The study of the palaoseismic events in the karst terrains of the Bulgarian
Black Sea coast is a very important up-to-date problem. The investigated r
egion is one of the highest-energy regions in Bulgaria with established and
recorded catastrophic historic and contemporary earthquakes. The terrain i
s subjected to the influence not only of its own earthquake foci but also o
f those in Romania and Russia. The palaeoearthquakes that caused considerab
le disturbances in the karst terrains along the Northern Bulgarian Black Se
a coast have left significant traces. They caused disturbances in the envir
onment and the relief (rearrangement of the surface and ground water karst
basins, partially or entirely collapsed caves, deformed caves, oil, gas and
salt intrusions and gravitationally formed caves). The ecological conseque
nces in historic and contemporary aspects were catastrophic. The palaeoseis
mic dislocations were formed as a result of global, regional and local geod
ynamic events related with the destruction of the Moezian platform and the
regional extension of the Black Sea basin. The time of their display and th
eir spatial interrelations were established as a result of complex investig
ations accompanied by original documents.