Death Valley Railroad was scrapped around 1925 after the closure of the Terry lumber mill following a devastating fire. Death Valley Railroad The Death Valley Railroad (DVRR) was a narrow gauge railroad that operated in California's Death Valley to carry borax with the route running from Ryan, California to the mines at Ryan C., located just east of Death Valley National Park, to Death Valley Junction, a distance of approximately 20 miles. When mining operations at the Lila C. Mine were declining around 1914, Pacific Coast Borax Company began scouting the land outside Furnace Creek for richer borax deposits. Once they found some
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