|Great Central Valley, The Valley|
Topography, major parts and cities of the Central Valley
|Location||California, United States|
|Long-axis length||450 mi (720 km)|
|Width||40 to 60 miles (64 to 97 km)|
|Area||22,500 square miles (58,000 km2)|
|Depth||2,000 to 6,000 feet (610 to 1,800 m)|
|Age||2-3 million years|
|Bounded by||Sierra Nevada (east), Cascade Range, Klamath Mountains (north), Coast Range, San Francisco Bay (west), Tehachapi Mountains (south)|
|Population centers||Redding, Chico, Yuba City, Sacramento, Stockton, Porterville, Modesto, Merced, Fresno, Visalia, Bakersfield, Clovis|
|Traversed by||Interstate 5, Interstate 80, State Route 99|
|Watercourses||Sacramento River, San Joaquin River, Kings River|
California's Central Valley is a large, flat valley that dominates the central portion of California. It is 40 to 60 miles (60 to 100 km) wide and stretches approximately 450 miles (720 km) from northwest to southeast, inland from and parallel to the Pacific Ocean coast. It covers approximately 22,500 square miles (58,000 km2), about 13.7% of California's total land area (slightly smaller than the state of West Virginia), and is home to some of California's most productive agricultural areas.
The Central Valley comprises multiple major watershed systems: the Sacramento Valley, which receives well over 20 inches (510 mm) of rain annually, in the north, and the drier San Joaquin Valley in the south, with the Tulare Basin and its semi-arid desert climate at the southernmost end. The Sacramento and San Joaquin river systems drain their respective valleys and meet to form the delta, a large expanse of interconnected canals, stream beds, sloughs, marshes and peat islands, ultimately flowing to the Pacific by way of San Francisco Bay. The waters of the Tulare Basin essentially never flow to the ocean, though they are connected by man-made canals to the San Joaquin and could drain there again naturally if they were ever to rise high enough.
The Central Valley is outlined by the Cascade, Sierra Nevada, and Tehachapi mountain ranges on the east, and the Coast Ranges and San Francisco Bay on the west. The broad valley floor is carpeted by vast agricultural regions, and dotted with numerous population centers. Subregions and their counties commonly associated with the valley include:
About 6.5 million people live in the Central Valley today, and it is the fastest growing region in California. There are 12 Metropolitan Statistical Areas (MSA) and 1 Micropolitan Statistical Area (μSA) in the Central Valley. Below, they are listed by MSA and μSA population. The largest city is Fresno, followed by the state capital, Sacramento. The following metropolitan and micropolitan statistical areas listed from largest to smallest:
The flatness of the valley floor contrasts with the rugged hills or gentle mountains that are typical of most of California's terrain. The valley is thought to have originated below sea level as an offshore area depressed by subduction of the Farallon Plate into a trench further offshore. The San Joaquin Fault is a notable seismic feature of the Central Valley.
The valley was later enclosed by the uplift of the Coast Ranges, with its original outlet into Monterey Bay. Faulting moved the Coast Ranges, and a new outlet developed near what is now San Francisco Bay. Over the millennia, the valley was filled by the sediments of these same ranges, as well as the rising Sierra Nevada to the east; that filling eventually created an extraordinary flatness just barely above sea level; before California's massive flood control and aqueduct system was built, the annual snow melt turned much of the valley into an inland sea.
Another significant geologic feature of the Central Valley lies hidden beneath the delta. The Stockton Arch is an upwarping of the crust beneath the valley sediments which extends southwest to northeast across the valley.
Physiographically, the Central Valley lies within the California Trough physiographic section, which is part of the larger Pacific Border province, which in turn is part of the Pacific Mountain System.
The 'Central Valley Grassland' is the Nearctic temperate and subtropical grasslands, savannas, and shrublands ecoregion which was once a diverse grassland containing areas of desert grassland (at the southern end), prairie, savanna, riverside woodland, marsh, several types of seasonal vernal pool, large lakes such as now-dry Tulare Lake, the largest lake in the United States west of the Mississippi, Buena Vista Lake and Kern Lake. However much of the Central Valley environment has been removed or altered by human activity including the introduction of exotic plants, especially grasses. The oak woodlands and chapparal that fringe the valley have been categorised as the California interior chaparral and woodlands ecoregion. The wetlands have been the target of rescue operations to restore areas nearly destroyed by agriculture.
