2015
DOI: 10.3986/ac.v44i1.898
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Geological influence on the formation of Samar natural bridge and collapse valley of Ravna River from the NE Kučaj Mountains (Carpatho-Balkanides, eastern Serbia)

Abstract: Carević: Pomen geologije za nastanek naravnega mostu Samar in udorne doline Ravna Reka v severovzhodnem delu gore Kučaj (Karpatsko-Balkansko gorovje, vzhodna Srbija) V članku obavnavamo naravni most Samar in udorno dolino Ravna Reka v vzhodni Srbiji. Njun razvoj pojasnujemo s specifičnimi litološkimi in tektonskimi pogoji, procesi zakrasevanja in petrološko analizo. Posebej poudarimo povezavo med razvojem kraških površinskih oblik in geologijo območja. Glavni prispevek študije je concept, v katerem opišemo, ka… Show more

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Cited by 7 publications
(5 citation statements)
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“…Represents an imposing natural stone bridge made of Jurassic limestones (Figure 3a). It has a length of 6 m, an opening height of 15 m, and a width of 12 m. The overall height of the karst bridge is 24 m (Petrović and Carević 2015;Miljković et al 2020). It is protected as a natural monument of the III category, on an area of 40.20 ha (Miljković 2018).…”
Section: Gs5 Samar Karst Bridgementioning
confidence: 99%
“…Represents an imposing natural stone bridge made of Jurassic limestones (Figure 3a). It has a length of 6 m, an opening height of 15 m, and a width of 12 m. The overall height of the karst bridge is 24 m (Petrović and Carević 2015;Miljković et al 2020). It is protected as a natural monument of the III category, on an area of 40.20 ha (Miljković 2018).…”
Section: Gs5 Samar Karst Bridgementioning
confidence: 99%
“…Formation of natural bridges by roof collapse of through caves (Cvijić, 1918;1960) was described exactly on the case studies from this karstic area. After Cvijić, the genesis of through caves and natural bridges was the subject of many studies (Petrović & Gavrilović, 1969;Petrović, 1971;1974;Gavrilović, 1981;1998;2005;Manojlović, 1985;Ćalić-Ljubojević, 2000;2001;Petrović & Carević, 2015). One of the most conspicuous landforms within this group is the cave Pećina na Reci Zamni (Cave on the Zamna River; in further text: the Zamna Cave).…”
Section: Fig 1 Map Of Karst Units Within the Carpatho-balkanides Ofmentioning
confidence: 99%
“…Настанак прерасти урушавањем таваницa тунелских пећина (Цвијић, 1918; 1960) објашњен је баш на примеру прерасти из ове крашке регије. Након тога је генеза тунелских пећина и прерасти у Карпато-балканидима Србије била тема већег броја истраживања (Петровић & Гавриловић, 1969;Петровић, 1971;1974;Гавриловић, 1981;1998;2005;Манојловић, 1985;Ćalić-Ljubojević, 2000;2001;Petrović & Carević, 2015). Циљ овог рада је да се генеза једног од проучаваних локалитета, Пећине на реци Замни, проучи у светлу нових истраживања.…”
Section: уводunclassified
“…The range of its arch is 15 m and it is 14 m high. In addition, there is another natural stone bridge in Homolje -Osanica Bridge (both are protected by law as exceptional natural rarities) [11].…”
Section: Geological and Geo-morphological Tourism Featuresmentioning
confidence: 99%