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San Joaquin River

The San Joaquin River is the longest river of Central California. The 366-mile (589 km) long river starts in the high Sierra Nevada and flows through the rich agricultural region of the northern San Joaquin Valley before reaching Suisun Bay, San Francisco Bay, and the Pacific Ocean. An important source of irrigation water as well as a wildlife corridor, the San Joaquin is among the most heavily dammed and diverted of California's rivers.

Name
The river was called many different names; at times different parts of the river were known by different names. The southern Yokuts called the river, Tihshachu (Tih-shah-choo), meaning salmon-spearing place. The present name of the river dates to 1805–1808, when Spanish explorer Gabriel Moraga was surveying east from Mission San José in order to find possible sites for a mission. Moraga named a tributary of the river (it is not known which one) for Saint Joachim, husband of Saint Anne and father of Mary, the mother of Jesus. The name Moraga chose was later applied to the entire river; it was in common use by 1810. In 1827, Jedediah Smith wrote in his journal that an unknown group of Native Americans called the river the Peticutry, a name which is listed as a variant in the U.S. Geological Survey (USGS) Geographic Names Information System. An earlier name for the lower section of the San Joaquin was Rio de San Francisco, which was the name Father Juan Crespí gave to the river he could see entering the Sacramento-San Joaquin Delta from the south. A member of the Pedro Fages party in 1772, Crespi's vantage point was the hilltops behind modern Antioch. Another early name was Rio San Juan Bautista, the origin of which is unknown. ==Course==
Course
and the Union Pacific Railroad along the northern border of Fresno. The early stages of construction of California High-Speed Rail's San Joaquin River Viaduct is also visible. during the high flows of April 2006 The river's source is located in the Ansel Adams Wilderness, in the south-central Sierra Nevada at the confluence of three major affluents: the Middle Fork, which rises from Thousand Island Lake at almost above sea level, and the South Fork, which begins at Martha Lake in Kings Canyon National Park and flows through Florence Lake, joins a short distance downstream. The Middle Fork is considered the largest of the 3 forks. From the mountainous alpine headwaters, the San Joaquin flows generally south into the foothills of the Sierra, passing through four hydroelectric dams. It eventually emerges from the foothills at what was once the town of Millerton, the location of Friant Dam since 1942, which forms Millerton Lake. This lack of riverwater begins in the between Friant Dam and Mendota, The numerous tributaries of the San Joaquin – the Fresno, Chowchilla, Merced, Tuolumne, Mariposa Creek, Calaveras, Mokelumne, and others – flowed freely across alluvial flood plains to join the river. All of the major tributaries of the river originate in the Sierra Nevada; most of the streams that start in the Coast Range are intermittent, and contribute little to the flow of the San Joaquin. During the winter, spring, and early summer, storms and snowmelt swell the river; in 1914 – before the development of major dams and irrigation diversions – the California Department of Engineering estimated the river's flow in full flood at . This range is less extreme than the temperatures below Vernalis where the range is from 2°Celsius (35.6 °F)on Dec 26, 1987 to on August 9, 1990. The river typically ends above the Mendota Pool. Larger flows in the fall may make it possible for the river to extend further towards the ocean, but for the last several years, this is a rare occurrence. The water is largely held behind Friant Dam. The typical monthly flow of the San Joaquin River near the Sack Dam is 0. There have been seepage concerns below this part of the river, so current flows are restricted below the Sack Dam. The present annual flow of the San Joaquin River near Vernalis is about , or 4.5 million acre-feet (5.6 million m3) per year. According to USGS stream gauge #11303500 at Vernalis, above Suisun Bay and below the mouth of the Stanislaus River, the average discharge of the San Joaquin River between 1924 and 2011 was , or 3.3 million acre-feet (4.0 million m3) per year.''' Colors= id:lightgrey value:gray(0.8) id:darkgrey value:gray(0.3) id:sfondo value:rgb(1,1,1) id:barra value:rgb(0.6,0.8,0.9) ImageSize = width:800 height:280 PlotArea = left:60 bottom:30 top:30 right:60 DateFormat = x.y Period = from:0 till:10000 TimeAxis = orientation:vertical AlignBars = justify ScaleMinor = gridcolor:lightgrey increment:1000 start:0 BackgroundColors = canvas:sfondo BarData= bar:Jan text:Jan. bar:Fév text:Feb. bar:Mar text:Mar. bar:Avr text:Apr. bar:Mai text:May bar:Jun