skypostman je napisao:
Херц, краљу, царе, знам ја све то, исто тако да Бања Лужа лежи на једном малом "расцјепу". Али говорим ти о неким мојим личним опсервацијама, ево колико ја ово пратим није се десило да за мање од један дан буду 4 мала земљотреса у БиХ.
kako ono bjese 400-500 km juznije
Velike tektonske ploce su jedna stvar a mikro ploce su druga stvar kako bi recmo banjaluka koja je 400-500 km udaljena od prve ploce mogla imati epicentre 12-13 km istocno od centra grada
This scene depicts another segment of the complex tectonic terrane that makes up the alpine mountain system. The Dinaride Alps (Plate KL-5), run southeast along the western side of the Balkans and pass through Yugoslavia into Macedonia, where they join the Hellenide segment. The Plate image shows the Pindus Mountains of central and northwestern Greece (Epirus Mountains in Albania).
Following the breakup of Pangaea, there were several microplates between the Eurasian, African, and Arabian plates. During the Mesozoic and Cenozoic convergence, the microplates were caught between the major plates and underwent a complex series of deformations in the Eastern Mediterranean. The Italo/Adriatic plate moved eastward against the Balkan segment of the Eurasian plate to create the Dinaric orogenic belt. To the south, various microplates (e.g., the Messina, Macedonian, Ionian, Aegean, Turkish, and Levantine plates) became involved along subduction and transform boundaries. The Macedonian microplate that underlies the terrain appearing in the Plate image is bounded on the west and north by suture zones.
A i kad zadrma nema veze sjecam se onaj 81 kad je zatresao cijela ulica je noc provela vani kao veliko kampovanje

bilo