Migrated seismic section MCS-EK9 and its interpretation. This section displays shallow normal faults terminating at about 100 ms depths. The extension of these faults coincides with western bank of Küçükçekmece Lake where land sliding is observed (see Fig. 2). Some other faults cutting the strata at shot locations 150, 250 and 350 are observed in the section. The layers between shots 150 and 250 are depressed and this depression is more pronounced at greater depths indicating fault controlled mechanism.