## 7 Results of the InSAR Processing
### Vertical and Horizontal Displacements
The uplift detected at the Potami coastal area with the Akra and Pounta promontories was 20-22 cm, while the InSAR analysis showed a smaller uplift of 1.3 cm from the SARscape software and 5 cm from the SNAP software (sections and profile graphs A9-A9\({}^{\prime}\) and B9-B9\({}^{\prime}\) in Figures 30 and 31). 5. The uplift detected at the Marathokambos coastal area was 10 cm, while the InSAR analysis showed a smaller uplift of 2 cm from the SARscape software and 5.5 cm from the SNAP software (sections and profile graphs A10-A10\({}^{\prime}\) and B10-B10\({}^{\prime}\) in Figures 30 and 31). Figure 31: _Cont._  
Therefore, with the exception of the Asprochorti and Kokkari sites, where there is neither a qualitative nor a quantitative correlation between the field measurements and the InSAR results, in the other studied sites and areas the results from both methods are qualitatively identical, but quantitatively different. As regards the studied areas affected by coeismic surface ruptures, a change in the surface deformation on both sides of the ruptures was observed. A typical example is the section and the corresponding graphs A7-A7\({}^{\prime}\) and B7-B7\({}^{\prime}\) (Figure 31) in the area of Ayios Konstantinos-Kontakaieka-Vrysses, where the southeastern fault block (the southeastern part of the section) is characterized by uplift and the northwestern fault block (northwestern part of the section) by subsidence. The type of the surface deformation detected by the InSAR analysis is qualitatively identical to the field observations since, as determined, the offset along the ruptures was normal with subsidence of the northwestern fault block and uplift of the southeastern one. Similar observations can be made and similar conclusions can be drawn for the sections and the respective graphs in the areas of Ano Ayios Konstantinos (A5-A5\({}^{\prime}\) and B5-B5\({}^{\prime}\)) and Ampelos (A6-A6\({}^{\prime}\) and B6-B6\({}^{\prime}\)) (Figure 31). \begin{table}
\begin{tabular}{c c c c} \hline \hline \multicolumn{5}{c}{**Surface Deformation Measurements**} \\ \multicolumn{2}{c}{**Surface Deformation**} & \multicolumn{3}{c}{**InSAR Analysis**} \\ \multicolumn{2}{c}{**Field Surveys**} & \multicolumn{3}{c}{**(Amount of Uplift Based on Sections**} \\ \multicolumn{2}{c}{**A1–A11 and B1–B11)**} \\ \cline{2-4} \multicolumn{1}{c}{} & **[PERSON] et al. (2021)** & **This Study** & **SARscape** & **SNAP** \\ \hline Sykia (S Samos) & +23 cm & - & stability & \\ Klima (SE Samos) & stability & - & stability & \\ Posidonio (E Samos) & +13 cm & - & stability & \\ Mourtia (NE Samos) & +8 cm & - & stability & \\ Kokkari (NE Samos) & +22 cm & - & \(-\)2.0 cm & \(-\)1.4 cm \\ Ayios Nikolaos chapel, Potami & +20 cm & +20 cm & uplift & \\ beach(NW Samos) & +22 cm & +22 cm & uplift & \\ Punta Promororty (NW Samos) & +22 cm & +22 cm & uplift & \\ Megalo Seitani (W Samos) & +22 cm & - & uplift & \\ Ayios Isidoros (W Samos) & +35 cm & +30 cm & uplift & \\ Ayios Nikolaos (N Samos) & - & +15–20 cm & uplift & \\ Pythagoreio (SE Samos) & +15 cm & +15–20 cm & \(-\)1.3 cm & \(+\)2.5 cm \\ PSII Ammos (SE Samos) & +13 cm & +15 cm & stability, small uplift & \\ Potokaki (SE Samos) & - & +17–25 cm & stability, small uplift & \\ Karlovasi vessel shelter (NW Samos) & - & +24 cm & +2.8 cm & \(+\)6.3 cm \\ Marathokampos (Molos) (SW Samos) & - & +15–20 cm & +2.0 cm & \(+\)5.5 cm \\ Kampos (SW Samos) & - & +15–20 cm & uplift & \\ Asprochorti (NE Samos) & - & +10 cm & \(-\)6.0 cm & \(-\)1.0 cm \\ \hline \hline \end{tabular}
\end{table} 
Table 4: Uplift from field surveys and the interferometric synthetic aperture radar (InSAR) analysis. Figure 31: Surface displacement profile graphs resulting from the sections in the displacement map (descending) of Figure 30. Profile graphs (**A1–A11**) resulted from the SARscape software and the profile graphs (**B1–B11**) from the SNAP software. A change in the type of surface deformation was observed on both sides of the surface ruptures. In both cases, the southern part was uplifted and the northern part had subsided.