Bulletin of the Seismological Society of America
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Bulletin of the Seismological Society of America; February 2005; v. 95; no. 1; p. 18-30; DOI: 10.1785/0120040045
© 2005 Seismological Society of America
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Coal-Mining Seismicity and Ground-Shaking Hazard: A Case Study in the Trail Mountain Area, Emery County, Utah

W. J. Arabasz1, S. J. Nava*,1, M. K. McCarter2, K. L. Pankow1, J. C. Pechmann1, J. Ake3 and A. McGarr4

1 University of Utah Seismograph Stations
Department of Geology and Geophysics
University of Utah
Salt Lake City, Utah 84112
 (W.J.A., S.J.N., K.L.P., J.C.P.)

2 Department of Mining Engineering
University of Utah
Salt Lake City, Utah 84112
 (M.K.M.)

3 Seismotectonics and Geophysics Group
U.S. Bureau of Reclamation
Denver, Colorado 80225
 (J.A.)

4 U.S. Geological Survey
Menlo Park, California 94025
 (A.M.)

* Present address: ENSCO, Inc., Melbourne, Florida 32940.

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.




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