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          At first glance, the plumbing of the San Luis Valley
         looks simple. It's easy to assume, as the Spanish did, that
         the whole thing drains south via the Rio Grande. 
         
         But the Valley actually comprises two drainages. There's
         the Rio Grande in the south, from Creede to Alamosa and then
         down to New Mexico. The upper Valley -- roughly, everything
         north of Hooper -- has no natural outlet. It's the "Closed
         Basin." Streams flow into Saguache Creek, which terminates
         in lakes near the Great Sand Dunes, where the water
         evaporates. 
         
         As if that isn't complication enough, there's a third
         dimension. The water in the surface gravels of the Closed
         Basin belongs to the "Unconfined Aquifer." About 150 feet
         below that is a layer of rather impermeable clay, and
         between the clay and the bedrock floor of the Valley is the
         "Confined Aquifer." 
         
         The San Luis Valley is part of a bigger geologic
         formation called the Rio Grande Rift, which extends south
         from the headwaters of the Arkansas River at Leadville to El
         Paso, Texas. Over millions of years, the flanking mountain
         ranges (Mosquito and Sangre de Cristo on the east, Sawatch
         and San Juan on the west) rose while the block of crust in
         between either stayed put or sank. 
         
         In the San Luis Valley, that block of bedrock could be as
         much as 30,000 feet below the surface. Between the surface
         and the bedrock is whatever washed off the mountains --
         everything from sand to boulders -- over the years. 
         
         The fill isn't monolithic; it has gaps between its solid
         matter. Since water runs from the mountains down into the
         Valley, those spaces get filled with water. Just how much
         water is a good question, but hydrologists say a fair
         estimate is 2 billion acre feet -- about as much water as
         the Colorado River carries in 150 years. 
         
         You don't need UFO sightings to decide that the Closed
         Basin is a strange place. On the surface, it's a chico-bush
         desert that gets less than a foot of precipitation each
         year. Beneath the surface, there could be as much water as
         in 75 Lake Powells. 
         
         That's the water that's at issue with the proposal by
         Gary Boyce and his Stockman's Water Company to drill wells
         into the Confined Aquifer and pump the water, up to 150,000
         acre feet a year, to the Front Range. 
         
         Boyce controls a fair-sized chunk of land -- about
         100,000 acres -- over the Closed Basin. One big question is
         whether he can operate wells there without injuring the
         others who pump water from the Closed Basin. 
         
         Among the current pumpers is the U.S. Bureau of
         Reclamation, which transferred 40,000 acre-feet in 1997 from
         the Closed Basin to the Rio Grande. This helps Colorado meet
         its obligations to New Mexico, Texas, and the Republic of
         Mexico, and it also means more water for irrigators along
         the Rio Grande. 
         
         So there really isn't a question about "should water be
         pumped out of the Closed Basin?" That was settled in 1985,
         when the Closed Basin Project began pumping water. The real
         question is how much water, which direction it goes, and who
         profits. 
         
         Boyce is about as popular in the Valley as anthrax or
         potato blight, and it's easy to say "save agriculture in the
         San Luis Valley." 
         
         I'm all for that. I like Valley potatoes and carrots and
         beer made from Valley barley. I cherish the Valley, all 100
         miles from that make-you-gasp view at Poncha Pass to
         Colorado's oldest business, the R&R Market in San
         Luis. 
         
         But there are a lot of other places in Colorado, from
         Ovid to Norwood, that I like, too. And which place will get
         trashed if Boyce is stopped? 
         
         Since 1990, Colorado has gained about 700,000 residents,
         which works out to an increased domestic demand for about
         150,000 acre-feet of water each year. If this population
         growth continues, mostly in developments along the Front
         Range, new domestic water supplies will have to be
         developed. 
         
         The water is available in Colorado; the question is where
         it will come from. It's very easy for a public official like
         Attorney General Ken Salazar to say that he will go to court
         to stop Gary Boyce, but what does he propose instead? 
         
         Will he also go to court to stop all those subdivisions
         between Fort Collins and Pueblo that cause the need for
         water development? 
         
         Or will some other venue get drained or drowned if the
         Closed Basin doesn't? Transfer some more South Platte water
         from agricultural to municipal, and put the farmers at Ovid
         out of business? Expand some deception like Windy Gap
         Reservoir (supposedly built to save agricultural supplies,
         and in fact used to cool a power plant), and see how many
         more trout we can infect with whirling disease? Drown more
         of Taylor Park with Union Park Reservoir? 
         
         The next time you hear "Boyce must be stopped," ask one
         question. And when you hear that "We can't stop people from
         moving to the Front Range," then ask "What basin do you
         propose to trash if it's not the Closed Basin?" 
         
         Let me know if you get an answer. 
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