The Ballona Creek watershed totals about . According to a 1948 report in the Venice
Evening Vanguard, "The total area drained by Ballona Creek consists of square miles of coastal plain and of foothills and plain range from sea level to and in the mountains from to . The average gradient of the valley floor is about and that of the canyon channels is about . The longest distance at any given time taken by the water in this drainage system is ." Before most of Los Angeles' watercourses were buried underground, Ballona Creek drained the whole of the west Los Angeles region and fed directly from a chain of and lakes that stretched from the
Hollywood Hills to the
Baldwin Hills. Land use in the watershed is 64% residential, 17% open space, 8% commercial, and 4% industrial. Natural channels remain at some of the headwaters of Ballona Creek tributaries, while the lower portion of the stream is encased in concrete channels either rectangular in the east or trapezoidal toward the west; to the west of Centinela Avenue, the bottom of the creek is unpaved and subject to
tidal influence.
Tributaries and drains • Brush Canyon Creek – an intermittent stream, about long, begins in what everyone calls
Bronson Canyon, roughly between the
Hollywood Reservoir and
Mount Hollywood, travels south, passes under
Wilshire Country Club, enters the Arroyo de los Jardines, (also known as Longwood Stream and El Río del Jardín de las Flores) through the
Brookside neighborhood of Hancock Park • Arroyo de la Sacatela –
Shakespeare Bridge in
Franklin Hills–
Los Feliz was built to cross this watercourse, which fed
Bimini Slough in what is now Koreatown; infrastructure built 1929 drained a area, which among other things permitted development of land below
Santa Monica Boulevard between Mariposa and Kenmore • Ferndell in
Griffith Park •
Laurel Canyon Creek – an intermittent stream, about long, draining a small area in the
Santa Monica Mountains and flowing southward into Ballona Creek through
La Brea Rancho (vicinity of
Fairfax/
Hancock Park) •
Nichols Canyon Creek – an intermittent stream, long, draining a small area in the eastern part of the Santa Monica Mountains and discharging southward into Ballona Creek through La Brea Rancho • Arroyo de Los Jardines – According to a 1937 news report, "Nearly all of the flood waters from Hollywood business and residential district eventually find their way into the Arroyo de Los Jardines channel, concentrating near
Wilshire Boulevard and
La Brea Avenue. The county flood control district has prepared a $361,000 plan to build a new and adequate channel for the Arroyo de Los Jardines between Wilshire and Ballona Creek. The water will pour into Ballona Creek, two blocks west of La Brea Avenue. Water from Nichols Canyon also reaches Ballona Creek by way of the Arroyo de Los Jardines." • Dry Canyon Creek (Arroyo Seco?) – an intermittent stream, about long, draining a small area in the Santa Monica Mountains and flowing southeastward to
San Jose de Buenos Ayres Rancho (vicinity of
Westwood/
Holmby Hills) • Benedict Canyon Channel – constructed by the U.S. Army Corps of Engineers in 1961–62 •
Benedict Canyon Creek – an intermittent stream, long, draining a small area in the Santa Monica Mountains, and flowing southward into
Rodeo de las Aguas Rancho •
Coldwater Canyon Creek – an intermittent stream, long, draining a small area in the Santa Monica Mountains, and flowing southward and southeastward into Rodeo de las Aguas Rancho. Near the mouth of its canyon it receives streams draining
Franklin and Higgins canyons. • Higgins Canyon Creek – an intermittent stream, about long • Franklin Canyon Creek – an intermittent stream, about long, draining a small area in the Santa Monica Mountains and flowing southward to its junction with Coldwater Canyon Creek • Peavine Canyon Creek – an intermittent stream, about long, draining a small area in the Santa Monica Mountains and flowing southward to the mouth of its canyon near what is now Beverly Hills – essentially San Ysidro Drive • Sepulveda Canyon Creek – an intermittent stream, about long, draining a small area in the Santa Monica Mountains and flowing southeastward toward Ballona Creek; sinks north of the
VA in
Brentwood • Sawtelle-Westwood Channel, plan in 1934 was a "large conduit from Pico Boulevard to Venice Boulevard and eventually southward to Ballona Channel"; construction began 1956 • Sepulveda Channel – sometimes called the Mar Vista drain, initial plans in 1927 were for it to begin at Midvale and Pico •
Stone Canyon Creek – an intermittent stream, about long, draining a small area in the Santa Monica Mountains and flowing southward into Westwood – still accessible on
UCLA campus between
Sunset Boulevard and the Anderson School of Management • Brown Canyon Creek – an intermittent stream, about long, draining a small area in the Santa Monica Mountains, and flowing east of south to a point near
Palms, where its waters would sink or might feed into Ballona during particularly wet yearscreek recently
daylighted as part of the
Westwood Greenway adjacent to
Westwood/Rancho Park station • Centinela Creek Channel – ancient waterway, channelized in mid-20th century; rises near
Centinela Park (once the site of
Centinela Springs); surfaces near La Tijera Boulevard, The West Adams storm drain was built in 1925 and started at
Vermont Avenue – a segment of the "West Adams sewer" under construction in 1926 presented "unusual engineering difficulties, it is said, because water is found within a few feet of the surface in almost the entire territory, which extends from Angeles Mesa drive
[Crenshaw Boulevard] to the end of West Adams street and on either side of that street from Washington to Jefferson streets". • Rexford Channel • North Culver Drain Ballona Wetlands, Del Rey Lagoon, Ballona Lagoon, and Oxford Basin are connected to the Ballona estuary through
tide gates. The Ballona watershed is estimated to have roughly 35% impervious surface, which affects rainwater infiltration and groundwater recharge. A 2011 study determined that as little as 2% of Ballona's water may now come from underground springs, meaning that 98% of the creek's flow consists of various forms of runoff throughout the watershed. == Crossings ==