The beginnings of the mighty Colorado River on the west slope of Rocky Mountain National Park are humble. A large marsh creates a small trickle of a stream at La Poudre Pass, and thus begins the long, labyrinthine 1,450-mile journey of one of America’s great waterways.
Several miles later, in Rocky Mountain National Park’s Kawuneeche Valley, the Colorado River Trail allows hikers to walk along its course and, during low water, even jump across it. This valley is where the nascent river falls prey to its first diversion — 30 percent of its water is taken before it reaches the stream to irrigate distant fields.
The Never Summer Mountains tower over the the valley to the west. Cut across the face of these glacier-etched peaks is the Grand Ditch, an incision visible just above the timber line. The ditch collects water as the snow melts and, because it is higher in elevation than La Poudre Pass, funnels it 14 miles back across the Continental Divide, where it empties it into the headwaters of the Cache La Poudre River, which flows on to alfalfa and row crop farmers in eastern Colorado. Hand dug in the late 19th century with shovels and picks by Japanese crews, it was the first trans-basin diversion of the Colorado.
Many more trans-basin diversions of water from the west side of the divide to the east would follow. That’s because 80 percent of the water that falls as snow in the Rockies here drains to the west, while 80 percent of the population resides on the east side of the divide.
Read more at Yale Environment 360
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