## 3 ETL Inventory in Cephalonia Island
### Historical and Recent ETL in Cephalonia Island  
Landslides in Cephalonia have been triggered by earthquakes generated in 1636, 1658, 1767, 1867, 1912, 1953, 1983 and 2014 (Figure 4). The focal parameters of these earthquakes are presented in the following Table 2.  
Figure 4: The neotectonic map of Cephalonia along with the historical and recent ETL in the island. Legend of the geological formations in Figure 3.  
3.3.1. The 30 September 1636 Earthquake  
The 30 September 1636 earthquake caused severe structural damage to all buildings of Cephalonia, resulting in 520 fatalities and about 1500 injured people [41; 42; 67]. Heavier damage was reported in the southern part of Cephalonia, where many villages were completely destroyed. Regarding the environmental effects, the earthquake affected the southeastern part of the island. Failures, comprising slides and rockfalls, were triggered along the south facing southern slopes of Aenos Mt. Unstable limestone boulders were detached from slopes in Eleios area (Figure 4) and rolled down resulting in effects on vegetation, buildings and livestock. In particular, a part of the forest on the slopes was destroyed [42], buildings collapsed after crushing and animals were buried under debris. 3.3.2. The 24 August 1658 Earthquake  
This earthquake affected the western part of Cephalonia [41; 42]. It caused the destruction of 500 houses, resulting in 20 fatalities [67; 68; 69]. As regards the induced earthquake environmental effects, [PERSON] [69] referred to the triggering of landslides in the coastal eastern part of Paliki peninsula (Lixouri) resulting in submergence of two coastal sites. Furthermore, ETL were induced, resulting in the collapse of a church founded on the top of a hill. Unfortunately, there is no more information available for determining the exact location of the induced phenomena. 3.3.3. The 22 July 1767 Earthquake  
Cephalonia was also affected by the 22 July 1767 earthquake [41; 42; 67; 70; 71]. Lixouri, in the eastern part of Paliki peninsula, was completely destroyed, Argostoli, in the northern part of the eponymous peninsula, was less affected, while Sami, in the eastern part of the island, and Fiskardo, in the northern part of Erissos peninsula, were extensively damaged as all churches and monasteries were razed to the ground [72; 73; 74]. As a result, 303 fatalities were reported, with 50 of them in Paliki peninsula [69]. Concerning the ETL, rockfalls were generated in Assos area, located in the central-western part of Erissos peninsula [75; 76] (Figure 4). 3.3.4. The 4 February 1867 Earthquake  
This earthquake is the largest that ever hit the Ionian Sea. The greatest damage was observed in the western part of Cephalonia, especially in Paliki peninsula, where Lixouri and the surrounding villages as well as residential areas in Thinia valley were completely destroyed ([67]; AN, 04.02.1867; AV, 06.02.1867; ME, 07.02.1867). As a result, 3200 houses were destroyed and 2600 were damaged, resulting in 224 fatalities [42]. \begin{table}
\begin{tabular}{c c c c c c c c c} \hline
**Lat** & **Lon** & **Year** & **Month** & **Day** & **Mw** & **Io** & **Fatalities** & **Injured** & **Sources 1**  \\ \hline
37.928 & 20.885 & 1636 & 9 & 30 & 6.62 & IX & 520 & 1500 & [41; 54] \\
38.2 & 20.42 & 1658 & 8 & 24 & 6.7 & IX & 20 & - & [41; 54] \\
38.268 & 20.464 & 1767 & 7 & 22 & 6.65 & X & 330 & - & [41; 54] \\
38.233 & 20.424 & 1867 & 2 & 4 & 7.15 & X & 224 & - & [41; 54] \\
38.10 & 20.50 & 1912 & 1 & 24 & 6.1 & X & 8 & - & [40; 54] \\
38.24 & 20.80 & 1953 & 8 & 9 & 5.9 & - & & & [40; 54] \\
38.35 & 20.74 & 1953 & 8 & 11 & 6.6 & - & 455 & 2412 & [40; 54] \\
38.13 & 20.74 & 1953 & 8 & 12 & 7.0 & X+ & & & [40; 54] \\
38.07 & 20.25 & 1983 & 1 & 17 & 6.7 & VI & - & - & [40; 54] \\
38.2113 & 20.4425 & 2014 & 1 & 26 & 6.1 & VII & - & - & [65; 66] \\
38.2716 & 20.4198 & 2014 & 2 & 3 & 5.9 & VIII & - & - & [65; 66] \\ \hline \end{tabular}
\end{table}