Paper No. 58-3
Presentation Time: 8:00 AM-12:00 PM
REDISTRIBUTION OF VOLCANIC ASH ALONG THE FORTYMILE WASH SYSTEM, YUCCA MOUNTAIN, NEVADA; PREDICTING THE DOSE CONSEQUENCES TO THE CRITICAL POPULATION OF AN ERUPTION THROUGH THE YUCCA MOUNTAIN REPOSITORY
EBERT, K. Teryn, Earth and Environmental Sciences, Lehigh Univ, 31 Williams Drive, Bethlehem, PA 18015, teryne@hotmail.com, HARRINGTON, Charles D., Los Alamos National Lab, PO Box 1663, Los Alamos, NM 87545-0001, and WHITNEY, John W., U.S. Geol Survey, Federal Ctr, M.S. 425, Denver, CO 80225

A volcanic eruption through the Yucca Mountain Repository, although highly improbable (1x10-8 per year) would be an event with a possible very high hazard. This study is to determine the effects on the critical population from erupted tephra carried along or through the Fortymile Wash drainage system, which is main drainage for the eastern slope of the Yucca Mountain area. The critical population (REMI) lives at a distance of approximately 20 km from the repository, on the alluvial fan/delta of the Fortymile Wash. Our study will evaluate ash redistribution resulting from wind or water erosion in order to determine the impact to the dose that the critical population would experience. In order to predict the dose amount we will determine the nature of ash redistribution area and how the ash is diluted through the drainage system. We purpose to calculate the volume of material that has been deposited within the past 50 years using Cesium-137, a bomb produced tracer, to determine the erosional and depositional patterns around Yucca Mountain. Most Cesium-137 studies to date have only covered a small (<5 square km) area. Initial results will be presented. This study will cover a much larger area of >1500 square km and require more than 200 samples. The Lathrop Wells volcanic cone, located 12 km south of Yucca Mountain, erupted 70,000 years ago and produced an extensive tephra sheet. This tephra sheet will be studied as an analog to the possible eruption through the repository to determine the nature of tephra dilution in drainages west and south of the cone. Samples have been collected at 100-ft intervals along the tephra sheet and along the ash filled drainage systems. Stratigraphy of the pits will be mapped and sampled to establish a transect along which ash is diluted from its source over a distance of > 2km. The values obtained from the ash dilution study, applying the scaling factor for the Fortymile wash system, will be used to calculate the amount of contaminated ash that would reach the critical population and impact the calculation of the dose.

2002 Denver Annual Meeting (October 27-30, 2002)
Session No. 58--Booth# 33
Quaternary Geology/Geomorphology (Posters) I
Colorado Convention Center: Exhibit Hall
8:00 AM-12:00 PM, Monday, October 28, 2002
 

© Copyright 2002 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.