The Goleta Slough is an area of estuary, tidal creeks, tidal marsh, and wetlands near Goleta, California, United States. It primarily consists of the filled and unfilled remnants of the historic inner Goleta Bay about west of Santa Barbara. The slough empties into the Pacific Ocean through an intermittently closed mouth at Goleta Beach County Park just east of the UCSB campus and Isla Vista. The slough drains the Goleta Valley and watershed, and receives the water of all of the major creeks in the Goleta area including the southern face of the Santa Ynez Mountains.
The Santa Barbara Airport has the largest border on the slough and contains the largest part of the slough. UCSB, Isla Vista, the City of Goleta and other unincorporated areas of the county, including the landward bluffs of More Mesa, surround and encompass the rest of the slough.
The Goleta Slough as it exists today is the result of two major historical events of the late 19th century and first half of the 20th century. The first was the heavy grazing by cattle on the surrounding foothills and mountainsides followed by wide-ranging grassfires, heavy rains in 1861/62, and flooding which caused so much erosion and deposition of sediment in the mouths of the creeks emptying into Goleta Bay that most of the bay became silt-filled salt marsh in just a couple of years. The second event was the conversion of the marsh and remaining bay into a military airbase during World War II. The fill material was obtained by reducing the rest of Mescalitan Island which provided the material to fill the airport and the surrounding area. The former location of Mescalitan Island now contains a sewage treatment plant.
While no longer having a regularly navigable mouth, nor depths in most places suitable for anything except canoes, kayaks, and very small boats, the slough remains a very important area of vital wetlands, salt marsh, and estuarian creeks.
"The Goleta Slough wetlands ... are fragmented along the coast from More Mesa to UCSB Storke Campus". The Goleta Slough Ecological Reserve is administered by the Calif. Dept. of Fish and Game. The Slough contains approximately of wetland habitat (including the ecological reserve and at Storke Campus). The approximate historic area was .
"The primary function of the Ecological Reserve is to provide habitat for wildlife and a setting for educational and research activities. Public utility and transportation corridors traverse the wetlands while airport runways, a sewage treatment plant, a power generation station, and light industrial facilities are constructed on filled portions of the marsh."
Historic use
"It is estimated that Native American peoples began inhabiting the area some 9,000 years ago. Early European explorers used the embayment as an anchorage for large ships until the 1860s. The severe winter storms of 1861/62 filled the embayment with sediment. Agricultural development in the slough began in the 1870s and the following decades saw the construction of berms, levees and roads to further facilitate agricultural development. In 1928 a landing strip was established in the northeastern portion of the slough, which was expanded in 1942-43 for construction of the Marine Corps Air Station, now the Municipal Airport."
The Marine station, known as Marine Corps Air Station Santa Barbara, became inactive in 1946.
Adjacent use
Goleta Slough is almost entirely surrounded by urban development, some of which extends into the wetlands. This includes the municipal airport to the north, the sewage treatment plant and the Southern California Gas Company's La Goleta Gas Field to the east, a public beach between the ocean and the slough, the campus of UC Santa Barbara to the south and west, and residential and light industrial operations to the north and west.
Adjacent historic use
Cattle ranching began in 1846 followed by agricultural development on the uplands around the slough. A whaling station was established in about 1870, asphaltum mining commenced in the 1890s, development of small farms expanded to cover the entire mesa in the 1920s, and rapid urbanization began in the 1940s.
Tidal influence
Extensive areas of the historic marsh below the high tide line are isolated from tidal influence by berms and dikes. Tidal flooding is limited to the south-central portion of the slough, extending into several of the major tributaries. Tidal amplitude in the upper reaches of the slough is diminished. During the summer months the tidal amplitude may become attenuated and eventually eliminated by progressive berming of the mouth. The beach berm is mechanically breached to maintain water quality in the slough.