Aftershocks Magnitude 4.0 and Greater

2001/01/13 20:56:19  12.11N  88.34W  33.0 4.7    
2001/01/14 08:28:14  12.82N  88.75W  33.0 4.1    
2001/01/14 11:09:11  12.06N  88.82W  33.0 4.6    
2001/01/14 22:41:26  12.92N  88.81W  33.0 5.5    
2001/01/14 22:47:52  12.83N  88.78W  33.0 5.1    
2001/01/15 00:22:50  12.65N  88.79W  33.0 5.0    
2001/01/15 00:50:09  12.73N  88.97W  33.0 4.7    
2001/01/15 05:09:05  12.79N  88.80W  33.0 5.0    
2001/01/15 12:20:03  12.74N  88.63W  33.0 5.2    
2001/01/16 04:38:45  12.61N  88.35W  33.0 4.7    
2001/01/16 08:22:08  12.81N  88.77W  33.0 5.2    
2001/01/16 10:58:13  12.90N  88.73W  33.0 5.7    
2001/01/16 11:24:29  12.90N  88.99W  33.0 4.9    
2001/01/16 23:32:40  12.19N  88.76W  33.0 4.4    
2001/01/17 01:40:15  12.99N  88.91W  33.0 4.9    

From experience with earthquakes around the world, we know that there are likely to be aftershocks. Some of the aftershocks may be large enough to cause additional damage. Buildings that have already been damaged by an earlier earthquake are at highest risk from damage due to a future aftershock. We also know from past experience that the number of aftershocks will decrease over the next few months. There might be short episodes of higher activity, but the overall trend will be for fewer aftershocks as time goes by. Seismologists are not able to predict the timing and sizes of individual aftershocks.

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