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 Creek Basin opened in this area and the rest of Death Valley followed in stages. One of the last stages was the formation of Badwater Basin, which occurred by about 4 Ma. Data from gravimeters show that Death Valley's bedrock floor tilts down toward the east and is deepest under Badwater Basin; there is of fill under Badwater. By about 2 Ma Death Valley, Panamint Valley and their associated ranges were formed. Much of the extra local stretching in Death Valley that is responsible for its lower depth and wider valley floor is caused by "left" lateral strike-slip movement along