text:Jun. bar:Jul text:Jul. bar:Aoû text:Aug. bar:Sep text:Sep. bar:Oct text:Oct. bar:Nov text:Nov. bar:Déc text:Dec. PlotData= color:barra width:30 align:left bar:Jan from:0 till: 5010 bar:Fév from:0 till: 6860 bar:Mar from:0 till: 7220 bar:Avr from:0 till: 7100 bar:Mai from:0 till: 7560 bar:Jun from:0 till: 6280 bar:Jul from:0 till: 2570 bar:Aoû from:0 till: 1450 bar:Sep from:0 till: 1760 bar:Oct from:0 till: 2280 bar:Nov from:0 till: 2260 bar:Déc from:0 till: 3430 PlotData= bar:Jan at: 5010 fontsize:S bar:Fév at: 6860 fontsize:S bar:Mar at: 7220 fontsize:S bar:Avr at: 7100 fontsize:S bar:Mai at: 7560 fontsize:S bar:Jun at: 6280 fontsize:S bar:Jul at: 2570 fontsize:S bar:Aoû at: 1450 fontsize:S bar:Sep at: 1760 fontsize:S bar:Oct at: 2280 fontsize:S bar:Nov at: 2260 fontsize:S bar:Déc at: 3430 fontsize:S ==Geology==
Geology
In a geologic context, the San Joaquin River can be divided into two major segments. The upper above Friant Dam in the Sierra is characterized as a steep-gradient, rocky mountain stream. Over millions of years, the upper San Joaquin, as well as the upper reaches of most of its tributaries, have eroded enormous amounts of rock and sediment from the mountains. Most of the Sierras are underlain by granitic igneous and metamorphic rock dating back to the Mesozoic Era (250–66 MYA); in addition many of the San Joaquin's tributaries flow across a foothills region of metamorphosed volcanic rock more famously known as the Mother Lode Gold Belt. The lower part of the river, in sharp contrast, is a meandering stream flowing over Cenozoic alluvial deposits (66 MYA-present), which together comprise the flat floor of the Central Valley. The aquifer receives in excess of of inflow per year, mostly from precipitation and irrigation water seepage. Concentration of chloride and other minerals generally increases from east to west across the basin.{{cite web |url=https://ca.water.usgs.gov/groundwater/gwatlas/valley/quality.html |archive-url=https://web.archive.org/web/20090525151639/http://ca.water.usgs.gov/groundwater/gwatlas/valley/quality.html |archive-date=2009-05-25 ==History==
History
Indigenous people Archaeological finds near the southern end of the San Joaquin Valley suggested that humans first arrived in the region as early as 12,000 but no later than 5,000 years ago. In contrast, the Miwok occupied land deeper within the Sierra Nevada stretching north from the Merced River to the Mokelumne or the American, a tributary of the Sacramento, and west to the Delta region. Most of the Miwok people in the watershed were part of the appropriately named Sierra Miwok group. The Yokuts were unique among California natives in that they were divided into true tribes. Each had a name, a language, and a territory. Of the about 63 known Yokuts tribes, 33 lived along or around the San Joaquin River and its tributaries. The staple food for San Joaquin Valley inhabitants was the acorn, which when ground, could be made into various foods such as cakes. Grinding the acorns was a simple process where they crushed the nuts using rocks in natural granite depressions. Many of the surviving examples of acorn milling areas can still be found in the foothills, especially around the Kaweah River area. Another narrative does not mention Fages' name, but does say that Crespí was the one who reached Suisun Bay in 1772. During this visit, Crespí called the San Joaquin River "El Rio de San Francisco", a name that was not used widely due to the river's remoteness but persisted until the early 19th century. (background), where Juan Crespí first gazed upon the Sacramento-San Joaquin Delta in 1772, with Suisun Bay in the foreground In the autumn of 1772 Fages set out from Mission San Luis Obispo de Tolosa in pursuit of deserters from the Spanish army, and traveled east then north over the Tehachapi Mountains through Tejón Pass, which today carries Interstate 5 into the San Joaquin valley. After crossing the mountains, he came upon the shore of Buena Vista Lake at the southern end of the San Joaquin Valley, and gave the name Buena Vista ("beautiful view") to the pass and a nearby Native American village. However, Fages did not venture farther north, and thus did not further explore the main stem of the San Joaquin River. California became part of Mexico in 1821. The new government secularized the Spanish missions and as a result the conversos in the missions were no longer protected by the missionaries from exploitation. The Mexican government began to tax the missions excessively. From 1820, El Camino Viejo, a route between Los Angeles and the San Francisco Bay along the west side of the San Joaquin Valley, brought settlements from the United States into the valley. During Mexican rule, the mission lands in the San Joaquin Valley were subdivided to wealthy landowners (rancheros). The mission lands that were supposed to be