## 7 The 4 February 1739 Jagodina Earthquake
\begin{table}
\begin{tabular}{c c c c c c c c c c} \hline \multirow{2}{*}{**Source**} & \multirow{2}{*}{**h**} & \multirow{2}{*}{**min**} & \multirow{2}{*}{**sec**} & \multirow{2}{*}{**LAT**, \({}^{\circ}\)**N**} & \multirow{2}{*}{**LON**, \({}^{\circ}\)**E**} & & \multicolumn{3}{c}{**I0, Radii of**} & \\  & & & & & & & **Isoseismal** & **Scale** & **M\({}_{\text{S}}\)** & **M\({}_{\text{W}}\)** \\  & & & & & & & **Areas [km]** & & & \\ \hline [PERSON] et al. [5] & - & - & - & 44.0 & 21.30 & 16 & 8 & MS-5-220, R3-340 & MSK-64 & 6.1 & - \\ [PERSON] et al. [6] & - & - & - & 44.0 & 21.30 & - & 9 & - & - & 6.42 \\ RSZS [2] & - & - & - & 44.0 & 21.30 & 16 & - & EMS & 5.7 & 5.7 \\ \hline \end{tabular}
\end{table} 
Table 6: Seismological data from various sources for the 4 February 1739 earthquake. The table also shows estimations of M\({}_{\text{S}}\) and M\({}_{\text{W}}\) from observed intensities and supposed depths. 117 km from the epicenter of the 8 April 1893 earthquake, and during which the church in Valjevo was damaged. The following two reports about the 1739 earthquake (Appendix F, under serial number 2) are for the Ravanica (Vrdnik) monastery, which is located on the Fruska Gora Mountain. We found these records in the book: \"Old Serbian Records and Inscriptions\" from 1903 [31]. The first contains the information that: \"everything in the temple shook, and it seemed to us that everything was collapsing from the many shaking; the earth shook three times, and we all ran outside for fear of a lot of destruction\". The second report confirms the date and time of the event, as well as that there were several aftershocks and that during the mainshock: \"all the people fell with their faces to the ground for fear of [PERSON]\". Based on these two reports, we assigned the interval value I = VI-VII for this location. For the same monastery, there is information regarding the harmful effects of the 8 April 1893 earthquake, which we found on its website: \"Renovations of the church and the lodge were recorded in 1885, as well as in 1898, after being devastated in the earthquake (1893)\". We can infer from this short text that the church was damaged in the earthquake of 8 April 1893, but there is not enough data to assign a particular value of intensity. We believe we can assign a possible interval value of I = VI-VII for this location. In the report from the Paragovo Forest (Appendix F, also under serial number 2), which is also located on the Fruska Gora mountain, we can learn that the earthquake was felt by a monk who happened to be in the forest in the vicinity of the village of Paragovo, about 5.5 km NE of the monastery (Rakovac) where he lived. From this information alone, we cannot rate the intensity value. Here, we should note that the reporter was in a forest during the earthquake and that for Ravanica (Vrdnik) monastery, which is only about 10 km southwest of Paragovo, we assessed the effects of the earthquake with I = VI-VII. The third report (Appendix F, example number 3) we managed to find is for the Savina monastery, located near the city of Hercego Novi in today's Montenegro: \"the earth shook in the month of January on the 24 th day at noon or in the afternoon\". From this short text, we can estimate the intensity at the location of the Savina monastery with I = IV-V. It should be noted that this monastery is located 288 km SW from the epicenter of the 1739 earthquake. Unfortunately, we have not found any records from this monastery or nearby villages or cities reporting the 1893 earthquake to compare the effects of the 1739 and 1893 earthquakes. Four reports from Timisoara, Romania, are given in Appendix F under serial number 4. The first, the third, and the fourth contain only the information that there was a strong earthquake in Timisoara. However, in the second one, we find that the earthquake was: \"violent enough that the clock bell on the Jesuit tower struck the hammer rising above it, and distinct chimes were heard.