Kammala jumla mai zuwa: An gano wani ɓarna mai aiki a arewa maso yammacin Dubrovnik, yana ƙarawa zuwa tsibirin Dalmatian yayin da Plate na Eurasian ke zamewa a kan ƙaramin Adriatic. Bugu da ƙari, kuskuren ya sa kudancin kudancin Apennine ya motsa zuwa gabar da ke gaba da kusan kowace shekara. Idan wannan motsi ya ci gaba, kasan teku zai cinye gaba ɗaya kuma Tekun Adriatic ya rufe cikin shekaru miliyan 50-70. A arewacin Adriatic, gabar tekun Gulf of Trieste da yammacin Istria suna raguwa a hankali, sun nitse kusan shekaru dubu biyu da suka gabata. A tsakiyar Adriatic Basin, akwai shaidar volcanism na Permian a yankin Komiža a tsibirin Vis da tsibirin volcanic na Jabuka da Brusnik. An lura da girgizar ƙasa a yankin tun farkon bayanan tarihi. Wani girgizar kasa mai karfi da aka yi a yankin a baya-bayan nan shi ne girgizar kasa mai karfin gaske.
Girgizar kasa ta 1979 Montenegro, auna 7.0 a kan sikelin Richter. Girgizar ƙasa ta tarihi a yankin sun haɗa da 1627 Gargano peninsula da 1667 Dubrovnik girgizar ƙasa, duka biyun sun biyo bayan tsunami mai ƙarfi. A cikin shekaru 600 da suka gabata, tsunami goma sha biyar sun faru a cikin Tekun Adriatic.