Calaveras River | |
---|---|
Location | |
Country | United States |
State | California |
Physical characteristics | |
Source | Confluence of North and South Forks |
• location | West of San Andreas |
• coordinates | 38°11′50″N120°43′12″W / 38.19722°N 120.72000°W [1] |
• elevation | 705 ft (215 m) |
Mouth | San Joaquin River |
• location | Near Stockton |
• coordinates | 37°58′01″N121°22′04″W / 37.96694°N 121.36778°W [1] |
Length | 51.9 mi (83.5 km) |
Basin size | 470 sq mi (1,200 km2) |
Discharge | |
• location | Jenny Lind, CA |
• average | 225 cu ft/s (6.4 m3/s) |
• minimum | 0 cu ft/s (0 m3/s) |
• maximum | 50,000 cu ft/s (1,400 m3/s) |
The Calaveras River is a river in the San Joaquin Valley of California.
It flows roughly southwest for 51.9 miles (83.5 km) from the confluence of its north and south forks in Calaveras County to its confluence with the San Joaquin River in the city of Stockton. [2]
In the past, it has been used for agriculture and irrigation, drinking water, and for recreational purposes. There have been many improvement projects on the Calaveras River to address its pollution and efficiency for local residents.
The Spanish word calaveras means "skulls." The river was said to have been named by Spanish explorer Gabriel Moraga in 1806 when he found many skulls of Native Americans along its banks. He believed they had either died of famine or been killed in tribal conflicts over hunting and fishing grounds.
Later, human remains were of the native Miwuk people killed by Spanish soldiers after they banded together to rise against Spanish missionaries. The Stanislaus River is named for Estanislau, a coastal Miwuk who escaped from Mission San Jose in the late 1830s. He is reported to have raised a small group of men with crude weapons, hiding in the foothills when the Spanish attacked. The Miwuk were quickly decimated by Spanish gunfire.
In 1836, John Marsh, Jose Noriega, and a party of men, went exploring in Northern California. They made camp along a river bed in the evening, and when they woke up the next morning, discovered that they had camped in the midst of a great quantity of skulls and bones. They also gave the river the appropriate name: Calaveras. [3] [4] [5]
New Hogan Lake is the only lake on the river. It is formed by New Hogan Dam, which was completed in 1963. The dam was built by the United States Army Corps of Engineers, primarily for flood control. The dam also provides drinking water, water for irrigation, hydroelectricity and recreation, including fishing, camping, swimming and water skiing.
Downstream from the Calaveras River is Mildred Island, a submerged island that also provides recreation such as fishing. [6]
The Mormon Slough, a distributary of the Calaveras, splits away about five miles east of Linden, California. In east Stockton, the Stockton Diverting Canal reconnects the Mormon Slough and the Calaveras. Downstream from this flood control channel, the often dry Mormon Slough continues on its southerly path, through downtown, to the Stockton Channel. The Calaveras makes a northerly arc, passing through farmland, orchards, and the University of the Pacific Stockton Campus, then alongside its namesake Brookside district, before flowing into the Deepwater Channel about three miles downriver from the Mormon Slough. Thus much of central Stockton, being completely surrounded by these waterways, is itself one of the many river islands which make up the San Joaquin Delta.
The Sacramento River meets the San Joaquin River in what is known as "The Delta" between Lodi, California, and the Carquinez Strait. Deltas are a geographical feature where river water flows and branches out into a larger, flatter area. However, the Sacramento-San Joaquin Delta is special because instead of splitting into multiple channels as water flows downstream, multiple channels are coming together. [7]
Hundreds of thousands of people are licensed to fish in the Bay Area and Delta regions, and 90% of people from low-income communities depend on fish from these rivers for food. [8] The Calaveras River has various species of fish that people catch, eat, and even some that are federally protected such as steelhead and rainbow trout. [9]
Since the California Gold Rush of the Mid-1800s, water running through the state has been introduced to mercury and other industrial chemicals. Per-and Polyfluoroakyl substances (PFAs) are man-made chemicals designed to make products stain and water resistant, but are of concern to the environment because of their difficulty to be decomposed. They are a class of chemicals known as forever chemicals that don’t get degraded well naturally and tend to stay in the environment including in the soil, air, and water. [10]
As the Calaveras River is used for agriculture, use of pesticides and herbicides also impact cleanliness of the water. Although present in small amounts, diazinon and chlorpyrifos are toxic to water life. Organophosphate pesticides are brought to the water by seasonal stormwater runoff. Poor drainage for soils and the amount of pesticides farmers are using affect the water to varying degrees. Since learning about the effect of pesticides, farmers have started to reduce the use of them either by switching to more organic options, diluting the chemicals, etc. [11]
There have been hazardous material spills in the past from maintenance issues such as sewers overflowing as well as recreational accidents such as fuel spills from boats and vehicles. [12]
Cyanobacteria (blue green algae) can grow anywhere in the world, but they are especially harmful when they produce toxins. Producing toxins, blocking sunlight by dense blooms and potentially using up all the oxygen in the water are many ways in which aquatic life is harmed. For the Calaveras River, the first algal bloom was found April 2019 in the New Hogan Reservoir but it was resolved by June 2019. [13]
Many improvement projects have been done in the past to better the Calaveras River for residents and its inhabitants.
