The Mokelumne River near the State Highway 49 bridge above Pardee Reservoir
|Source||Confluence of North and Middle Forks|
|- location||Sierra Nevada, Amador/Calaveras Counties|
|- elevation||916 ft (279 m)|
|Mouth||Sacramento-San Joaquin Delta|
|- location||Walnut Grove, San Joaquin County|
|- elevation||0 ft (0 m)|
|Length||95 mi (153 km) |
|Basin||2,143 sq mi (5,550 km2) |
|Discharge||for near Mokelumne Hill, above Pardee Reservoir|
|- average||996 cu ft/s (28 m3/s) |
|- max||41,300 cu ft/s (1,169 m3/s)|
|- min||9 cu ft/s (0 m3/s)|
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. 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 river is colloquially divided into the Upper Mokelumne River, which stretches from the headwaters to Pardee Reservoir in the Sierra foothills, and the Lower Mokelumne River, which refers to the portion of the river below Camanche Dam. In its lower course the Mokelumne is used heavily for irrigation and also provides water for the east San Francisco Bay Area through the Mokelumne Aqueduct. Several major tributaries of the river have been developed for the generation of hydroelectric power.
The Mokelumne is formed by the confluence of several forks that rise in the central Sierra Nevada in the Stanislaus National Forest. The 62-mile (100 km) North Fork is the largest, originating at Highland Lakes at an elevation of 8,584 feet (2,616 m). From its source it flows north then west for 28 miles (45 km) to Salt Springs Reservoir. Below Salt Springs it receives the Bear River from the north and then passes through the smaller Tiger Creek Reservoir before joining with the Middle Fork southeast of Pine Grove. The lower portion of the North Fork defines the border between Amador and Calaveras Counties.
The 28-mile (45 km) Middle Fork rises at 6,800 feet (2,100 m) on the west side of Bailey Ridge, near Ganns. It flows generally west, past Wilseyville and West Point, to its confluence with the North Fork. The South Fork begins at an elevation of 6,380 feet (1,940 m) very near the head of the Middle Fork, and flows west 26 miles (42 km), roughly parallel and south of the Middle Fork, to join the Middle Fork about 1.3 miles (2.1 km) above the confluence of the North and Middle Forks.
The confluence of the North and Middle Forks forms the Mokelumne River proper. The main stem flows west-southwest past Mokelumne Hill into Pardee Reservoir, formed by the 345-foot (105 m)-high Pardee Dam. Below Pardee the river flows directly into Camanche Reservoir, formed by Camanche Dam. The entire stretch of the Mokelumne between the forks and a point just above Camanche Dam defines the Amador—Calaveras county line; below here, it flows westwards into San Joaquin County.
Below Camanche Dam the Mokelumne continues southwest out of the Sierra foothills past Lockeford and then turns northwest at Lodi, where the small Woodbridge Dam impounds the river, forming Lodi Lake. The river receives Dry Creek from the east near Thornton and shortly afterwards receives its major tributary, the Cosumnes River, from the northeast. At this point, the river has reached its northernmost point about 25 miles (40 km) south of Sacramento.
The river continues west then south into the Sacramento–San Joaquin River Delta where it becomes tidal and splits into a pair of distributaries, the North and South Mokelumne River (not to be confused with the North and South Forks in the Mokelumne headwaters) which together encircle the 9,100 acres (3,700 ha) of Staten Island. About 7 miles (11 km) downstream the branches rejoin, and two miles (3.2 km) below this point the Mokelumne flows into the San Joaquin River.
The Mokelumne River watershed drains 2,143 square miles (5,550 km2) in parts of Alpine, Amador, Calaveras, San Joaquin, and Sacramento Counties. Elevations range from sea level at the confluence with the San Joaquin River to 10,400 feet (3,200 m) at the crest of the Sierra Nevada in the headwaters of the North Fork.
The Mokelumne watershed divide borders the basins of the American River on the north, the Calaveras and Stanislaus rivers to the south, and the Carson River to the east. The American, Calaveras and Stanislaus rivers, like the Mokelumne, drain westwards into the Central Valley, while the Carson flows eastwards into the Great Basin. Drainage within the Mokelumne watershed generally occurs from east to west with all of the perennial streams originating in the Sierra Nevada.
The Mokelumne River and its headwater forks above Lodi drain the southernmost part of the basin. The part of the basin above Pardee Dam is referred to as the Upper Mokelumne River Basin and drains about 550 square miles (1,400 km2), or 25.7% of the total watershed. The Cosumnes River and its own North, Middle and South forks drain about 724 square miles (1,880 km2) in the northern part of the basin, or about 33.8% of the total watershed. Dry Creek, which itself is formed by four Sierra streams – Jackson, Sutter, Amador and Rancheria Creeks – drains most of the area between the upper Mokelumne and Cosumnes basins, or about 324 square miles (840 km2).
