Academic Journals Database
Disseminating quality controlled scientific knowledge

Some large dolines in the Dinaric karst

ADD TO MY LIST
 
Author(s): Kranjc Andrej

Journal: Speleogenesis and Evolution of Karst Aquifers
ISSN 1814-294X

Volume: 4;
Issue: 1;
Start page: 3297;
Date: 2006;
Original page

Keywords: 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, Snežnik in Slovenia), on the contact karst (Škocjanske Jame), on the levels above poljes (Crveno Jezero above the Imotsko Polje), and behind large karst springs (Unška Koliševka above the springs of Malni). Slovene terms for karst depressions are defined.
RPA Switzerland

RPA Switzerland

Robotic process automation

    

Tango Jona
Tangokurs Rapperswil-Jona