In 2014, the Calaveras River was struggling to house natural wildlife because of its past diversions that spread the river water too thin. The U.S. Fish and Wildlife Service worked with residents to restore bridges and rebuild structures that would serve to connect residents on both sides of the river while not inhibiting the natural migration of fish species, the Caprini Crossing for example. [14] After these restorations, the river was able to produce more salmon and steelhead, considerable amounts for the relatively small system that is the Calaveras River.
In 2020, the Stockton East Water District planned out a program that would protect the threatened Central Valley steelhead, endangered Chinook salmon, and more natural wildlife. [15] They called this the 2020 Calaveras River Conservation Plan. It was the first habitat conservation plan in the Central Valley to be approved by the National Marine Fisheries Service. The program helped federally protected species and helped to maintain water quality of the Calaveras 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.
The Sacramento–San Joaquin River Delta, or California Delta, is an expansive inland river delta and estuary in Northern California. The delta is formed at the western edge of the Central Valley by the confluence of the Sacramento and San Joaquin rivers and lies just east of where the rivers enter Suisun Bay, which flows into San Francisco Bay, then the Pacific Ocean via San Pablo Bay. The Delta is recognized for protection by the California Bays and Estuaries Policy. Sacramento–San Joaquin Delta was designated a National Heritage Area on March 12, 2019. The city of Stockton is located on the San Joaquin River at the eastern edge of the delta. The total area of the Delta, including both land and water, is about 1,100 square miles (2,800 km2). Its population is around 500,000.
The Mokelumne River is a 95-mile (153 km)-long river in northern California in the United States. The river flows west from a rugged portion of the central Sierra Nevada into the Central Valley and ultimately the Sacramento–San Joaquin River Delta, where it empties into the San Joaquin River-Stockton Deepwater Shipping Channel. Together with its main tributary, the Cosumnes River, the Mokelumne drains 2,143 square miles (5,550 km2) in parts of five California counties. Measured to its farthest source at the head of the North Fork, the river stretches for 157 miles (253 km).
The Yokuts are an ethnic group of Native Americans native to central California. Before European contact, the Yokuts consisted of up to 60 tribes speaking several related languages. Yokuts is both plural and singular; Yokut, while common, is erroneous. 'Yokut' should only be used when referring specifically to the Tachi Yokut Tribe of Lemoore. Some of their descendants prefer to refer to themselves by their respective tribal names; they reject the term Yokuts, saying that it is an exonym invented by English-speaking settlers and historians. Conventional sub-groupings include the Foothill Yokuts, Northern Valley Yokuts, and Southern Valley Yokuts.
The delta smelt is an endangered slender-bodied smelt, about 5 to 7 cm long, in the family Osmeridae. Endemic to the upper Sacramento-San Joaquin Estuary of California, it mainly inhabits the freshwater-saltwater mixing zone of the estuary, except during its spawning season, when it migrates upstream to fresh water following winter "first flush" flow events. It functions as an indicator species for the overall health of the Delta's ecosystem.Delta Smelt are usually found at temperatures of less than 25°C and prefer temperatures of around 20°C. They are euryhaline but occur mostly at salinities of 0–7 practical salinity units.
The splittail, also called Sacramento splittail, is a cyprinid fish native to the low-elevation waters of the Central Valley in California. It was first described by William O. Ayres in 1854. It is the sole living member of its genus, the Clear Lake splittail P. ciscoides having become extinct in the 1970s.
Alameda Creek is a large perennial stream in the San Francisco Bay Area. The creek runs for 45 miles (72 km) from a lake northeast of Packard Ridge to the eastern shore of San Francisco Bay by way of Niles Canyon and a flood control channel. Along its course, Alameda Creek provides wildlife habitat, water supply, a conduit for flood waters, opportunities for recreation, and a host of aesthetic and environmental values. The creek and three major reservoirs in the watershed are used as water supply by the San Francisco Public Utilities Commission, Alameda County Water District and Zone 7 Water Agency. Within the watershed can be found some of the highest peaks and tallest waterfall in the East Bay, over a dozen regional parks, and notable natural landmarks such as the cascades at Little Yosemite and the wildflower-strewn grasslands and oak savannahs of the Sunol Regional Wilderness.
The Peripheral Canal was a series of proposals starting in the 1940s to divert water from California's Sacramento River, around the periphery of the San Joaquin-Sacramento River Delta, to uses farther south. The canal would have attempted to resolve a problem with the quality of water pumped south. Pumps create such a powerful suction that the boundary between freshwater to saltwater has shifted inland, negatively affecting the environment. The pumps have increased by 5 to 7 million acre-feet the amount of water exported each year to the Central Valley and Southern California. However, the peripheral canal as proposed would have reduced the overall freshwater flow into the Delta and move the freshwater-saltwater interface further inland, causing damage to Delta agriculture and ecosystems.