The upper watershed is situated principally in Alpine, Amador and Calaveras Counties and consists mostly of wilderness managed under various federal designations. Most of the Mokelumne and Cosumnes River headwaters lie within the Stanislaus and Eldorado National Forests. Much of the upper watershed is also protected under the 105,165-acre (42,559 ha) Mokelumne Wilderness. The Salt Springs State Game Refuge is located along the Mokelumne River near Salt Springs Reservoir. There are also significant private holdings in the upper basin including commercial timber land and protected watershed areas administered by the East Bay Municipal Utility District, which diverts urban and industrial water from Pardee Reservoir.
The lower watershed, mainly within San Joaquin and Sacramento Counties, is part of the rich agricultural region of the Central Valley. Grapes are the major crop grown in the Mokelumne River watershed; as of 2001, vineyards comprised 51% of the basin's farmland. Of the remaining land, 31% is used for livestock, 9% for orchards, and 8% for annual crops. About 90,000 acres (36,000 ha) in the lower basin are part of the Mokelumne River AVA.
The Mokelumne River basin was originally inhabited by Yokuts, Miwok, and Wintun Native American people. The lower (western) basin was the most densely populated, with numerous villages between the fringe of the Sierra foothills and the eastern edge of the Sacramento–San Joaquin Delta. This area is believed to have been predominantly Plains Miwok; various subgroups that lived in the Mokelumne River basin included the Mokellos, Lalas, and Machacos. The Miwoks called the river Wakalumitch, possibly meaning "big river".
The first European parties to explore the river were likely Spanish military expeditions in Alta California in the late 18th or early 19th century. The name Mokelumne was first recorded by Spanish missionary Narciso Durán as Muquelumnes in 1817. However it was not until 1830 when the first permanent European settlement was established on the Mokelumne River, at Happy Valley near present-day Mokelumne Hill, as an outpost for French fur trappers. John C. Frémont is credited with establishing the modern spelling of the name Mokelumne circa 1844.
During the California Gold Rush, the Mokelumne was a major gold-producing stream. The first person to discover gold in the Mokelumne was likely Charles Weber in 1848. Weber did not stay in the area for long; he moved on to the Coloma diggings on the South Fork American River before establishing a supply center at present-day Stockton, several miles south of the Mokelumne River. Most of the Gold Rush profits and trade on the Mokelumne River would end up passing through Stockton. Also in 1848, Samuel W. Pearsall found gold at Mokelumne Hill, which by 1850 grew into a boomtown of 15,000 people. 
The Mokelumne River is home to five notable whitewater kayaking runs: Fantasy Falls, Devil's Nose, Tiger Creek Dam, Ponderosa and Electra-Middle Bar. Fantasy Falls, a Class V+, 26-mile wilderness reach, runs from below Highway 4 in Alpine County to the backwaters of Salt Springs Reservoir. Devil's Nose, Class IV-V, runs 17 miles from Salt Springs Dams to Tiger Creek Powerhouse. Below Tiger Creek Dam is the Tiger Creek Dam Whitewater run, a scenic, 3 mile Class IV run. The Ponderosa run goes from Ponderosa Way to Electra Powerhouse. The westernmost run is Electra-Middle Bar, a 5+-mile Class II-III run. It begins just below the Electra Powerhouse and ends at the Middle Bar Bridge.
The Mokelumne is also a popular site for fishing, camping, water play, birding, picnics, gold panning, spring wildflower watching, and other activities. Electra Road, just east of Highway 49, is a popular place to run, walk, and enjoy the river. The large granite domes, Calaveras Dome and Hammer Dome, near Salt Springs Reservoir, are popular for technical rock climbing. Three campgrounds are also located near Salt Springs: Mokelumne River, White Azalea, and Moore Creek.
Above Salt Springs Reservoir, the Mokelumne Wilderness challenges those who seek a true wilderness experience. Backpacking in this federally designated wilderness area requires good back-country skills.
The first diversions of the Mokelumne were made during the California Gold Rush in the mid-1850s to provide water for placer and hydraulic mining. The first irrigation scheme was organized by a local collective, the Mokelumne Ditch and Irrigation Company, in 1875, but their dam was demolished by a flood and never rebuilt. The Woodbridge Canal and Irrigation Company was founded in 1891, and was somewhat more successful at tapping Mokelumne River water, but they were still hampered by damaging spring floods and lack of water in the dry season.
In 1929 the East Bay Municipal Utilities District (EBMUD) built the large Pardee Dam several miles upstream from Lodi and the irrigation diversion points on the Mokelumne River. Pardee is the primary storage facility and diversion point for the 91-mile (146 km) Mokelumne Aqueduct, which provides water to 35 municipalities in the eastern San Francisco Bay Area in Alameda and Contra Costa Counties. The first water deliveries to the Bay Area were made on June 23, 1929. The dam can store about 215,000 acre feet (0.265 km3) which is slightly over one quarter of the Mokelumne's annual flow. Through an agreement between EBMUD and local farmers, Pardee also stabilized the dry season water level in the lower Mokelumne, allowing much greater use of the river for agriculture.