The dominant grass of the valley was Nassella pulchra mixed with other species, but today only 1% of the grassland in the valley is original and intact. Grassland flowers include California poppy (Eschscholzia californica), lupins, and Purple Owl's Clover (Castilleja exserta) which can still be seen, especially in Antelope Valley in the Tehachapi hills. Riverside trees include willows, western sycamore (Platanus racemosa), box elder (Acer negundo), Fremont cottonwood (Populus fremontii), and the endemic Valley oak (Quercus lobata).
The Central Valley was once home to large populations of pronghorn antelope (Antilocapra americana), elk including the endemic Tule Elk subspecies (Cervus elaphus nannodes), mule deer (Odocoileus hemionus), California ground squirrels, gophers, mice, hare, rabbits and kangaroo rats, along with their predators including the San Joaquin Kit Fox which is now an endangered subspecies survival on the hillsides of the San Joaquin Valley. The wetlands of the Valley were an important habitat for wintering waterbirds and migrating birds of other kinds. Reptiles and amphibians of the valley include the endemic San Joaquin coachwhip snake (Masticophis flagellum ruddocki), blunt-nosed leopard lizard (Gambelia sila), Gilbert's skink (Eumeces gilberti) and the western aquatic garter snake (Thamnophis couchii). There are also a number of endemic invertebrates. <3
Agriculture, especially the creation of grazing land, and the draining of lakes and rivers have radically altered the habitats of the Valley. Most of the grassland has been overtaken by new species, most of the vernal pools have been drained or otherwise destroyed with only those on the higher slopes remaining, the marshland has mostly been drained too, and the riverbank woodlands have nearly all been affected.
The Great Valley Grasslands State Park preserves an example of the native grass habitat in the valley, while oak savanna habitats remain near Visalia. There are areas of wetland and riverside woodland in the north especially on the Sacramento River system including the Nature Conservancy’s Cosumnes River Preserve just south of Sacramento, Gray Lodge Wildlife Area, Butte Sink Wildlife Management Area, and other patches in the delta area. Remaining vernal pools include Pixley National Wildlife Refuge between Tulare, California and Bakersfield and Jepson Prairie Preserve in the delta. There are large blocks of desert scrubland in the southern San Joaquin Valley and in the Carrizo Plain which is just outside the valley but has a similar landscape.
All these patches of natural habitat are disconnected and this is particularly damaging for wildlife that is used to migrating along the rivers of the valley, birds such as warblers and cuckoos, and reptiles and amphibians. Meanwhile clearance and alteration are ongoing.
The northern Central Valley has a hot Mediterranean climate (Köppen climate classification Csa); the more southerly parts in rainshadow zones are dry enough to be Mediterranean steppe (BShs, as around Fresno) or even low-latitude desert (BWh, as in areas around Bakersfield). It is hot and dry during the summer and cool and damp in winter, when frequent ground fog known regionally as "tule fog" can obscure vision. Summer daytime temperatures approach 100 °F (38 °C), and common heat waves might bring temperatures exceeding 115 °F (46 °C). Mid-autumn to mid-spring comprises the rainy season — although during the late summer, southeasterly winds aloft can bring thunderstorms of tropical origin, mainly in the southern half of the San Joaquin Valley but occasionally to the Sacramento Valley. The northern half of the Central Valley receives greater precipitation than the semidesert southern half. Frost occurs at times in the winter months, but snow is extremely rare.
Tule fog (pron.: //) is a thick ground fog that settles along the length of the Great Central Valley. Tule fog forms during the late fall and winter (California's rainy season) after the first significant rainfall. The official time frame for tule fog to form is from November 1 to March 31. This phenomenon is named after the tule grass wetlands (tulares) of the Central Valley. Accidents caused by the tule fog are the leading cause of weather-related casualties in California.
Two major river systems drain and define the two parts of the Central Valley. The Sacramento River, along with its tributaries the Feather River and American River, flows southwards through the Sacramento Valley for about 447 miles (719 km). In the San Joaquin Valley, the San Joaquin River flows roughly northwest for 365 miles (587 km), picking up tributaries such as the Merced River, Tuolumne River, Stanislaus River and Mokelumne River.