Sherman Island is an island in the Sacramento-San Joaquin River Delta at the confluence of the two rivers in Sacramento County, California, 1.2 miles (1.9 km) northeast of Antioch. The 5,500 ha island, mostly managed by Reclamation District 341, is the meeting point of Sacramento, Solano, and Contra Costa Counties, and is bordered on the north and northwest by the Sacramento River, on the northeast by Three Mile Slough, and on the east, and south west by the San Joaquin River. Sherman Island is a widely known kite and windsurfing area.
Bouldin Island is an island in the Sacramento-San Joaquin River Delta, 20 kilometers (12 mi) northwest of Stockton on the Stockton Deepwater Shipping Channel. It is in San Joaquin County, and managed by Reclamation District 756. The island is owned by the Metropolitan Water District of Southern California.
Marsh Creek is a stream in east Contra Costa County, California in Northern California which rises on the eastern side of Mount Diablo and flows 30 miles (48 km) to the Sacramento–San Joaquin River Delta at Oakley, California, near Big Break Regional Shoreline. The creek flows through Marsh Creek State Park (California), where water is impounded to form Marsh Creek Reservoir, then through the city of Brentwood, California.
The Delta Cross Channel is a facility in California's Sacramento-San Joaquin Delta that diverts water from the Sacramento River. The facility was built in 1951 in Walnut Grove, California.
Winter Island is a 453-acre (183 ha) island in Suisun Bay, in the western Sacramento-San Joaquin River Delta. It is north of Pittsburg, separated from Browns Island to the west by a slough. It was private property, and contained one house. It is used as a duck hunting area, a wetland, and a dredging disposal area. In 2016 Winter Island was purchased by the California Department of Water Resources in order to restore the island as a tidal marsh. Winter Island is part of Contra Costa County, and managed by Reclamation District 2122. It is shown, labeled "Ruckels Island", on an 1850 survey map of the San Francisco Bay area made by Cadwalader Ringgold and an 1854 map of the area by Henry Lange.
Stockton Channel is a waterway in California's Sacramento–San Joaquin River Delta. It runs 2.5 miles from the San Joaquin River-Stockton Deepwater Shipping Channel at the Port of Stockton to McLeod Lake in Downtown Stockton. The Stockton Channel is contained by levees, with Miners Levee is on the north side and Tuleburg Levee on the south side. The Mormon Slough branches off the Stockton Channel to the Southeast. The Smith Channel runs parallel to the north of the Stockton Channel. Interstate 5 crosses the Channel at its midpoint.
Stockton Deepwater Shipping Channel, also called the Baldwin-Stockton Deepwater Shipping Channel or Stockton Deep Water Channel, is a manmade deepwater water channel that runs from Suisun Bay and the Sacramento River - Sacramento Deep Water Ship Channel to the Port of Stockton and the Stockton Channel in California. The Stockton Ship Channel is 41 mi (66 km) long and about 37 ft (11 m) deep, allowing up to Panama Canal size ocean ships access to the Port of Stockton at the City of Stockton. The Stockton Deepwater Shipping Channel is part of the vast Sacramento–San Joaquin River Delta that has a connection to the Pacific Ocean. Stockton Deepwater Shipping Channel is also called the lower San Joaquin River.
Headreach Island is a small island in the Sacramento–San Joaquin River Delta, in northern California. A naturally-formed island existing in a complex with Tule Island to the southeast and Fern Island to the northwest, it was used for farming as late as the 1920s. While several proposals for real estate development on the island were made in the late 20th century, it now consists mostly of marsh and submerged land. Black rails live on the island.
Hog Island is an island in the San Joaquin River, and is one of many islands which constitute the Sacramento–San Joaquin River Delta. It was used for agriculture in the early 20th century, but has now mostly become marsh or submerged land; it remains a spot for fishing, particularly channel and blue catfish.
Chain Island is an island in Suisun Bay, downstream of the Sacramento–San Joaquin River Delta in northern California, and the westernmost piece of land in Sacramento County. In the late 1800s, it was considered an "obstruction to navigation" on the Sacramento River. As it was built up significantly from hydraulic mining tailings upstream on the river, plans were made in the early 20th century to remove it and recoup costs by mining the debris. However, this never happened; it was sold by the California State Lands Commission to a private individual in 1959, who listed it for sale the next year. In April 2016, the deed for the island was transferred; as of December 2022, Sacramento County assesses its land value at $18,622.
Sacramento–San Joaquin is a freshwater ecoregion in California. It includes the Sacramento and San Joaquin river systems of California's Central Valley, which converge in the inland Sacramento–San Joaquin Delta. It also includes the mostly-closed Tulare Lake basin in the southern Central Valley, the rivers and streams that empty into San Francisco Bay, and the Pajaro and Salinas river systems of Central California which empty into Monterey Bay.
San Felipe Lake is a perennial natural lake located in the southern Santa Clara Valley, almost wholly in northern San Benito County with its western edge on the border with Santa Clara County, California. The lake is a critical wetland, rare plant, and wildlife resource in need of additional conservation and enhancement.