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Some large dolines in the Dinaric karstKeywords: karst geomorphology , depression , collapse doline , Dinaric karst Abstract: The main characteristics of the Dinaric karst are all kind of depressions, not only poljes and dolines, but also collapse dolines and similar forms. Some examples of such forms of large dimensions are located on the higher karst plateaus (Pokljuka, Jelovica, Sne nik in Slovenia), on the contact karst ( kocjanske Jame), on the levels above poljes (Crveno Jezero above the Imotsko Polje), and behind large karst springs (Un ka Koli evka above the springs of Malni). Slovene terms for karst depressions are defined.
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