In the south part of the San Joaquin Valley, the alluvial fan of the Kings River and another one from Coast Ranges streams have created a divide and resultantly the currently dry Tulare basin of the Central Valley, into which flow four major Sierra Nevada rivers, the Kings, Kaweah, Tule and Kern. This basin, usually endorheic, formerly filled during heavy snowmelt and spilled out into the San Joaquin River. Called Tulare Lake, it is usually dry nowadays because the rivers feeding it have been diverted for agricultural purposes.
The rivers of the Central Valley converge in the Sacramento-San Joaquin Delta, a complex network of marshy channels, distributaries and sloughs that wind around islands mainly used for agriculture. Here the freshwater of the rivers merges with tidewater, and eventually reach the Pacific Ocean after passing through Suisun Bay, San Pablo Bay, upper San Francisco Bay and finally the Golden Gate. Many of the islands now lie below sea level because of intensive agriculture, and have a high risk of flooding, which would cause salt water to rush back into the delta, especially when there is too little fresh water flowing in from the Valley.
The Sacramento River carries the vast majority of the runoff, about 24,000 cubic feet per second (680 m3/s), while the San Joaquin averages a comparatively mere 4,500 cubic feet per second (130 m3/s). Over 25 million people, living both in the valley and in other regions of the state, rely on the water carried by these rivers.
Runoff from the Sierra Nevada flow into the Central Valley provide some of the largest water resources of California. The Sacramento River is the second largest river to empty into the Pacific from the Continental United States, behind only the Columbia River and greater than the Colorado River. Combined with the fertile and expansive area of the Central Valley’s floor, the Central Valley is ideal for agriculture.
Today, the Central Valley is one of the most productive growing regions of the United States. But to enable this, water control was needed to prevent rivers from overflowing during the spring snowmelt while drying up in the summer and autumn. As a result, many large dams, including Shasta Dam, Oroville Dam, Folsom Dam, New Melones Dam, Don Pedro Dam, Friant Dam, Pine Flat Dam and Isabella Dam, were constructed on rivers entering the Central Valley, many part of the Central Valley Project. These dams have had a profound impact on the physical, economic, cultural, and ecological state of Central Valley: for example, enabling development of its vast agricultural resources but leading to the loss of the chinook salmon.
Post World War II demand for urban development in California’s urban areas, most notably the San Francisco Bay Area and the Los Angeles/Inland Empire/San Diego, required water resources to support it. Moreover, rapid development of agricultural in the southern Central Valley required far more water than available locally. The Feather River in the Sacramento Valley was looked to as a water source, leading to public financing of the California State Water Project. This transports water to the southern San Joaquin Valley and vast urban lands south of the Tehachapi Mountains.
Runoff from the Sacramento and San Joaquin Rivers is intercepted in the delta by the state Department of Water Resources through a series of massive pumps, which divert water into the California Aqueduct that runs south along the entire length of the San Joaquin Valley. In parallel, pumps operated by the Bureau of Reclamation divert water into the Delta Mendota Canal. The flow of the Sacramento River is further supplemented by a tunnel from the Trinity River (a tributary of the Klamath River, northwest of the Sacramento Valley) near Redding. Cities of the San Francisco Bay Area, also needing great amounts of water, built aqueducts from the Mokelumne River and Tuolumne River that run east to west across the middle part of the Central Valley.
Most lowlands of the Central Valley are prone to flooding, especially in the old Tulare Lake, Buena Vista Lake, and Kern Lake beds. The Kings, Kaweah, Tule and Kern rivers originally flowed into these seasonal lakes, which would expand each spring to flood large parts of the southern San Joaquin Valley. Due to the construction of farms, towns and infrastructure in these lakebeds while preventing them from flooding with levee systems, the risk of floods damaging properties increased greatly.
Major public works projects beginning in the 1930s sought to reduce the amount of snowmelt flooding by the building of large dams. In 2003, it was determined that Sacramento had both the least protection against and nearly the highest risk of flooding. Congress then granted a $220 million loan for upgrades in Sacramento County. Other counties in the valley that face flooding often are Yuba, Stanislaus, and San Joaquin.
Agriculture is the primary industry in most of the Central Valley. A notable exception to the predominance of agriculture has been the Sacramento area, where the large and stable workforce of government employees helped steer the economy away from agriculture. Despite state hiring cutbacks and the closure of several military bases, Sacramento's economy has continued to expand and diversify and now more closely resembles that of the nearby San Francisco Bay Area. Primary sources of population growth are people migrating from the San Francisco Bay Area seeking lower housing costs, as well as immigration from Asia, Central America, Mexico, Ukraine and the rest of the former Soviet Union.
