Na kraškem površju, ki je pokrito z naplavino ali prstjo, nastajajo tudi podtalne skalne oblike. So posledica pretakanja vode po stiku med skalo in prstjo, prenikanja vodo skozi prst in pritekanja vode do površine prsti, ki obdaja skalo. Podtalne skalne oblike so pogosto pomembna sled razvoja kraškega površja. To je poskus razločevanja tipičnih kraških podtalnih skalnih oblik in zasnova za njihovo novo tipizacijo. Subcutaneous rock forms occur on karst surfaces covered with sediment or soil. They are the consequence of water running along the contact between rock and soil, the percolation of water through the soil, and inflow of water to the surface of the soil surrounding the rock. Subcutaneous rock forms are often important traces of the ...
Usjeci i zasjeci, zajedno s nasipima, su vrlo česti tijekom izgradnje svih vrsta prometnica, pa tako...
Abstract UDC: 551.44(55+437.1) JiÞ Bruthans & OndÞej Zeman: Factors controlling exokarst morpho...
Abstract UDC: 551.4.(495) Kyriaki Papadopoulou-Vrynioti: The role of epikarst in the morphogenesis o...
The distribution and characteristics of surface karst landforms in the Notranjska region, exemplifi ...
Na brečasti dolomitni kamnini se pod debelimi tlemi oblikuje podtalni kamniti gozd. Kamniti stebri s...
This paper explains the investigation of shallow and sediment-covered areas of the Dolenjska karst d...
The relief of Bela Krajina and Semiška Reber in southeastern Slovenia is mainly a consequence of pos...
The paper is a geomorphological classification of pseudokarst forms in Czechoslovakia/Bohemien Massi...
The study of the formation and development of karst phenomena and their rock relief using laboratory...
Karst is a landscape created by the dissolution of carbonate rocks, although similar features can al...
Na hrvaškem krasu je veliko udornic. So tudi take, nastale zaradi posedanja (subsidence). Analiziran...
Skriti kras (cryptokarst) je kras, razvit pod prepustnim, vendar netopnim pokrovom. Nastane zaradi v...
Jame brez stropa so bile stare jame, ki so zaradi znižanja kraškega površja razkrite. Posebno pozorn...
Članek obravnava zakrasevanje ob narivnem kontaktu dolomita in apnenca v Idrijskem Logu in Koševniku...
Debelino krovnine je mogoče razporediti v 4 razrede. Za vsakega so značilne posebne površinske in po...
Usjeci i zasjeci, zajedno s nasipima, su vrlo česti tijekom izgradnje svih vrsta prometnica, pa tako...
Abstract UDC: 551.44(55+437.1) JiÞ Bruthans & OndÞej Zeman: Factors controlling exokarst morpho...
Abstract UDC: 551.4.(495) Kyriaki Papadopoulou-Vrynioti: The role of epikarst in the morphogenesis o...
The distribution and characteristics of surface karst landforms in the Notranjska region, exemplifi ...
Na brečasti dolomitni kamnini se pod debelimi tlemi oblikuje podtalni kamniti gozd. Kamniti stebri s...
This paper explains the investigation of shallow and sediment-covered areas of the Dolenjska karst d...
The relief of Bela Krajina and Semiška Reber in southeastern Slovenia is mainly a consequence of pos...
The paper is a geomorphological classification of pseudokarst forms in Czechoslovakia/Bohemien Massi...
The study of the formation and development of karst phenomena and their rock relief using laboratory...
Karst is a landscape created by the dissolution of carbonate rocks, although similar features can al...
Na hrvaškem krasu je veliko udornic. So tudi take, nastale zaradi posedanja (subsidence). Analiziran...
Skriti kras (cryptokarst) je kras, razvit pod prepustnim, vendar netopnim pokrovom. Nastane zaradi v...
Jame brez stropa so bile stare jame, ki so zaradi znižanja kraškega površja razkrite. Posebno pozorn...
Članek obravnava zakrasevanje ob narivnem kontaktu dolomita in apnenca v Idrijskem Logu in Koševniku...
Debelino krovnine je mogoče razporediti v 4 razrede. Za vsakega so značilne posebne površinske in po...
Usjeci i zasjeci, zajedno s nasipima, su vrlo česti tijekom izgradnje svih vrsta prometnica, pa tako...
Abstract UDC: 551.44(55+437.1) JiÞ Bruthans & OndÞej Zeman: Factors controlling exokarst morpho...
Abstract UDC: 551.4.(495) Kyriaki Papadopoulou-Vrynioti: The role of epikarst in the morphogenesis o...