given to the natives were also fraudulently taken over by American settlers. His expedition then turned east in an attempt to cross the Sierra Nevada. They tried to summit the range by way of both the Kings River and the American River (a tributary of the Sacramento), but it was early spring and the snow was too deep. They crossed the mountains along the Stanislaus River canyon, becoming the first recorded whites to cross the Sierra Nevada on foot. It is still disputed over whether Smith's party discovered gold on the San Joaquin or one of its tributaries. Although some of his men confirmed it, Smith did not make any mention in his journal. In the early 1830s, a few fur trappers from the Pacific Northwest exploring southwards into the San Joaquin Valley saw an epidemic of smallpox and malaria brought unintentionally by the Europeans that had swept down the San Joaquin River corridor during the summer of 1833, killing between 50 and 75 percent of the entire native population in the valley. The outbreak continued year after year with diminishing acuteness until about 50,000–60,000 indigenous people were dead. Explorer Kit Carson noted in 1839 that "... cholera or some other fearful scourge broke out among them and raged with such fearful fatality that they were unable either to bury or burn their dead, and the air was filled with the stench of their decaying bodies." During the time Mexico was in control of California, the San Joaquin River region was only sparsely populated, and used almost exclusively for cattle ranching. When California won independence from Mexico in 1846, becoming part of the United States the following month, a flood of American settlers descended upon the valley. Just a year before, Benjamin Davis Wilson "drove a herd of cattle from his Riverside rancho through the San Joaquin Valley to Stockton and reported seeing not a single white man". After the Americans took over, emigrants began trickling in increased numbers, establishing the towns of Kingston City, Millerton, and Fresno City. The newcomers also included a group of Mormons led by Samuel Brannan, who sailed aboard the Comet to establish a settlement at the confluence of the San Joaquin and the Stanislaus called "New Hope" (later Stanislaus City). The real influx came in 1848, when a gold strike on the American set off the California Gold Rush. Within one year, the population of the San Joaquin Valley increased by more than 80,000. quickly extended the length of the valley, some following old cattle routes and Native American trails, and were served by mule teams and covered wagons. Another notable but much smaller settlement was Las Juntas, near present-day Mendota. This was a haven for criminals and fugitives, and was frequented by the infamous bandits Joaquín Murrieta and Tiburcio Vásquez. It was in the mid-1860s that the San Joaquin River and its surrounds underwent a substantial change: the introduction of irrigated agriculture. As early as 1863, small irrigation canals were built in the Centerville area, southeast of Fresno, but were destroyed in subsequent floods. The vulnerability of the small local infrastructure led to the establishment of irrigation districts, which were formed to construct and maintain canals in certain areas of the valley. One of the first was the Robla Canal Company in the Merced River area, which went into operation in March 1876, but was soon surpassed by the Farmers Canal Company. The district built a diversion dam on the Merced, sending its water into a pair of canals still in use today. Haggin soon ran into conflicts with other landowners over riparian water rights, as the larger districts, including his, had more financial reserves and engineering expertise, and were the first to build dams and diversions on a large scale. This resulted in the drying out of streams and rivers before they reached downstream users and sparked conflict over how much water could be allotted to whom. In Haggin's case, his company ran into problems with the Miller & Lux Corporation, run by Henry Miller and Charles Lux, who owned more than throughout the San Joaquin Valley, Tulare Basin, and other regions of California. The court battle that resulted would change water laws and rights in the San Joaquin River valley, and ended up promoting large-scale agribusiness over small farmers. Miller and Lux were not any newer to the San Joaquin Valley than had been Haggin, but were the driving influence on valley agribusiness until well into the early 20th century. The corporation had begun acquiring land in the valley in 1858, eventually holding sway over an enormous swath reaching from the Kern River in the south to the Chowchilla River in the north. Much of the land that Miller and Lux acquired was swamp and marsh, which was considered virtually worthless. However, with their huge capital, they could afford to