Death Valley '49ers group—the Jayhawkers—wanted to stay with the original plan of traveling west. The group eventually split and went their separate ways but they both were to have two things in common. They were both saved from dying of thirst by a snow storm and they both ended up meeting again at Ash Meadows in the Amargosa Desert of the Amargosa Valley located east of Death Valley. From here they continued on, following the Amargosa River bed to present-day Death Valley Junction, California, and then along the same route followed by current California State Route 190 past the Funeral Mountains. On Christmas
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