%0 Journal Article
%@ 0037-1106
%A Arabasz, W. J.
%A Nava, S. J.
%A McCarter, M. K.
%A Pankow, K. L.
%A Pechmann, J. C.
%A Ake, John
%A McGarr, Arthur F.
%A University of Utah Seismograph Stations Department of Geology and Geophysics University of Utah Salt Lake City, Utah 84112,
%A ENSCO, Inc., Melbourne, Florida 32940,
%A University of Utah Seismograph Stations Department of Geology and Geophysics University of Utah Salt Lake City, Utah 84112,
%A University of Utah Seismograph Stations Department of Geology and Geophysics University of Utah Salt Lake City, Utah 84112,
%A University of Utah Seismograph Stations Department of Geology and Geophysics University of Utah Salt Lake City, Utah 84112,
%A Seismotectonics and Geophysics Group U.S. Bureau of Reclamation Denver, Colorado 80225,
%A U.S. Geological Survey Menlo Park, California 94025,
%D 2005
%F epos:1423
%I Seismological Society of America
%J Bulletin of the Seismological Society of America
%N 1
%P 18-30
%T Coal-Mining Seismicity and Ground-Shaking Hazard: A Case Study in the Trail Mountain Area, Emery County, Utah
%U https://episodesplatform.eu/eprints/1423/
%V 95
%X We describe a multipart study to quantify the potential ground-shaking hazard to Joes Valley Dam, a 58-m-high earthfill dam, posed by mining-induced seismicity (MIS) from future underground coal mining, which could approach as close as ~1 km to the dam. To characterize future MIS close to the dam, we studied MIS located ~3-7 km from the dam at the Trail Mountain coal mine. A 12-station local seismic network (11 stations above ground, one below, combining eight triaxial accelerometers and varied velocity sensors) was operated in the Trail Mountain area from late 2000 through mid-2001 for the dual purpose of (1) continuously monitoring and locating MIS associated with longwall mining at a depth of 0.5-0.6 km and (2) recording high-quality data to develop ground-motion prediction equations for the shallow MIS. (Ground-motion attenuation relationships and moment-tensor results are reported in companion articles.) Utilizing a data set of 1913 earthquakes (M ≤ 2.2), we describe space-time-magnitude distributions of the observed MIS and source-mechanism information. The MIS was highly correlated with mining activity both in space and time. Most of the better-located events have depths constrained within +-0.6 km of mine level. For the preponderance (98%) of the 1913 located events, only dilatational P-wave first motions were observed, consistent with other evidence for implosive or collapse-type mechanisms associated with coal mining in this region. We assess a probable maximum magnitude of M 3.9 (84th percentile of a cumulative distribution) for potential MIS close to Joes Valley Dam based on both the worldwide and regional record of coal-mining-related MIS and the local geology and future mining scenarios.