Big Lagoon (California)

Big Lagoon is similar to other coastal features of northern California including Humboldt Bay to the south and Lake Earl to the north; an alluvial plain is surrounded by steep uplands. Hills adjacent to Big Lagoon have been identified as the Franciscan Assemblage along the eastern shore and Pleistocene dune sandstone to the south. The plain may support fresh water wetlands or Sitka Spruce forests following uplift events and salt marsh or inundated shellfish beds following subsidence events. At the present lagoon level, the sand bar normally separates the lagoon from the ocean during summer months. Winter precipitation may raise the water level in the lagoon a few meters above sea level. Hydrostatic pressure and storm surf may then breach the sand bar allowing the lagoon to drain into the sea and then receive tidal inflow until wave action reforms the bar. ==History==

Roosevelt elk graze the wetlands south of the lagoon and may sometimes be seen where U.S. Route 101 crosses the lagoon. Hammond Lumber Company Plant Three included 20th century company housing and a sawmill log pond built where Maple Creek enters the south end of Big Lagoon. The coastal portion of Big Lagoon was used as an aerial rocket range by the United States Navy during World War II. Canoe access to Big Lagoon is available from a park on the south shore near the community of Big Lagoon and Big Lagoon Rancheria. The deaths of 14 dogs after going swimming have occurred in the last twenty years due to cyanobacteria in blue-green algae on the Big Lagoon, South Fork Eel River or the Van Duzen River during times of warm weather and low water flow. ==See also==