The San Diego Aqueduct, or San Diego Project, is a system of four aqueducts in the U.S. state of California, supplying about 90 percent of the water supply for the city of San Diego.
 The system comprises the First and Second San Diego Aqueducts, carrying water from the Colorado River west to reservoirs on the outskirts of San Diego.
 The 70 mi First Aqueduct consists of the pipelines 1 and 2, which run from the Colorado River Aqueduct near San Jacinto, California, to the San Vicente Reservoir, approximately 15 mi northeast of the city.
 Pipelines 3 and 4 make up the 94 mi Second Aqueduct.
 Together, these four pipelines have a capacity of 826 ft3/s .
 The smaller, 12.5 mi Fallbrook-Ocean Branch branches from the First Aqueduct into Morrow Reservoir.
 The La Mesa-Sweetwater Branch originates from the First Aqueduct, flowing into the Sweetwater Reservoir.
Centreport Aqueduct is a historic aqueduct located in the town of Brutus near Weedsport in Cayuga County, New York.
 The aqueduct was consrtructed in 1854-1857 as a part of the Weedsport section of the "Improved Erie Canal."
 The wood and stone aqueduct carried the Erie Canal over Cold Spring Brook near its juncture with North Brook.
 The aqueduct structure is approximately 125 feet in length, 125 feet in width, and 16 feet in height.
 Improvements were made to the aqueduct in 1895 as part of the "Nine Million Dollar Improvement."
 The aqueduct ceased being used after development of the New York State Barge Canal System in 1917.
 The aqueduct stone work is still intact and is the prime feature of a roadside park constructed by the New York State Department of Transportation in 1972 with the assistance of the Weedsport Lions Club.
The Inland Feeder is a 44 mi high capacity water conveyance system that connects the California State Water Project to the Colorado River Aqueduct and Diamond Valley Lake.
 The Metropolitan Water District of Southern California designed the system to increase Southern California's water supply reliability in the face of future weather pattern uncertainties, while minimizing the impact on the San Francisco Bay/Sacramento–San Joaquin River Delta environment in Northern California.
 The feeder takes advantage of large volumes of water when available from Northern California, depositing it in surface storage reservoirs, such as Diamond Valley Lake, and local groundwater basins for use during dry periods and emergencies.
 This improves the quality of Southern California drinking water by allowing more uniform blending of better quality water from the state project with Colorado River supplies, which has a higher mineral content.
Miramar Reservoir is a reservoir located in the Scripps Miramar Ranch community of San Diego, California.
 Owned, operated and maintained by the City of San Diego, the reservoir was completed in 1960 as part of the second San Diego Aqueduct project.
 Water flowing south to the reservoir originates from both the Colorado River Aqueduct and the California Aqueduct, brought into San Diego by the San Diego County Water Authority.
The Colorado River Aqueduct, or CRA, is a 242 mi water conveyance in Southern California in the United States, operated by the Metropolitan Water District of Southern California (MWD).
 The aqueduct impounds water from the Colorado River at Lake Havasu on the California-Arizona border west across the Mojave and Colorado deserts to the east side of the Santa Ana Mountains.
 It is one of the primary sources of drinking water for Southern California.
Tinkers Creek Aqueduct is an aqueduct that was constructed to bridge the Ohio and Erie Canal over Tinkers Creek near its confluence with the Cuyahoga River in Valley View, Ohio.
 It is a relatively rare surviving example of an Ohio and Erie Canal aqueduct.
 It was originally constructed in 1825-1827 by, and re-built due to flood damage in 1845 and 1905.
 Tinkers Creek Aqueduct was included in a National Historic Landmark district established in 1966, and it was separately listed on the National Register of Historic Places in 1979.
 The original Tinkers Creek Aqueduct was a wood plank, steel truss, and Ashlar-sandstone structure constructed in 1827, south of the present aqueduct's location.
 Cuyahoga River and Tinkers Creek flooding caused continual damage to the original aqueduct, so successive structures were built in 1845 and 1905 in the present location.
 Today, Tinkers Creek Aqueduct is the only aqueduct which remains of the four original aqueducts in the Cuyahoga Valley.
 Of Furnace Run Aqueduct, Mill Creek Aqueduct, Peninsula Aqueduct, and (?
 Yellow Creek ?)
 Aqueduct; Mill Creek Aqueduct, of newer construction, is the only aqueduct which still carries Ohio and Erie Canal water.
 After 102 years of flooding, weathering, and deterioration, Tinkers Creek Aqueduct was removed in 2007.
 The National Park Service is currently working on Phase II of the project to reconstruct it from newer materials.
The All-American Canal is an 80-mile (130 km) long aqueduct, located in southeastern California.
 It conveys water from the Colorado River into the Imperial Valley and to nine cities.
 It is the Imperial Valley's only water source, and replaced the Alamo Canal, which was located mostly in Mexico.
 The Imperial Dam, about 30 miles (48 km) northeast of Yuma, Arizona on the Colorado River, diverts water into the All-American Canal, which runs to just west of Calexico, California before its last branch heads mostly north into the Imperial Valley.
 Five smaller canals branching off the All American Canal move water into the Imperial Valley.
 These canal systems irrigate up to 630,000 acres (250,000 ha) of crop land and have made possible a greatly increased crop yield in this area, originally one of the driest on earth.
 It is the largest irrigation canal in the world, carrying a maximum of 26,155 cubic feet per second (740.6 m/s).
 Agricultural runoff from the All American Canal drains into the Salton Sea.
Water tunnels are tunnels (below-ground channels) used to transport water to areas with large populations or agriculture.
 They are frequently part of aqueducts.
 Some aqueducts, such as the Delaware Aqueduct are single long tunnels.
 In other cases, such as the San Jacinto tunnel on the Colorado River Aqueduct, water tunnels form parts of far longer aqueducts.
 In cases where the outflow of a water tunnel is into an existing stream or river flowing to the point of water use, the term aqueduct is less likely to be used, as with the Harold D. Roberts Tunnel from Dillon Reservoir to the North Fork South Platte River.
Eastside Canal is an irrigation canal in Kern County, California.
 It originates from a common diversion at Manor Street in Bakersfield, which also serves the Carrier Canal and Kern Island Canal.
 The common diversion originates from the Kern River, about 1 mi south of Gordon's Ferry.
 The canal terminates south of Bear Mountain Boulevard (SR 223), just west of Arvin.
Vidal Valley is a 20-mile (32 km) long valley in the far eastern Colorado Desert bordering the Colorado River.
 Most of the valley is in eastern San Bernardino County, California, but the outfall on the Colorado River is in northeast Riverside County.
 Vidal Valley forms the large border of the south side of the east-west block of the Whipple Mountains massif, the landform that forces the Colorado to flow southeast, then back southwest.
 The southeast exit of the valley into Parker Valley on the Colorado River skirts the north end of the Riverside Mountains (see photo).
 The Colorado River Aqueduct crosses the midpoint of the valley at Vidal Junction, California.
 The Vidal Valley also lies due east of the Danby Dry Lake landform.

Question: Are Colorado River Aqueduct and Eastside Canal both in the same state?
Answer: yes