drain thousands of acres of it, beginning an enormous environmental change that eventually resulted in the loss of over 95 percent of the wetlands adjoining the San Joaquin River and Tulare Basin. Henry Miller exercised enormous political power in the state, and most San Joaquin Valley inhabitants either were avid supporters of him or despised him. When Miller died in 1916, his company owned in the San Joaquin Valley alone with hundreds of miles of well-developed, maintained irrigation canals. As said by Tom Mott, the son of Miller and Lux' irrigation superintendent, "Miller realized you couldn't do anything with the land unless you had the water to go with it. Perhaps more than any other person, Miller had more of a lasting impact on the San Joaquin River than any other individual." By the early 20th century, so much water was being diverted off the San Joaquin River and its tributaries that the river was no longer suitable for navigational purposes. As a result, commercial navigation began a decline starting in the late 19th century and was completely gone by 1911. With over under irrigation along the river by 1900 It has been said that fights over the river have caused "some of the most bitter and longest running lawsuits ever to clog the courts. Arguably, it is the most litigated river in America."{{cite news ==Dams, diversions and engineering==
Dams, diversions and engineering
Hydroelectric development in the early 1900s , the principal dam of the Big Creek Hydroelectric Project, completed in 1959 By the early 20th century, Californian cities as far south as Los Angeles were looking to new sources for electricity because of their rapidly growing populations and industries. Two visionaries, railroad baron Henry E. Huntington and engineer John S. Eastwood established a fledgling power company in 1902 today known as Southern California Edison, and acquired water rights to the upper San Joaquin River from the Miller and Lux Corporation. During that year, Huntington and Eastwood devised plans to utilize the water of the San Joaquin River and some of its headwaters tributaries in what would become one of the most extensive hydroelectric systems in the world, known as the Big Creek Hydroelectric Project. Construction of the system's facilities, which included Mammoth Pool and Redinger Dams on the San Joaquin and four additional reservoirs on its tributaries with a total storage capacity of , started in 1911. In 1926, Stockton pooled its finances with the federal and state governments for a total of $8.2 million. Construction on the channel, which included widening and deepening the riverbed and cutting off meanders and oxbow lakes, began in earnest in 1928. These included major cuts at Hog Island, Venice Island and Mandeville Island, plus five smaller straightening projects. The navigation project shortened the river length by and deepened it to . Additional deepening work was carried out in 1968 and 1982. Today, the navigation channel, known as the Stockton Deep Water Ship Channel, can handle fully loaded vessels of up to and up to long. As a result, the project was transferred to the federal government and switched hands several times between the U.S. Army Corps of Engineers (USACE) and U.S. Bureau of Reclamation (USBR) before finally being authorized in the Rivers and Harbors Act of 1937 as a USBR undertaking and part of the New Deal, a series of large-scale reforms and construction projects intended to provide jobs for the millions of unemployed during the Depression. , the reservoir of Friant Dam and the largest on the San Joaquin mainstem The bypass system starts with the Chowchilla Canal Bypass, which can divert up to off the San Joaquin, a few miles above Mendota. After intercepting the flow of the Fresno River, the system is known as the Eastside Bypass, which runs northwest, crossing numerous tributaries: Berenda and Ash Sloughs, the Chowchilla River, Owens Creek and Bear Creek. Near the terminus, the bypass channel has a capacity of roughly . The Eastside Bypass ends just upstream of the Merced River confluence, where the San Joaquin levee system is better designed. However, the levees on the bypass channel are generally more well-built than those on the San Joaquin mainstem and thus the channel of the San Joaquin runs dry in some places where the entire flow has been diverted to the bypass system. Millerton Lake, the reservoir of Friant Dam, is small compared to other reservoirs in the San Joaquin basin, such as Don Pedro and Pine Flat. The Bureau of Reclamation in conjunction with the California Department of Water Resources has proposed the construction of a new dam on the San Joaquin, Temperance Flat Dam, a few miles upstream of Friant. The proposed $1.2-3.5 billion dam would stand high and create a reservoir of , well over twice the capacity of Millerton Lake. However, opponents assert that the upper San Joaquin River, which is already controlled by dozens of smaller reservoirs upstream of Millerton Lake, will not provide sufficient discharge to fill the reservoir except in very wet years. There would be significant evaporation losses from the reservoir, and the water required to fill it would put further pressure on already stressed water resources in the San Joaquin River basin. ==Ecology and environment==
