False color composite Landsat 8 images, including thermal bands (thermal bands: Band 7, wavelength: 2.11-2.29 µm; Band 10, wavelength: 10.6-11.19 µm) combined with texture enhancements, provide clear visibility of linear features, such as those seen in Figure 10. The spectral emissivity properties of larger fault zones in the thermal bands are often influenced by soil moisture. Surface water often finds easy passage through fault zones and, therefore, increases soil moisture. This, in turn, influences the emissivity pattern of thermal bands. The reservoir area is characterized by estimated V s 30 **data** ranging between 600 and 760 m/s. The dam site area is obviously not affected by higher susceptibility to soil amplification, as in the case of lower V s 30 velocities (<400 m/s) within broader valleys and depressions.