a point where the riverbed is higher than the adjacent ground surface behind the levees, are found for the Yellow River in China and the Mississippi in the United States. Levees are very common on the marshlands bordering the Bay of Fundy in New Brunswick and Nova Scotia , Canada . The Acadians who settled the area can be credited with the original construction of many of

22218-493: The sediments washed down by the millions of tons by hydraulic mining, which filled the beds of the Sacramento, Feather and American rivers up to 7 feet (2.1 m) in Sacramento and also covered thousands of acres of Central Valley lands. A flood in 1875 covered the city of Marysville and when it subsided the town's streets were filled with debris and rocks washed down from the "hydraulicking" going on upstream. Repeated floods and increased demand for Sacramento River water saw

22379-404: The soil to better resist instability. Artificial levees can lead to an elevation of the natural riverbed over time; whether this happens or not and how fast, depends on different factors, one of them being the amount and type of the bed load of a river. Alluvial rivers with intense accumulations of sediment tend to this behavior. Examples of rivers where artificial levees led to an elevation of

22540-499: The speed of flood flow in the Sacramento River has increased, creating a significant hazard for the farms and towns along its course. By the early 20th century engineers had realized not all the floodplains could be safely reclaimed, leading to the intentional creation of flood bypasses where development is limited to annual crops and recreational uses. Further south, much of the delta region is actually below sea level: subsidence caused by wind erosion and intensive farming have caused

22701-415: The two waterways, was finally completed in 2009. The aqueduct begins at Pardee Reservoir, which is formed by Pardee Dam on the Mokelumne River. The reservoir has a capacity of 197,950 acre-feet (0.24417 km), or about a 10-month supply. Camanche Reservoir, located directly below Pardee, has a storage capacity of 417,120 acre-feet (0.51451 km) – twice the size of Pardee – but is not directly linked to

22862-418: The valley into an inland sea. In 1880 State Engineer William H. Hall developed the first flood control plan for the Sacramento River. Hall recognized that with the combination of flat topography and extremely heavy winter runoff volumes, a system of levees alone could not hope to contain flooding, as had been proven time and again in the flood prone city of Sacramento. The Sacramento River Flood Control Project

23023-490: The water stays fresh in all but the driest years. Saltwater intrusion from the Pacific Ocean was one of the main reasons for the construction of the federal Central Valley Project (CVP), whose dams maintain a minimum flow in the Sacramento River to keep seawater at bay. Below Rio Vista , the lower Sacramento River is rejoined by the Deep Water Ship Channel and the Yolo Bypass and curves southwest along

23184-608: The water system by San Francisco. In 1923, the EBMUD was organized and in 1924 acquired water rights to the Mokelumne River, a major tributary in the San Joaquin River system. On November 4, 1924, residents approved $ 39 million in bonds to finance the project. Construction began in 1926 and by 1929, the 345-foot (105 m) high, concrete arch Pardee Dam and the First Mokelumne Aqueduct, consisting of

23345-494: The water which is over the flooded banks of the channel is no longer capable of keeping the same number of fine sediments in suspension as the main thalweg . The extra fine sediments thus settle out quickly on the parts of the floodplain nearest to the channel. Over a significant number of floods, this will eventually result in the building up of ridges in these positions and reducing the likelihood of further floods and episodes of levee building. If aggradation continues to occur in

23506-468: The watershed, which had one of the densest Native American populations in California. The river has provided a route for trade and travel since ancient times. Hundreds of tribes sharing regional customs and traditions have inhabited the Sacramento Valley, first coming into contact with European explorers in the late 1700s. The Spanish explorer Gabriel Moraga named the river Rio de los Sacramentos in 1808, later shortened and anglicized into Sacramento . In

23667-599: The watershed. By geologic standards, the Sacramento is a fairly young river; the borders of its watershed began to form only a few million years ago as magma welling up below the Earth's crust pushed up by the Pacific Plate colliding with the North American Plate caused the formation of the Sierra Nevada . Although mountains had existed as early as 100 million years ago in this region (before then

23828-592: The west. Stony Creek joins from the west in Glenn County, near Hamilton City and about 15 miles (24 km) west of Chico . The river then forms the Glenn– Colusa County line for a short distance before crossing entirely into Colusa County. It passes by the Sutter Buttes , a group of volcanic hills that rise abruptly from the middle of the Sacramento Valley, where it receives Butte Creek from

23989-528: The world, to the Sacramento River in search of fortunes, kicking off the California Gold Rush . People flocked to the region by the Oregon Trail -Siskiyou Trail, California Trail , Southern Emigrant Trail and various land and/or sea routes through the Isthmus of Panama and around southern South America by ship. Steamboats traveled up and down the Sacramento River carrying miners from San Francisco to

