Death Valley Junction, California Death Valley Railroad was established in 1914, it used of tracks belonging to the Tonopah and Tidewater Railroad east-southeast of Death Valley Junction to Horton. Local wired telephones were manual telephone service until the 1980s. To reach a phone in Death Valley Junction when the area was under manual service required dialing the operator and asking for "Death Valley Junction, California, Toll Station" (and the one-digit number). Placing an outbound call required lifting the receiver and waiting for an operator. The operator who answered was in Los Angeles (over 150 miles away). Death Valley Junction is now in area codes
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