Saltwater intrusion in California  Seawater intrusion is either caused by groundwater extraction or increased in sea level. For every 1 foot of freshwater depression, sea-salty waters rises 40 feet as the cone of depression forms. Salinization of groundwater is one of the main water pollution ever produced by mankind or from natural processes. It degrades water quality to the point it passes acceptable drink water and irrigation standards. To this day, the State of California enforced several methodologies through technical innovation and scientific approach to combat saltwater intrusion in areas vulnerable to saltwater intrusion. Groundwater basin in Los Angeles County, California is considered as a vital resource both for agricultures and residential areas. For more than 40 years, Los Angeles County have managed to protect local groundwater basins from seawater intrusion. By injecting freshwater along coastal regions, Los Angeles County tends to create hydraulic gradients between freshwater and saltwater. This prevents saltwater to advance further inland . One critical factor affecting water supply in Los Angeles is population growth. As population growth increases in Los Angeles County, saltwater intrusion tends to advance further inland into Los Angeles groundwater aquifers. This occurs due to population growth, demanding an excess amount of freshwater from groundwater pumping wells. This sets an hydrologic condition for saltwater to follow the geomorphic pressure gradient produced landward. A cone of depression develops as a result through pumping wells operation to supply water for residential areas and agriculture. To combat saltwater intrusion, Los Angeles water districts decides to construct injection wells to form an hydraulic barrier, preventing advancement of saltwater intrusion in Los Angeles aquifers. Geologists, however, continue to study and survey Los Angeles County coastline because creating this hydraulic gradients is not fully efficient. To better understand saltwater intrusion in Los Angeles County, the U.S Geological Survey partners with Water Replenishment District of Southern California and Los Angeles County Department of Public Works to conduct a geological survey through using reflection seismology. This means that seismic profiles is essential to understand how sedimentation influence saltwater intrusion. The Alamitos Barrier Project is one of the three hydraulic barriers in Los Angeles County. It was created mainly to protect groundwater supplies from seawater intrusion. It is currently operated under Los Angeles County Flood Control District and the Orange County Water District. Other joint committees include the Water Replenishment District of Southern California who is responsible for supplying water to each hydraulic barrier and then the County of Los Angeles Department of Public Works who operates the projects on a daily basis. The effects of seawater intrusion took first noticed in 1956.