Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Petra Gostinčar"'
Autor:
Petra Gostinčar, Uroš Stepišnik
Publikováno v:
Acta Geographica Slovenica, Vol 63, Iss 1, Pp 111-129 (2023)
This study investigates the spatial distribution of karst in Slovenia using advanced GIS technologies and accurate lithology, hydrology, and digital relief data. Previous approaches led to an incomplete understanding of karst distribution, as they fo
Externí odkaz:
https://doaj.org/article/4592ee32cdfe4aac89c664f9a9f3a6de
Autor:
Uroš Stepišnik, Petra Gostinčar
Publikováno v:
Acta Geographica Slovenica, Vol 60, Iss 2, Pp 91-150 (2020)
Within the area of Upper Pivka there is a number of intermittent lakes because of oscillation of water table level close to the surface i.e. shallow karst. Our survey was focused on morphogenetic interpretation of depressions hosting intermittent lak
Externí odkaz:
https://doaj.org/article/0d0a1fd4de22402d9b82710272293bc2
Publikováno v:
Geologija, Vol 63, Iss 2, Pp 203-220 (2020)
Tracing with artificial tracers is a research method that gives very good results in examining the direction and characteristics of groundwater flow in karst aquifers. The first mention of such experiments in Slovenian karst dates back to history a
Externí odkaz:
https://doaj.org/article/cb88488aafbe43f68504307e6d3c8f7a
Autor:
Petra Gostinčar
Publikováno v:
Dela, Iss 35, Pp 27-44 (2011)
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
Externí odkaz:
https://doaj.org/article/45e0a59fb016496fbdaf8d00177fd266
Publikováno v:
Dela, Iss 28, Pp 29-42 (2007)
Na slovenskem krasu je več različnih tipov kontaktnega krasa. Najpogostejši je ponorni tip kontaktnega krasa, ki se pojavlja med fliši in apnenci. Najdaljši kontakt te vrste v Sloveniji je na območju Matarskega podolja v zahodni Sloveniji, kjer
Externí odkaz:
https://doaj.org/article/aa0e691234084982a542d3744b010f85
Publikováno v:
Acta Carsologica, Vol 41, Iss 1 (2012)
The Planina Polje is located in the northwestern part of Notranjsko Podolje, Slovenia. Annual floods cover the flattened floor of the polje at elevation 445 m a.s.l. and reach the depth of approximately 8 meters. Loamy sediments which were found on s
Externí odkaz:
https://doaj.org/article/a672bdf183884b65b25108c9eacfe278
Autor:
Uroš Stepišnik, Mateja Ferk, Petra Gostinčar, Luka Černuta, Karmen Peternelj, Tomaž Štembergar, Urša Ilič
Publikováno v:
Acta Carsologica, Vol 36, Iss 2 (2007)
Several types of contact karst are found within the Slovenian karst, but the most common is the ponor type, which usually appears between flysch and limestone. The most extensive contact of this type is in western Slovenia, in the area of Matarsko po
Externí odkaz:
https://doaj.org/article/f268d0bc072b4656a20df66517a91b18
Autor:
Petra Gostinčar, Manja Žebre, Petra Jamšek Rupnik, Eva Mencin Gale, Jernej Jež, Uroš Stepišnik, Jure Atanackov, Miloš Bavec
On a global scale, inventories and databases are gaining value and there is a demand for openly accessible and reusable data. Here presented GIS database of glacial geomorphological evidence is a compilation of all available glacial and other relevan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a26c489a2ac4cb0ecefabc7b0f08a755
https://doi.org/10.5194/icg2022-227
https://doi.org/10.5194/icg2022-227
Autor:
Petra Gostinčar, Uroš Stepišnik
Publikováno v:
Acta geographica Slovenica. 60:91-150
Within the area of Upper Pivka there is a number of intermittent lakes because of oscillation of water table level close to the surface i.e. shallow karst. Our survey was focused on morphogenetic interpretation of depressions hosting intermittent lak
Publikováno v:
Geologija, Vol 63, Iss 2, Pp 203-220 (2020)
Tracing with artificial tracers is a research method that gives very good results in examining the direction and characteristics of groundwater flow in karst aquifers. The first mention of such experiments in Slovenian karst dates back to history and