MadSci Network: Environment & Ecology |
Death Valley is a large closed basin. If the tunnel you describe were constructed, water would flow into Death Valley until the level of the water in the valley reached the level of water in the ocean (sea level). Since the valley is closed (it has no drainage to the outside), any water that flowed in would stay in the valley and a long narrow salty lake would form. At the deepest point in Death Valley, known as Badwater, the water in this lake would be about 280 feet deep (Badwater is 282 feet below sea level). If you go to the National Park Service web site for Death Valley: http://www.nps.gov/deva/ and click on the link to maps and then download the PDF file that contains the park service map, you will be able to see what the outline of the lake would be. The map has a darker brown color for areas below sea level and it is those areas that would be flooded. The lake would cover less than half of the floor of the valley, so there would not be wall-to-wall water. The valley would hold a bigger lake, but to make it, you would have to pump water in, it would not flow in on its own. Initially, the new lake would probably only be a little saltier than sea water, and if the tunnel was left open, the saltiness would stay close to sea water. Any excess salt on the Death Valley end would tend to migrate toward the less salty ocean, equalizing the salt levels. If the tunnel were closed, the lake would get saltier and saltier as it gradually dried up. Eventually the lake would become salty enough that salt minerals would start to crystallize out of it, as they do today in the little lake that already exists at Badwater. Then the amount of salt in the water would stay about the same as in Great Salt Lake or the Dead Sea or other salty lakes. The Salton Sea in the Imperial Valley of California actually formed in a way similar to what you describe, except it wasn't done with a tunnel. There, a dike on a very large irigation canal broke and allowed fresh water to flood the deepest part of the valley. Evaporation has turned the lake salty over time. See http://www.smithsonianmag.si.edu/smithsonian/issues96/jun96/salton.html and http://www.desertusa.com/salton/salton.html I hope this answers your question. Dave Smith Associate Professor of Geology and Environmental Science La Salle University, Philadelphia, PA 19141
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