Hi, sorry that I can't answer in Bosnian, I can read it quite well, but not write it more than a few words. The text was translated in Bosnian, from my original text in French, by a visitor.seljak_cojek wrote: Pošto se očito razumiješ u geologiju (pročitao sam ovo sa tvog linka) htio bih pitati, da li je normalno, uobičajeno ili kako god da se ovako različite geološke strukture nađu tako blizu (dvestotinjak metara).
I drugo pitanje (nisam našao odgovor u tvom tekstu), šta uzrokuje pojavu da se između dva okamenjena sloja nalazi sloj (od metar i nešto) rastresitog materijala.
Yes it is; the geological structures are not very different (same kind of sedimentary layers), only one (Visocica) has been more deformed, being nearer to the axis of the anticline, so that the layers have a much more important dip ("pad slojeva"). The region had a long and agitated tectonical history, so that you can find various dips in a few hundred meters, that is quite usual in sedimentary folded regions.da li je normalno, uobičajeno ili kako god da se ovako različite geološke strukture nađu tako blizu (dvestotinjak metara)
Well, I think it's explained in the article (second part, "Sedimentarni «mille-feuilles»") : these layers were deposited during a very long period, millions years, during which the conditions (climatic and tectonical) have varied a lot; each layer reflects a different phase, that could last a few months or a few years. Again it is quite usual in lacustrine sediments, where the condition of the sedimentation varies much more than in deep sea.šta uzrokuje pojavu da se između dva okamenjena sloja nalazi sloj (od metar i nešto) rastresitog materijala
I hope you'll be able to understand my English, I would be totally unable to explain it in Bosnian !
Irna
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