Ecology and environment
, one of the few remaining wetland areas along the San Joaquin River Hundreds of years ago, the San Joaquin flowed freely through a grass and marsh-dominated region variously known as the "California prairie", "California annual grassland", or "Central Valley grasslands". It is widely believed that the dominant grass species throughout the San Joaquin River valley and Tulare Basin, as well as the Sacramento Valley, the Sierra foothills and Coast Ranges, was Nassella pulchra, a type of bunchgrass more commonly known as purple needlegrass. Today, this vegetation community exists only in isolated pockets because of development of the valley for agriculture, and in much of the remnant open areas where it once thrived, now grows introduced flora such as annual rye and wild oat. Up to 75 percent of the historic species were endemic to the Sacramento-San Joaquin basin. Most native fish stocks have suffered because of predation by introduced species and dam construction. In a study from 1993 to 1995, it was found that the main stem of the San Joaquin River was mainly populated by fathead minnow, red shiner, threadfin shad and inland silverside, all of which were introduced. Downstream portions of the river's main tributaries were populated mainly by largemouth and smallmouth bass, redear sunfish and white catfish, while native species have survived relatively well in the upper reaches of the river and its tributaries, which also play host to introduced brown trout. The California Department of Fish and Game estimated in the 1930s that the historic salmon run was likely in the vicinity of 200,000 to 500,000 spawners annually, but by the mid-20th century, reduction in river flows led to the run dropping to about 3,000-7,000. Some sources put the historic populations as high as three hundred thousand, but this is highly unlikely because of the limited habitat available in the watershed. The introduction of predatory fish species such as bluegill and various types of bass that prey on salmon smolt are also a major contributor to the decline. Groundwater overdraft Because of the heavy demand of water for agriculture and the insufficient flow of the San Joaquin River, groundwater in the San Joaquin Valley's rich aquifer has been an important source of irrigation supply since the late 19th century. Historically, surface water was able to provide all the needed supply, but as agricultural lands spread across more and more of the valley, groundwater pumping became increasingly common. Also, with the introduction of better technology that allowed farmers to dig deeper wells and install electrical pumps, groundwater was seen as an often cheaper and easily accessible source compared to the river. Water imported from Northern California through the Central Valley Project managed to stave off increasing rates of withdrawal for several years, until the 1977 California drought heavily decreased water supplies from these sources for a while and caused many farmers to return to groundwater pumping.{{cite web Groundwater withdrawal reached its peak during the 1960s with more than being drawn from the aquifer each year – over twice the present flow of the San Joaquin River – which accounted for 69.6% of all the groundwater pumped within the Central Valley, and nearly 14 percent of all the groundwater withdrawn in the United States.{{cite web Even after better practices and new sources of water through federal projects, groundwater pumping continues at a tremendous rate. The San Joaquin Valley aquifer lost about from 1961 to 2003, which despite being a dramatic reduction from the 1960s, still amounts to nearly per year. The subsidence caused by groundwater withdrawal has threatened infrastructure in the San Joaquin Valley, including the California Aqueduct, a State Water Project facility that conveys water from the delta region to coastal-central and southern California. Subsidence has also damaged highways and power lines as well as causing some areas to be more susceptible to flooding.{{cite web Reconnecting to the ocean In 2009, the Bureau of Reclamation began to release water from Friant Dam in an effort to restore two once-dry stretches of the San Joaquin of about .