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North Fork Valley Seismic Network — First Quarter 2011 <br />Depth to Top of layer (km) [mi] <br />Velocity (km /sec) [ft /sec] <br />1.00 [0.62] <br />3.9 [12,796] <br />1.50 [0.93] <br />4.60 [15,093] <br />2.50 [1.55] <br />5.20 [17,061] <br />3.50 [2.17] <br />6.00 [19,686] <br />6.00 [3.73] <br />6.5 [21,327] <br />Magnitude Estimation <br />M magnitudes are generally provided for the larger events recorded (M >_ 3.0) and located by <br />the National Earthquake Information Center (NEIC). There were three events reported by the <br />NEIC during the first quarter, two events on 6 January and one on 17 February. Mc values are <br />automatically calculated by Earthworm, based on a USGS northern California formula. M <br />values are approximately equivalent to M L . <br />RESULTS <br />Seismic Event Locations <br />Table 3 lists the 86 events recorded and relocated (M >_ 1.7) in the first quarter. The date and <br />origin time (hours, minute, and second) of the event, location (latitude, longitude, and general <br />area), magnitude, and largest PGA values (in g's; I = 980 cm /sec are listed. <br />Figure 2 shows the resulting locations for the mining - related seismic events of approximate M <br />1.7 and larger. Note event locations are better constrained when they occur within the perimeter <br />of the seismic network (greater azimuthal coverage). The events are located throughout the study <br />area but the vast majority are concentrated in the Oxbow Mine area, with only three events in the <br />West Elk Mine Permit Area (Figure 2). The largest event to occur during the reporting period <br />was a M 3.1 event on 17 February. The event occurred at 22:47 GMT within the Elk Creek <br />Mine. The largest event within the West Elk Permit Area was a M 1.8 on 12 January at 02:43 <br />GMT. <br />Two possible tectonic events occurred within the Oxbow Mine on 25 January and 22 February <br />with magnitudes of M 1.7 and 2.0, respectively (Figure 2 and Table 3). The events exhibited <br />some compressional first motions ( "up ") at most of the NFVSN stations. The mining - related <br />seismic events that have been observed to date by the NFVSN generally exhibit all dilatational <br />( "down ") first motions, typical of coal mine seismicity in Utah (e.g., Wong and McGarr, 1990). <br />The focal depth for the event on 22 February was 5.4 kin consistent with a tectonic origin. The <br />25 January event remains questionable due to its shallow focal depth of about 1 kin, and its <br />location within the area of active mining (Figure 2). <br />Seismic Event Magnitudes <br />Of the 84 mining - related events, all were assigned magnitudes (Table 3). M values assigned by <br />Earthworm are also listed in Table 3. The events on 6 January and 17 February were reported <br />during this quarter by NEIC as occurring within the bounds of Figure 2. Two NEIC recorded <br />WAX_WCFS \PROJECTS \WEST ELK -MTN COAL \2011 Q1 \Q1_2011_MCC.DOC \27- MAY -11\ \OAK 4 <br />