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Kontaktni kras v Kočevskem Rogu in Kočevski Mali gori
Gostinčar, Petra (Author)

URLURL - Presentation file, Visit http://revije.ff.uni-lj.si/Dela/article/view/dela.35.2.27-44/698 This link opens in a new window

Abstract
Na dinarskih kraških planotah Kočevskega Roga in Kočevske Male gore se je na kontaktu med kraškim in fluvialnim geomorfnim sistemom oblikoval t.i. kontaktni kras. Preučene so bile geomorfološke oblike in procesi na štirih območjih kontaktnega krasa. Na stiku med nekarbonatnimi in karbonatnimi kamninami so se razvile ponikve, slepe doline (aktivne in fosilne), konkavne oblike v bližini kontakta pa so zapolnjene z nekarbonatnimi sedimenti. Na kontaktu med različnimi karbonatnimi kamninami (dolomiti in apnenci) so reliefne oblike kontaktnega krasa manj jasno izoblikovane, mdr. ponori (aktivni in fosilni), ponorni zatrepi ter suhe doline.

Language:Slovenian
Keywords:geomorfologija, kras (geologija), krasoslovje, kontaktni kras, Slovenija, Kočevski Rog
Work type:Not categorized (r6)
Tipology:1.01 - Original Scientific Article
Organization:FF - Faculty of Arts
Year:2011
Publisher:Oddelek za geografijo Filozofske fakultete Univerze v Ljubljani
Number of pages:str. 27-43
Numbering:[Št.] 35
UDC:551.44(497.4)
ISSN on article:0354-0596
DOI:10.4312/dela.35.2.27-44 Link is opened in a new window
COBISS.SI-ID:47813218 Link is opened in a new window
Views:474
Downloads:149
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Record is a part of a journal

Title:Dela
Publisher:Oddelek za geografijo Filozofske fakultete Univerze v Ljubljani
ISSN:0354-0596
COBISS.SI-ID:23805442 This link opens in a new window

Secondary language

Language:English
Title:Contact karst of Kočevski Rog and Kočevska Mala gora
Abstract:
On high Dinaric karst plateaus of Kočevski Rog and Kočevska Mala gora, the so-called contact karst is present. Geomorphic processes and landforms of four case study areas of contact karst were researched in detail. Two types of contact karst were recognized: between non-carbonate and carbonate rocks and between different carbonate rocks. In the first case, ponors and blind valleys (active and fossil) were formed and concave forms near the contact are infilled with non-carbonate sediments. On the contact between different carbonate rocks (dolomite and limestone), the forms are similar but less evident, e.g. ponors (active and fossil), ponor steepheads and dry valleys.

Keywords:geomorphology, karstology, contact karst, Slovenia

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