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The Salton Buttes lie on the southeastern shores of the Salton Sea, with their peaks at an elevation of −40 m (−130 ft), [1] in Imperial County, California. [2] [3] The towns of Niland and Calipatria lie northeast and southeast of the Salton Buttes, respectively, [4] and Palm Springs is 140 kilometers (90 mi) northwest. [5]
The Salton Buttes are volcanoes in the geothermal field of the same name. Mudpots and mud volcanoes are found on the eastern side of the Salton Sea, [116] including the mobile Niland Geyser. [117] The area is used for geothermal electricity generation, with plants located along the southeastern shore of the Salton Sea in Imperial County. [118 ...
Mackenzie, Muschalik & Broesche (2021) provided comments on the 2018 report in three separately authored sections. [4] Broesche believes that Yellowstone should be ranked higher due to the size of the volcano and the popularity of Yellowstone National Park, and Muschalik considers Mount Rainier to be just as dangerous as Kilauea due to its proximity to large population centers in Washington.
The rotting, polluted lake is poisoning residents and wildlife. Interest in the lithium deposits under the Salton Sea could bring attention to the environmental crisis.
An air of decline and strange beauty permeates the Salton Sea, the largest lake in California that is on the verge of drying up as it competes against coastal cities for dwindling water resources ...
The Salton Sea has long been fed by Colorado River water draining from the farmlands in the Imperial Valley. The lake has been shrinking since the early 2000s, when the local irrigation district ...
The Salton Buttes, located within the Salton Sea, are rhyolite lava domes within the basin which were active 10,300 (± 1000) years BP. [6] The Niland Geyser is one of dozens of mudpots and mud volcanoes in the Salton Trough but is the only one in the world known to have moved significantly, affecting the Union Pacific Railroad , California ...
The Salton Buttes on the south shore of the Salton Sea are on the north margin of the Brawley Seismic Zone and are linked to volcanic and geothermal activity within the zone. The Brawley Seismic Zone has been interpreted as an "onshore spreading center" which runs diagonally across the Salton Trough. [1]