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Copyright of Journal of the Institute of Croatian History / Radovi Zavoda za Hrvatsku Povijest is the property of Zavod za Hrvatsku Povijest, Filozofski Fakultet and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

The process of formation of calcareous sinter is often related to karst areas, or areas covered by limestone and dolomite deposits. Such an area is the Dinaric Alps, which cover a large part of Bosnia and Herzegovina. The widely known waterfalls and cascades on the Trebizat - Mlade River, formed by geological and tectonic processes, provided the precondition for formation of waterfalls. Through parallel and subsequent processes of formation of calcareous sinter, they have been shaping the waterfalls. [ABSTRACT FROM AUTHOR]