Edge Springs
From Wikipedia, the free encyclopedia
Edge Springs[1] is an alignment of the depressions (intermittent springs) along the southeastern edge of the Racetrack playa. The alignment parallels the toes of alluvial fans along the base of the steep mountain range.
References
- ↑ Kletetschka, Gunther; Hooke, Roger LeB.; Ryan, Andrew; Fercana, George; McKinney, Emerald; Schwebler, Kristopher P. (2013). "Sliding stones of Racetrack Playa, Death Valley, USA: The roles of rock thermal conductivity and fluctuating water levels". Geomorphology 195: 110–117. doi:10.1016/j.geomorph.2013.04.032.
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