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We have examined the digital waveform data and relocated a number of events within the June 1987 earthquake swarm, which occurred beneath the northern part of Lake Aswan, 70 km southwest of the Aswan High Dam in Egypt. This swarm occurred between June 17th and 19th with a maximum magnitude event of ''M L '' ¼ 3.5.Cross correlation between a chosen master and the analyzed events has been carried out on seismograms from stations of the Aswan network. The cross correlation demonstrates the presence of a difference in both the P wave (Dt p ) and the S wave (Dt s ) arrival times at each station in the network relative to the arrival times of the master event at the same stations. Dt p ranges between )0.15 and 0.11 second, while Dt s ranges between )0.17 and 0.11 second.The primary interpretation is that these time differences represent an error in the manually picking arrival times. Then, Dt p and Dt s values for each event result from a change in the hypocentral parameters from those of the master event, assuming the P-and S-wave velocity distribution remains constant during the swarm activity. This interpretation enables us to determine the relative distribution of hypocenters with respect to the hypocentral location of the master event. We present the results from a swarm of 9 events demonstrating they originate from a nearly unique location, rather than the zone identified from the preliminary locations which used manually picked onset times.

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