Laguna Salada (Spanish, "salty lagoon") is a vast dry lake some 10 meters below sea level in the Sonoran Desert of Baja California, 30 km (19 mi) southwest of Mexicali. This lake was called "Ha wi mək" in Cocopah language and "Ha-sa-ai" in Kumeyaay language. When dry, the flatness of the exposed lake bed sediments makes it a favoured location for recreational driving. It is also notorious for its dust storms when dry, usually the result of monsoonal thunderstorms during the summer. During times of significant rain the lagoon can fill completely with water, leaving the unpaved road along its west bank as the only means of traversing the area. Flanked by the Sierra de Los Cucapah and the Sierra de Juárez mountain ranges, the lake is approximately 60 km (37 mi) long and 17 km (11 mi) at its widest point.

The lake itself is located on the bottom of a shallow depression, a graben, which is linked to the San Andreas Fault, and the East Pacific Rise as part of the Laguna Salada Fault. This fault is connected to the Salton Trough fault which holds a similar depression, the Salton Sink. This sink is bigger than Laguna Salada and contains the Salton Sea. The 2010 Baja California earthquake occurred here.

In the 2012 Boeing 727 crash experiment an airplane was deliberately crashed into the Laguna Salada.

• Lake Cahuilla - prehistoric lake near Laguna Salada

• Carlos Fiesta. Ocean Odyssey. Palos Verdes Estates, California: Mexico Expo Travel. Retrieved 2009-09-17.
• Becky Dorsey (2003). "Pleistocene to Holocene Laguna Salada". University of Oregon. Archived from the original on 2008-05-13. Retrieved 2009-09-17.
• G Jimenez; et al. (2000). "Preliminary Study of the Fishery in Laguna Salada, Baja California". University of San Diego. Retrieved 2009-09-17.

• Satellite Photo (Google Maps)
• Vol. 44, Num. 1, pp. 103-111, A technical paper by Juan Contreras, Arturo Martín-Barajas and Juan Carlos Herguera on sedimentation of the LS-basin. Published in Geofísica Internacional (2005)

←