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The Salton Trough region from orbit. The Salton Trough is an active tectonic pull-apart basin, or graben. [1] It lies within the Imperial, Riverside, and San Diego counties of southeastern California and extends south of the Mexico–United States border into the state of Baja California.
The Salton Sink is the low point of an endorheic basin, a closed drainage system with no outflows to other bodies of water, in the Colorado Desert sub-region of the Sonoran Desert. The sink falls within the larger Salton Trough and separates the Coachella Valley from the Imperial Valley , which are also segments of the Salton Trough.
Before the Salton Sea began to form in 1905 — the result of both human and natural causes — the low-lying Salton Trough, which sits below sea level, cycled over thousands of years between ...
The Salton Sea is a shallow, landlocked, highly saline endorheic lake in Riverside and Imperial counties at the southern end of the U.S. state of California. It lies on the San Andreas Fault within the Salton Trough, which stretches to the Gulf of California in Mexico. The lake is about 15 by 35 miles (24 by 56 km) at its widest and longest.
The Salton Trough Fault runs parallel to San Andreas and could be absorbing some of the strain.
The Salton Trough Fault runs parallel to San Andreas and could be absorbing some of the strain. Skip to main content. 24/7 Help. For premium support please call: 800-290-4726 more ...
This is the category for the geologic features within the Salton Trough of Southern California, U.S..The Salton Trough is an active tectonic pull-apart basin, or graben.It lies within the Imperial, Riverside, and San Diego counties of southeastern California, United States and extends south of the Mexico–United States border into the state of Baja California, Mexico.
The delta is part of a larger geologic region called the Salton Trough. [2] Historically, the interaction of the river's flow and the ocean's tide created a dynamic environment, supporting freshwater, brackish, and saltwater species.
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