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"The Colorado River is one of the most sediment-laden streams in North America," Dohrenwend said. "Deltas on the Colorado River, coming into Lake Powell on the north, and on the San Juan River, coming into Lake Powell on the southeast, are today more than 30 miles long, and advance at an average rate of about a mile a year."
During the past 35 to 40 years, sediment at the confluence of the Colorado and Dirty Devil rivers, just upstream from Hite Marina and the present delta front, has grown to about 185 feet thick. Sediments from the recently exposed delta have been eroding at a very rapid rate, Dohrenwend observed. "In the past several months, the delta front has advanced almost a mile and a half," he said.
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The important issue, beyond the immediate fate of Hite Marina, is "where does all of this sediment go when it reaches the lake?" Dohrenwend said. Scientists and engineers realized 60 years ago that when a sediment-laden river enters a reservoir, the river water deposits much of its sediment at the upstream end, but also creates a 'density' current that flows along the bottom of the reservoir, dumping sediments all the way along to the face of the dam. "There is significant sedimentation at the Glen Canyon dam face even now," Dohrenwend said. Added to that, the Colorado River is a desert river with a volume that fluctuates widely, so the reservoir volumes also fluctuate widely, and that further complicates how sediments are deposited behind the dams, he said.
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"My point is, who is studying this?" Dohrenwend said. "It's a time-sensitive problem that needs to be studied. We need to study it, if only to learn more about how sediment will be deposited in major reservoirs so that we can more accurately forecast the useful life of these reservoirs. Or perhaps we might develop some ideas of what we might do, or what future generations might do, when it's time to decommission these things."
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http://uanews.org/cgi-bin/WebObjects/UANews.woa/wa/MainStoryDetails?ArticleID=7290At the time of publication the delta front had moved abot 1.5 miles downstream in a couple of months. That was in spring, 2003. Now (August 2004), the water level is another 35 feet lower than when Dohrenwend wrote this article.
Sedimentation is about as unsexy a problem as I can imagine, but in large measure it (along with drought) is going to define life in the coming century for millions of Americans living west of the 100th meridian.