Pedzisa mutsara unotevera: Nzvimbo yacho inoratidza karst morphology, ine matombo makuru anoumbwa nematombo erima uye nzvimbo duku dzedolomites uye Quaternary sediments. Eocene flysch inoumba muganhu wekumaodzanyemba kwakadziva kumadokero kwenzvimbo yekuchera mvura, iyo nzvimbo yekuchera mvura inoyerera uye panomuka Ombla. Matombo aya akaumbwa sezvo nhevedzano yakakora yemakemikari ecarbonate yakaiswa pakati peNorian neLate Cretaceous seAdriatic Carbonate Platform, kusvika pakadzika. MuEocene uye kutanga kweOligocene, Adriatic Plate yakaenda kuchamhembe uye kuchamhembe kwakadziva kumabvazuva, ichibatsira kuAlpine orogeny kuburikidza nekusimudzwa kwe tectonic kweDinarides. Karst topography yebhazi yakatanga kubva pakuratidzwa kwepuratifomu yecarbonate kumamiriro ekunze. Karstification yakatanga zvikuru mushure mekusimudzwa kwekupedzisira kweDinarides muOligocene neMiocene, apo carbonates yakaratidzirwa kumigumisiro yemhepo; izvi zvakawedzerwa kusvika pazasi pegungwa razvino, rakaonekwa panguva yeLast Glacial Maximum. Mamwe mapoka ekarst akaumbwa munguva dzapakuvamba dzokudonha kwemwero wegungwa, zvikurukuru Messinian salinity crisis. Chimiro chenzvimbo yenzvimbo yacho chinoratidza chiitiko che tectonic chazvino mudziva, nekukanganisa kunoitika pakati peHum neOmbla. Kudengenyeka kwenyika kwakasimba kuchangobva kuitika munharaunda yakakura kwakanga kuri
Kudengenyeka kweMontenegro muna 1979, kwakayera 7.0 pachikero cheRichter. Kudengenyeka kwepasi kwakasimba chete munhoroondo munharaunda yacho kwaiva kudengenyeka kweDubrovnik muna 1667, kwakateverwa netsunami.