24150-431: The years to come, this path, which eventually extended from San Francisco to Portland, Oregon following parts of the Sacramento, Willamette , Klamath , Rogue , and other rivers would become an important trade and travel route. Although just one of thousands of American emigrants that poured into California over the next few years when California became part of the United States, John Augustus Sutter 's arrival marked

24311-478: Was 23,330 cubic feet per second (661 m /s). The maximum recorded flow was 115,000 cubic feet per second (3,300 m /s) on February 19, 1986; the lowest was 3,970 cubic feet per second (112 m /s) on October 15, 1977. Flow in the Yolo Bypass , a relief channel designed to carry a portion of the flood waters in order to protect the Sacramento area, is not measured by the Freeport gauge. A separate gauge on

24472-528: Was at least 1,000 feet (300 m) deep. About 650,000 years ago the lake catastrophically overflowed, draining into San Francisco Bay and creating the Carquinez Strait , the only major break for hundreds of miles in the Coast Ranges. The narrow outlet trapped some of the sediments of the rivers in the Central Valley, forming the inland Sacramento-San Joaquin River Delta . Since then, this inland sea has periodically reformed during times of intense flooding,

24633-416: Was authorized by the federal government in 1917. While it intended to contain minor floods in the river banks by strengthening the existing levee system, the main feature was a series of bypasses, or sections of the valley intentionally designed to flood during high water. Weirs placed at strategic points along the Sacramento River release water into the bypasses when the river reaches a certain stage, relieving

24794-642: Was built by the Qin as a water conservation and flood control project. The system's infrastructure is located on the Min River , which is the longest tributary of the Yangtze River , in Sichuan , China . The Mississippi levee system represents one of the largest such systems found anywhere in the world. It comprises over 5,600 km (3,500 mi) of levees extending some 1,000 km (620 mi) along

24955-465: Was completed in 1945. Controlling runoff from the upper 6,600 square miles (17,000 km ) of the Sacramento River watershed, Shasta greatly reduces flood peaks on the middle and lower parts of the Sacramento River. Flood waters are stored for irrigation in dry years as well as navigation and electricity generation. In the following decades, more huge reservoirs – capable of storing a combined 13 × 10 acre-feet (16 km ) of water – were constructed on

25116-400: Was completed in 1963, and was built to facilitate navigation of large oceangoing ships from the Delta to the port of Sacramento. The channel bypasses the winding lower part of the Sacramento River between the state capital and the Delta thus reducing water travel times. It also serves to discharge floodwaters from the lower end of the Yolo Bypass . Built by the Army Corps of Engineers, the canal

25277-488: Was constructed during the early 1400s, under the supervision of the tlahtoani of the altepetl Texcoco, Nezahualcoyotl. Its function was to separate the brackish waters of Lake Texcoco (ideal for the agricultural technique Chināmitls ) from the fresh potable water supplied to the settlements. However, after the Europeans destroyed Tenochtitlan, the levee was also destroyed and flooding became a major problem, which resulted in

25438-434: Was crucial to the renewal of existing wetlands and the creation of new ones. Since the late 19th century the river has been mostly locked in a fixed channel, which once could shift hundreds of feet or even several miles in a year because of floods. In 2010, about 100 miles (160 km) of the river's riparian forests were undergoing restoration. UC Davis initiated a project known as The Nigiri Project which takes place under

25599-643: Was practiced in a few areas. Settlement size ranged from small camps to villages of 30–50 permanent structures. Acorns were a staple food , and the Sacramento Valley's riparian zones, which supported seven species of native oaks, provided these in abundance. Native Americans pounded the acorns into flour, which they used to make bread and cakes. Abundant salmon and steelhead runs in the Sacramento River and its tributaries were harvested using fishing weirs, platforms, baskets and nets. The river also provided shellfish, sturgeon, eel and suckerfish They also hunted waterfowl, antelope and deer which all existed in huge numbers in

25760-656: Was the Trinity River Project (which would become part of the CVP), sending over 90 percent of the flow of that river into the Sacramento via a tunnel under the Klamath Mountains. Due to environmental damage and fish kills in the Trinity River, the volume of diverted water has been limited by law since the 1990s. Other, larger projects ultimately failed to take root. One of the most notorious,

25921-470: Was under the control of Mexico , although few Mexican settlers had come to what would later become the state, mostly settling in the small pueblos and ranchos along the south and central coast. The HBC mountain men created the Siskiyou Trail out of several Native American paths that ran through the mountains between Oregon's Willamette Valley and the northern part of the Sacramento Valley. In

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