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| 23-1 | 12 | THE INFLUENCE OF TRAVERTINE DAM STRUCTURES ON VALLEY MORPHOLOGY AT FOSSIL CREEK, ARIZONA: NILES, John H.1, SKLAR, Leonard S.2, and FULLER, Brian M.2, (1) Geosciences, San Francisco State University, 1600 Holloway Avenue, San Francisco, CA 94132, niles@sfsu.edu, (2) Geosciences, San Francisco State Univ, San Francisco, CA 94132 |
| 23-2 | 13 | INCISION HISTORY OF THE COLORADO RIVER IN WESTERN COLORADO AND ITS IMPLICATIONS FOR CLIMATE VS. TECTONIC DRIVEN INCISION: BROWN, Elizabeth, Dept. of Geology, Occidental College, 1600 Campus Rd, Los Angeles, CA 90041, ebrown@oxy.edu, GRANT, Daniel, Dept. of Geology, Whitman College, Walla Walla, WA 99362, PENDLETON, Matthew, Department of Geological Sciences, University of Minnesota Duluth, Duluth, MN 55812, and ASLAN, Andres, Department of Physical and Environmental Science, Mesa State College, PO Box 2647, Grand Junction, CO 81501 |
| 23-3 | 14 | NEW INSIGHTS ON THE PLUVIAL HISTORY OF LAKE MANLY AND TECTONIC DEVELOPMENT OF SOUTHERN DEATH VALLEY RECORDED IN PLIOCENE-TO-RECENT LACUSTRINE STRATIGRAPHY: LACKEY, Heather Green1, CASKEY, S. John1, WAN, Elmira2, WAHL, David B.2, and SARNA-WOJCICKI, Andrei M.3, (1) Dept. of Geosciences, San Francisco State University, 1600 Holloway Ave, San Francisco, CA 94132, hglackey@yahoo.com, (2) U.S. Geological Survey, 345 Middlefield Road, MS 975, Menlo Park, CA 94025, (3) U.S. Geological Survey (emeritus), 345 Middlefield Rd, MS 975, Menlo Park, CA 94025 |
| 23-4 | 15 | ESTIMATING BEDROCK INCISION RATES USING 10BE AND 26AL ON STRATH TERRACE GRAVELS, BULLFROG CREEK, UTAH: PERKINS, Jonathan1, SKLAR, Leonard1, WHIPPLE, Kelin2, NISHIIZUMI, Kunihiko3, and HANKS, Tom4, (1) Department of Geosciences, San Francisco State University, San Francisco, CA 94132, j.p.perkins@gmail.com, (2) School of Earth and Space Exploration, Arizona State University, Tempe, AZ 02139, (3) Space Sciences Laboratory, University of California, 7 Gauss Way, Berkeley, CA 94720, (4) U.S. Geol Survey, 345 Middlefield Rd, Menlo Park, 94025 |
| 23-5 | 16 | EVIDENCE THAT THE COLORADO RIVER FLOWED THROUGH UNAWEEP CANYON: HOOD, William C., Physical and Environmental Sciences, Mesa State College, P.O. Box 2647, Grand Junction, CO 81502-2647, WHood@compuserve.com |
| 23-6 | 17 | BALANCED ROCK ORIENTATIONS ARE CONTROLLED BY FRACTURE PATTERNS: WEISER, Deborah, Geology, Occidental College, 1600 Campus Road#649, Los Angeles, CA 90041, dweiser@oxy.edu, GRANT-LUDWIG, Lisa, Program in Public Health, U.C. Irvine, Irvine, CA 92697, and BOGUE, Scott, Geology, Occidental College, 1600 Campus Road, Los Angeles, CA 90041 |
| 23-7 | 18 | GEOLOGIC MAP OF THE PRINCE WILLIAM SOUND AND KENAI PENINSULA REGION, ALASKA: HULTS, Chad P., WILSON, Frederic H., and SHEW, Nora, Alaska Science Center, U.S. Geological Survey, 4200 University Dr, Anchorage, AK 99508, chults@usgs.gov |
| 23-8 | 19 | GEOMORPHOLOGY AND FIELD CHARACTERIZATION OF THE NEW PIEDRA CANYON LANDSLIDE, SOUTHWESTERN, COLORADO: HELD, Dustin, Geosciences Department, Fort Lewis College, 1000 Rim Drive, Durango, CO 81301, DRHELD@fortlewis.edu and KENNY, Ray, Geosciences Department, Fort Lewis College, Durango, CO 81301 |
| 23-9 | | Paper Withdrawn |
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