engleski

Reply to “Comment on ‘Historical Seismicity of the Rijeka Region (Northwest External Dinarides, Croatia)—Part I: Earthquakes of 1750, 1838, and 1904 in the Bakar Epicentral Area’ by Davorka Herak, Ivica Sović, Ina Cecić, Mladen Živčić, Iva Dasović, and Marijan Herak” by Stathis C. Stiros

Any analysis of historical earthquakes is done with the hope that it will help better explain local seismicity or provide new clues to understand independent observations constraining seismotectonic processes. We therefore welcome the comment on our paper (Herak et al., 2017 ; hereafter, Hea2017) by Stiros (2017 ; hereafter, S2017), who suggests that the 1750 Bakar earthquake, one of the three events we analyzed in Hea2017, could have been responsible for at least a part of the land subsidence in the Bakar area, evidenced by submerged tidal notches in the Bay of Bakar

historical seismicity ; Rijeka region

nije evidentirano