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Mokelumne Aqueduct

Mokelumne Aqueduct is a engineering topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Mokelumne Aqueduct rather than just read about it. In short: The Mokelumne Aqueduct is a 95-mile (153 km) water conveyance system in central California, United States. The aqueduct is supplied by the Mokelumne River and provides water to 35 municipalities in the East Bay in the San Francisco Bay Area.

Mokelumne Aqueduct — main illustration
Mokelumne Aqueduct — illustration

Key takeaways

  • Mokelumne Aqueduct belongs to engineering; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Mokelumne Aqueduct to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Mokelumne Aqueduct from memory before moving on to harder problems.

Reference excerpt

The Mokelumne Aqueduct is a 95-mile (153 km) water conveyance system in central California, United States. The aqueduct is supplied by the Mokelumne River and provides water to 35 municipalities in the East Bay in the San Francisco Bay Area. The aqueduct and the associated dams, pipelines, treatment plants and hydroelectric system are owned and operated by the East Bay Municipal Utility District (EBMUD) and provide over 90 percent of the water used by the agency. 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 m3) per day, or 364,000 acre-feet (0.449 km3) per year, from the Mokelumne River. In addition, up to 98 million gallons (371,000 m3) per day or 110,000 acre-feet (0.14 km3) per year can be supplied via a branch from the Sacramento River. However, this supply is expected only to be used in the driest 35% of years.

History 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 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 (equivalent to $564 million in 2025) 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 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 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 the two waterways, was finally completed in 2009.

Specifications 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 km3), or about a 10-month supply. Camanche Reservoir, located directly below Pardee, has a storage capacity of 417,120 acre-feet (0.51451 km3) – twice the size of Pardee – but is not directly linked to 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 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 a combined storage capacity of 155,150 acre-feet (0.19137 km3). 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 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.

Issues The aqueduct 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 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 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 km3), 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 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.

See also Hetch Hetchy Project Water in California

References

External links The Mokelumne Aqueduct – Maven's Notebook

Illustrations

Mokelumne Aqueduct illustration

Worked examples

Example 1 — a first encounter with Mokelumne Aqueduct

Start with the simplest possible case. Write down what Mokelumne Aqueduct claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In engineering, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Mokelumne Aqueduct before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Mokelumne Aqueduct ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Mokelumne Aqueduct

In research
Mokelumne Aqueduct appears in engineering research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Mokelumne Aqueduct in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Mokelumne Aqueduct is common in secondary-school and first-year university syllabi. It links to neighbouring topics 1929 establishments in California, Aqueducts in California, Buildings and structures in Amador County, California, so understanding it makes those chapters shorter.
In everyday life
Look for Mokelumne Aqueduct outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Mokelumne Aqueduct in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Mokelumne Aqueduct means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Mokelumne Aqueduct out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Mokelumne Aqueduct in simple terms?

The Mokelumne Aqueduct is a 95-mile (153 km) water conveyance system in central California, United States. The aqueduct is supplied by the Mokelumne River and provides water to 35 municipalities in the East Bay in the San Francisco Bay Area.

Why does Mokelumne Aqueduct matter?

Because it connects several engineering ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Mokelumne Aqueduct?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Mokelumne Aqueduct.

Tags

  • 1929 establishments in California
  • Aqueducts in California
  • Buildings and structures in Amador County, California
  • Buildings and structures in Calaveras County, California
  • East Bay Municipal Utility District
  • Infrastructure completed in 1929
  • Interbasin transfer
  • Mokelumne River
  • San Joaquin Valley
  • Transportation buildings and structures in Alameda County, California
  • Transportation buildings and structures in Contra Costa County, California
  • Transportation buildings and structures in San Joaquin County, California

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