2014
DOI: 10.7494/geotour.2014.37.55
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Surface Karst Landforms of the Notranjska region (south-western Slovenia)

Abstract: The distribution and characteristics of surface karst landforms in the Notranjska region, exemplifi ed in the Cerknisica and Rak river catchment, is presented. The geomorphology of the examined area, with respect to on the micro-, meso-and macroforms division, is described. The course and dynamics of morphogenetic and geological processes are analyzed. A geotourist route linking the described landforms of surface karst is proposed.

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Cited by 3 publications
(5 citation statements)
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“…As shown in the Fig. 1, typical result of this process is development of some salient features such as division of limestone into blocks (clints) bordered by vertical fractures (gricks) [1]. This is a widespread sign of landscape karstification presented by variety of shapes and sizes, spanning up to tens of meters.…”
Section: Karst Phenomenamentioning
confidence: 95%
See 1 more Smart Citation
“…As shown in the Fig. 1, typical result of this process is development of some salient features such as division of limestone into blocks (clints) bordered by vertical fractures (gricks) [1]. This is a widespread sign of landscape karstification presented by variety of shapes and sizes, spanning up to tens of meters.…”
Section: Karst Phenomenamentioning
confidence: 95%
“…Karstified carbonates pose significant challenges in drilling, which can be associated with both the drilling process and unique geological properties. In subsequent sections, we will refer to common in karstology definition of the karst, introduced to describe the landscape, which contains caves, underground channels, and other associated with soluble rocks features [1]. Sudden encountering of some karst-forms during drilling in carbonates may lead to potentially dangerous scenarios.…”
Section: Introductionmentioning
confidence: 99%
“…Green labels in the figure indicate the surface traces of karstification. For example, surface micro-forms can be presented by joints, which divide limestone into blocks with vertical cracks, called grikes [2]. These objects are the result of rock dissolution.…”
Section: Geological Signs Of Karstificationmentioning
confidence: 99%
“…Examples of such dangerous objects, which often occur when drilling in carbonates, are caves or systems of cavities formed due to complex karstification processes. We refer to the common definition of karst [2] that describes the landscape which contains caves, underground channels, and other associated soluble rock features.…”
Section: Introductionmentioning
confidence: 99%
“…Karstification processes often affect carbonate reservoirs and cause the development of a number of unique geological features called karsts. Here we refer to a common definition of the karst, introduced to describe the landscape, which contains caves, underground channels, and other features associated with soluble rocks [2]. Encountering karsts while drilling can cause critical safety incidents including uncontrollable losses of drilling fluid and gas kicks as reported in speciality reports [3][4][5][6].…”
Section: Introductionmentioning
confidence: 99%