The Central Valley is one of the world's most productive agricultural regions. More than 230 crops are grown there. On less than 1 percent of the total farmland in the United States, the Central Valley produces 8 percent of the nation’s agricultural output by value: 17 billion USD in 2002. Its agricultural productivity relies on irrigation from both surface water diversions and groundwater pumping from wells. About one-sixth of the irrigated land in the U.S. is in the Central Valley.
Virtually all non-tropical crops are grown in the Central Valley, which is the primary source for a number of food products throughout the United States, including tomatoes, almonds, grapes, cotton, apricots, and asparagus.
There are 6,000 almond growers that produce more than 600 million pounds a year, about 70 percent of the world's supply.
The top four counties in agricultural sales in the U.S. are in the Central Valley (2007 Data). They are Fresno County (#1 with $3.731 billion in sales), Tulare County (#2 with $3.335 billion), Kern County (#3 with $3.204), and Merced County (#4 with $2.330 billion.
Early farming was concentrated close to the Sacramento-San Joaquin Delta, where the water table was high year round and water transport more readily available, but subsequent irrigation projects have brought many more parts of the valley into productive use. For example, the Central Valley Project was formed in 1935 to redistribute and store water for agricultural and municipal purposes with dams and canals. The even larger California State Water Project was formed in the 1950s and construction continued throughout the following decade.
It was in the Central Valley, especially in and around Delano, that farm labor leader Cesar Chavez organized Mexican American grape pickers into a union in the 1960s, the National Farmworkers Association (NFWA), in order to improve their working conditions.
Since the 1980s, Bakersfield, Fresno, Porterville, Visalia, Tracy and Modesto have exploded in both area and population, as housing values along the coast increased. Many people from Los Angeles and the San Francisco Bay Area relocated to growing San Joaquin Valley suburbs in search of more affordable housing while retaining employment outside the Valley. This has led to traffic congestion between their Valley residences and their Bay Area employment with accompanying air pollution. Air pollution became a principal environmental and health concern as long ago as the 1960s, and resulted in the establishment of the California Air Resources Board in 1967.
Highways Interstate 5 and State Route 99 run, roughly parallel, north-south through the valley, meeting at its north and south ends. Interstate 80 crosses it northeast-southwest from Rocklin to Vacaville.
The state water project's Oroville Dam in the Sacramento Valley provides water and power for the California Aqueduct in the San Joaquin Valley. The aqueduct runs from Clifton Court Forebay in the Delta southwards across the Transverse Ranges. The federal (Central Valley Project) includes numerous facilities between Shasta Dam in the north to Bakersfield in the south. The California Independent System Operator, California-Oregon Transmission Project, and Western Area Power Administration have independent yet interconnected electrical transmission systems connecting the north and south ends of the Central Valley (examples include Path 15, Path 26, and Path 66).
BNSF (Burlington Northern Santa Fe Railway) and Union Pacific Railroad both have railway lines in the Central Valley. The BNSF Bakersfield Subdivision runs from Bakersfield to Calwa, four miles (6 km) south of Fresno. From Calwa the BNSF Stockton Subdivision continues to Port Chicago, west of Antioch. The Union Pacific Railroad Martinez Subdivision runs from Port Chicago through Martinez, Richmond and Emeryville to Oakland. The UP's Fresno Subdivision runs from Stockton to Sacramento and traffic passes through a large and historical yard in Roseville before heading to Oregon or Nevada. Amtrak operates six daily San Joaquins trains over these lines.
|California Central Valley grasslands||United States|
|Canadian aspen forests and parklands||Canada, United States|
|Central and Southern mixed grasslands||United States|
|Central forest-grasslands transition||United States|
|Central tall grasslands||United States|
|Columbia Plateau||United States|
|Edwards Plateau savanna||United States|
|Flint Hills tall grasslands||United States|
|Montana valley and foothill grasslands||United States|
|Nebraska Sand Hills mixed grasslands||United States|
|Northern mixed grasslands||Canada, United States|
|Northern short grasslands||Canada, United States|
|Northern tall grasslands||Canada, United States|
|Palouse grasslands||United States|
|Texas blackland prairies||United States|
|Western short grasslands||United States|
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