Saratoga Springs (Death Valley) the successful talc mines in the nearby Ibex Hills. Except for two partially collapsed stone structures, little evidence remains of human habitation at the spring. A dirt road provides access to an overlook of the area, but human entry into the wetland itself is prohibited in order to the protect the sensitive habitat. Saratoga Springs (Death Valley) Saratoga Springs is a desert oasis located in southern Death Valley National Park in California. The wetland lies at the southern tip of the Ibex Hills, on the floor of Death Valley and just northeast of the Amargosa River. Several springs overflow into
Geology of the Death Valley area laterally over the surface, laying down cobbles, sand, and mud. Outcrops of the resulting conglomerates, sandstone, and mudstone of the Titus Canyon Formation can be observed in road cuts at Daylight Pass on Daylight Pass Road, which becomes State Route 374 a short distance from the pass. Several other similar formations were also laid down. Large volcanic eruptions, originating near the Nevada Test Site, covered the Death Valley area and much of Nevada in thick sequences of silica-rich ash 27 million years ago. The ash has a rhyolitic composition, which is the volcanic equivalent of the plutonic rock granite; it