The Colorado River's geographic and historical role
The Colorado River drains the western slopes of the Rocky Mountains across a 1,450-mile course from its Rocky Mountain National Park headwaters to the Gulf of California (when sufficient water reaches it, which has become rare in the era of upstream diversions). The river crosses the Mojave Desert on its lower course, providing the only year-round water in a region that otherwise depends entirely on episodic flash flooding and underground aquifers. The river's value to all human inhabitants of the lower Colorado region — Mohave, Chemehuevi, Quechan, Cocopah indigenous peoples, Spanish missionaries, American mountain men, railroad surveyors, automobile travelers — has been incalculable.
Needles' specific position on the river was identified as a natural crossing point in the 1850s when Lt. Amiel Whipple's railroad survey expedition followed the 35th parallel west and identified the Needles vicinity as the appropriate location for a future transcontinental railroad bridge. The Atchison, Topeka & Santa Fe Railway built the first bridge across the Colorado at Needles in 1883; the railroad town that became Needles was founded that same year. The 1916 National Old Trails Highway (which became Route 66 in 1926) followed the same approximate alignment, crossing the river on a parallel automobile bridge.
The river's role in 20th-century Route 66 history was central. The Dust Bowl migration of the 1930s reached the Colorado at Needles as the principal crossing into California; the temperature differential between the Arizona desert (often 115°F in summer) and the cool river water provided the first relief many migrant families had experienced in days. The Steinbeck description in The Grapes of Wrath of the Joad family's Colorado crossing at Needles captured the geographic and emotional significance: the river marks the boundary between desert hardship and the promised California. The contemporary river-recreation industry — the swimming beaches, the boating, the fishing — continues this fundamental relief-from-desert function.
