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
Death Valley National Park parallel strike-slip faults that perpendicularly bound the central extent of Death Valley. The result of this shearing action is additional extension in the central part of Death Valley which causes a slight widening and more subsidence there. Uplift of surrounding mountain ranges and subsidence of the valley floor are both occurring. The uplift on the Black Mountains is so fast that the alluvial fans (fan-shaped deposits at the mouth of canyons) there are small and steep compared to the huge alluvial fans coming off the Panamint Range. Fast uplift of a mountain range in an arid environment often does not