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Coring to Study Sediment Dispersal in Lake Mead, Nevada
Sediment and sediment-hosted pollutant dispersal in the lake are of interest to several State and Federal agencies responsible for its management. Interest is peaking owing to a significant drop (more than 40 ft) in lake level over the past 2 years, causing shallow-water deltaic deposits to be remobilized and distributed deeper into the lake. Although some of the classic work on density flows and turbidities was already done in Lake Mead, systematic geophysical mapping and companion ground-truth sampling had not been conducted before this cooperative program. Participants in the fieldwork included Ken Parolski, VeeAnn Cross, and Dave Twichell (USGS, Woods Hole, MA), Keith Ludwig (USGS, St. Petersburg, FL), Mark Rudin, Brenda Buck, and Robyn Howley (UNLV), and Tom Hixon (St. Thomas University, Minneapolis, MN). The field program was conducted during a reportedly cool spring, when daily high temperatures reached only 98-112° F.
Cores were collected only in the western part of Lake Mead, with the primary focus on Las Vegas Bay. Runoff from the city of Las Vegas enters Las Vegas Bay, and geophysical data suggest that sediment associated with runoff is transported down the axial valley of this bay (as density flows) to the deep part of the lake. Some of the cores were split before the end of the field program. All of these cores penetrated the post-impoundment sediment (deposited after the lake was created) and as much as 1 m of the underlying pre-impoundment gravel. Post-impoundment sediment thickness in the cores closely matched the thickness inferred from seismic data. Graded silt and sand beds in the post-impoundment sediment indicate that density flows are actively transporting sandy sediment beyond the delta and significant distances into the lake.
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in this issue:
Lake Mead Sediment Study Williams' Presentation on Videotape Caribbean Climate Change Conference Scientists Speak in Reston & D.C. Regional Geologist Visits WHFC Award-Winning Student Volunteer
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