| Santa Maria River | |
| Map: | Santa_maria_river_map.png |
| Map Size: | 300 |
| Subdivision Type1: | Country |
| Subdivision Name1: | United States |
| Subdivision Type2: | State |
| Subdivision Name2: | California |
| Subdivision Type5: | Cities |
| Subdivision Name5: | Santa Maria, Guadalupe |
| Length: | 24.4miles |
| Discharge1 Location: | Guadalupe |
| Discharge1 Min: | 0cuft/s |
| Discharge1 Avg: | 30.2cuft/s |
| Discharge1 Max: | 32800cuft/s |
| Source1: | Confluence of Sisquoc River and Cuyama River |
| Source1 Location: | South of Twitchell Reservoir |
| Source1 Coordinates: | 34.9031°N -120.3125°W |
| Source1 Elevation: | 354feet |
| Mouth: | Pacific Ocean |
| Mouth Location: | Guadalupe Dunes County Park |
| Mouth Coordinates: | 34.9708°N -120.6503°W |
| Mouth Elevation: | 0feet |
| Basin Size: | 1760sqmi |
Santa Maria River on the Central Coast of California, is formed at the confluence of the Sisquoc River and Cuyama River, just east of the city of Santa Maria, and flows [1] to its delta at the Pacific Ocean.[2]
The entire river defines the border between northern Santa Barbara County and southern San Luis Obispo County, up to the Sisquoc River, with a major bridge on Highway 101 passing over it. The Santa Maria River Fault is a tectonic fault that roughly corresponds with the course of the river.
There are no dams or lakes on the Santa Maria River itself, although Twitchell Reservoir is formed by a dam on the tributary Cuyama River. Twitchell Dam was built by the United States Bureau of Reclamation and provides flood control and groundwater recharge of the aquifer. The Sisquoc River is also free-flowing, and a National Wild and Scenic Rivers System.
During much of the year, the Santa Maria River has very little water, but it can swell greatly during winter storms.