1_README.TXT Quaternary Paleoseismology and Stratigraphy of the Yucca Mountain Area, Nevada By Edited by William R. Keefer, John W. Whitney, and Emily M. Taylor Professional Paper 1689 2004 U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director Prepared in cooperation with the U.S. Department of Energy, Nevada Operations Office (Interagency Agreement DE-AI08-97NV12033) QUICK START Open the index.html document to get information about the database, view the table of contents and navigate the CD- ROM. ABSTRACT The U.S. Geological Survey has conducted a comprehensive series of fault studies to determine the history and extent of Quaternary deformation in the Yucca Mountain area of southwestern Nevada as part of a broad, multidisciplinary site-characterization program to evaluate the suitability of the mountain to host a geologic repository for the safe and permanent storage of high-level radioactive wastes. The results of the detailed studies reported here provide basic data that are fundamental to assessing the risks posed by potential future earthquakes and fault displacements with respect to the design and long-term performance of the proposed facilities. The scope and objectives of fault investigations were largely guided by regulations established by the U.S. Nuclear Regulatory Commission and the U.S. Department of Energy for the siting of geologic repositories for the storage of high-level radioactive wastes. This report focuses primarily on eight faults within and near Yucca Mountain that are known to have been active during Quaternary time, as well as on two other conspicuous fault systems in nearby areas that also demonstrate neotectonic activity. The overall objective was to obtain, for each individual fault or fault system, definitive information on the number, magnitude, and estimated dates of surface-rupturing paleoearthquakes. Compiling such information involved extensive field investigations, excavation and logging of trenches, detailed descriptions of surficial deposits and soils, and selected sampling and analyses for numerical age determinations, all of which were performed in accordance with a rigorous set of technical procedures and guidelines that were formulated to comply with quality- assurance standards- an essential requirement for activities related to the siting of nuclear facilities. Beyond the specific purpose of providing a basis for the seismic-risk analysis of Yucca Mountain, the accumulated data and resulting interpretations constitute a valuable contribution to our knowledge and understanding of the neotectonics in this part of the Basin and Range Province. Faults in few other parts of the region have been studied as thoroughly and comprehensively, and so the pattern of Quaternary deformation within this limited area may serve as an example of the structural relations and the locations and magnitudes of potential future earthquakes elsewhere in the Great Basin. SYSTEMS REQUIREMENTS IBM-compatible computers running Windows95 or higher or NT 4.0 or higher with Intel Pentium or equivalent processor. MacIntosh with PowerPC processor SOFTWARE Web browser; Adobe Acrobat Reader (Acrobat Reader installers for Macintosh and Windows are provided on this CD-ROM) FOR SALE BY: USGS Information Services Box 25286 Denver Federal Center Denver, CO 80225 Telephone: (888) ASK-USGS The bibliographical reference for this publication is: Keefer, William R., Whitney, John W., and Taylor, Emily M., eds., 2004, Quaternary paleoseismology and stratigraphy of the Yucca Mountain area, Nevada: U.S. Geological Survey Professional Paper 1689 (CD-ROM). ISBN: 0-607-95752-2 This report and any updates to it are available on line At http://pubs.usgs.gov/pp/pp1689/ DISCLAIMERS This Compact Disc Read-Only Memory (CD-ROM) publication was prepared by an agency of the U.S. Government. Neither the U.S. Government nor any agency thereof, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed in this report, or represents that its use would not infringe on privately owned rights. Reference therein to any specific commercial product, process, or service, by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the U.S. Government or any agency thereof. 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