{{cite web In addition to the dry reaches, the higher discharge in the San Joaquin will help restore a total of of river, figuring in stretches with low or polluted flows. It is also hoped that the water will help dilute contaminants in the river caused by pesticides and fertilizers that are applied to the surrounding farmland. In turn, the boost in flow could assist restoration efforts and help flush out saline water in the Sacramento-San Joaquin Delta, where water is pumped into state aqueducts which provide water supplies to two-thirds of Californians.{{cite web Phase One improvements include the following: The San Joaquin River east of Los Banos will be increased to route up to of water by December 2011. Salmon will be re-introduced to the river in 2012,{{cite news Phase Two improvements include the following: The USBR will begin releasing up to , or "full restoration flows", from the Friant Dam in 2014. Flows will depend on whether the year is wet, dry or for intermediate levels of precipitation. Additional rehabilitation work is projected to continue until 2016 to ensure that the river can transport of water through rainfall and releases from Friant Dam all the way to Bear Creek and the Eastside bypass. The higher capacity of the river is also to accommodate rainfall or prevent flooding. The total cost of the restoration, one of the largest river recovery efforts in the United States,{{cite web The San Joaquin River was last connected to the ocean in 2010. By reconnecting, it means the portion from Friant Dam to where the San Joaquin River joins the Merced river above Vernalis. This may happen in 2016 or 2017.{{cite web Wetlands Efforts have been under way to restore wetlands along the San Joaquin River as well as on the historic shores of Tulare Lake. These primarily entail the cleanup of existing wetlands and procuring additional water supplies, rather than converting agricultural land back into the original swamp and marsh. Since wetlands can provide a natural form of flood control – wetlands act like sponges, absorbing flood flows during the rainy season and releasing the accumulated water during the dry season – and also can filter out many forms of toxins, especially from fertilizers, they are important to maintaining good water quality in the San Joaquin River.{{cite web ==Watershed==
Watershed
At , the San Joaquin River watershed proper drains a fair swath of inland central California, an area comparable to the size of the Upper Peninsula of Michigan. If combined with the Tulare Basin, which historically (and still rarely) experiences northerly outflow to the San Joaquin River, it would be the largest single drainage basin entirely in the state. The San Joaquin Valley's major southeast–northwest axis runs roughly parallel with the Pacific coast of California; it measures covering all or parts of seventeen California counties stretching from north of Lodi to well south of Bakersfield. On the west and northwest, the San Joaquin watershed borders those of rivers draining into the Pacific, while beyond almost all of the other divides lie endorheic basins, mostly of the Great Basin. To the north, a low series of ridges separates the San Joaquin River basin from that of the Sacramento River. The Coast Ranges bound the watershed on the west and borders on the drainages of the Pajaro River, Salinas River and the endorheic Carrizo Plain. On the south, the Tehachapis wall off the Tulare Basin from the Mojave Desert. To the east, the Sierra Nevada separate the San Joaquin drainage from those of multiple smaller rivers that terminate in various Great Basin lakes. From north to south, these are the Carson, Walker, and Owens Rivers. The sloping alluvial fan of the Kings River divides the northern San Joaquin Valley from the Tulare Basin. Tributaries Seven major tributaries flow directly into the San Joaquin River, all of which run from the Sierra Nevada westwards into the main stem. In addition, some of the discharge of the Kings River also enters the San Joaquin directly (but seasonally) through a distributary. Of these, the Tuolumne River is the largest in any respect: longest, greatest drainage basin, and highest discharge. The Merced River is the second largest by length and drainage basin, but the Mokelumne River has a greater flow. Tributaries are listed below proceeding from the mouth upstream, with their respective main-stem length, watershed and discharge noted. Rivers of the Tulare Basin are noted below the San Joaquin's direct tributaries with their individual data. Most of the tributaries had much larger flows before irrigation diversions – for example, the Tuolumne's historic discharge was almost 48% higher than it is now. Tributaries in the Tulare Lake basin ==See also==
Works cited
• {{cite book • • • • • Gudde, Erwin G.; Bright, William (2004). California Place Names: The Origin and Etymology of Current Geographical Names. University of California Press. . • • • • • • • • {{cite book • • {{cite book • • • • ==External links==
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