As early as 1897, the Mokelumne was utilized for the generation of hydroelectric power at the Blue Lakes powerhouse, near the headwaters, to provide power for local communities. Pacific Gas and Electric (PG&E) began to develop the river for hydroelectricity in the late 1800s. In 1925, the Mokelumne hydroelectric project was licensed, and its major dam, Salt Springs, was completed on the North Fork of the Mokelumne in 1931. The project also includes two dams on the Bear River, the Tiger Creek Dam, and several smaller reservoirs in the Mokelumne headwaters. The project can provide a maximum output of 206 megawatts of electricity from four powerhouses.
In 1963 Camanche Dam was built directly below Pardee to capture additional Mokelumne River runoff. Its primary purpose is to ensure a dry-season water flow in the Mokelumne River so that more water can be retained in Pardee Reservoir for the Bay Area's use. Camanche forms the largest reservoir on the Mokelumne with a capacity of 431,000 acre feet (0.532 km3). The dam regulates releases from Pardee for local uses, primarily irrigation, and provides flood control for the lower Mokelumne River. The dam is also operated by EBMUD.
The Mokelumne River provides habitat for Pacific salmon and steelhead trout spawning runs. These fish were historically able to migrate up to near the present site of Pardee Dam where a natural waterfall prevented further progress. Between 1950 and 1997 the annual fall chinook salmon run has had an estimated average of 3434 fish. The construction of Camanche Dam has blocked access to several miles of the highest quality habitat formerly available to salmonids in the Mokelumne River. To compensate for the lost habitat, the Mokelumne River Fish Hatchery was built in 1964, a year after the completion of Camanche Dam.
The Cosumnes River, the Mokelumne's major tributary, is unique among Sierra rivers for its lack of large dams; however, irrigation diversions have also caused problems with fish migration on this river.
In its original 2040 long-range water plan, issued in 2009, the East Bay Municipal Utility District approved an optional expansion of Pardee Reservoir . The expansion would have flooded more than a mile of the river as well as unique cultural and historic sites. A broad coalition of local governments, conservation, recreation and fishery advocates opposed the reservoir expansion. Foothill Conservancy, Friends of the River  and California Sportfishing Protection Alliance  sued EBMUD in November 2009. In April 2011, Sacramento Superior Court Judge Timothy M. Frawley ruled in the groups' favor and voided the EBMUD plan. On December 5, 2011, East Bay Municipal Utility District announced that the soon-to-be released revised draft environmental impact report for its revised water plan would not recommend the controversial reservoir expansion. On April 24, 2012, the utility's board voted 7-0 to remove the Pardee expansion from its 2040 water plan.
- Mokelumne River AVA
- Mokelumne River Fish Hatchery
- Foothill Conservancy
- East Bay Municipal Utility District (EBMUD)
- Pardee Dam, Pardee Reservoir
- Camanche Dam, Camanche Reservoir
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- Bright, William (1998). 1500 California Place Names: their origin and meaning. University of California Press; Berkeley, California, 1998. ISBN 0-520-21271-1.
- United States Geological Survey. "United States Geological Survey Topographic Map: Dardanelles Cone, California quad". TopoQuest. Retrieved 2013-10-07.
- United States Geological Survey. "United States Geological Survey Topographic Map: Calaveras Dome, California quad". TopoQuest. Retrieved 2013-10-07.
- http://www.dfg.ca.gov/wildlife/gamerefuges/docs/Appendices.pdf p.6
- "Man's Use of the Mokelumne River". Society News Bulletin No. 3, Volume 2. San Joaquin County Historical Society. 1966-04-25. Retrieved 2013-10-06.
- "Pardee Reservoir". CalaverasHistory.org. 2010. Retrieved 2013-10-06.
- "Mokelumne River Project". Hydropower Reform Coalition. 2009. Retrieved 2013-10-07.
- Miyamoto, Joseph J.; Hartwell, Roger D. "Population Trends and Escapement Estimation of Mokelumne River Fall-run Chinook Salmon". Contributions to the Biology of Central Valley Salmonids. California Department of Fish and Wildlife. Retrieved 2013-10-07.
- Zito, Kelly (2011-05-12). "EBMUD set back by Pardee Reservoir ruling". The San Francisco Chronicle.
|Wikimedia Commons has media related to
- Lodi News-Sentinel: Searching for the Mokelumne Part II
- EPA: Lower Mokelumne watershed
- EBMUD's Mokelumne history
- Fantasy Falls kayaking video
- Amador Ledger-Dispatch: Mokelumne Frustrations Flow Toward EBMUD
- Indymedia: Chris Shutes of CSPA Slams Pardee Reservoir Expansion Project
- East Bay Express: Sierra Water Grab
- Mokelumne River Wild and Scenic video by Mikey Wier
- East Bay MUD 2040 Water Program