Mali Krš
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Mali Krš
Mali Krš ( sr-Cyrl, Мали Крш) is a mountain in eastern Serbia. Its highest peak, Garvan, has an elevation of 929 metres above sea level. While not particularly rugged, Mali Krš is remote, hidden between nearby mountains of Liškovac, Veliki Krš and Homolje Mountains. Like nearby Veliki Krš and Stol, Mali Krš is dominated by karst Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. Ther ... formations, and they are collectively known as "Gornjanski Kras". Mali Krš has an elongated karst ridge at the top section. References External linksSpecies of Mali kršBiking and photo tour through Gornjanski kras

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Serbia
, image_flag = Flag of Serbia.svg , national_motto = , image_coat = Coat of arms of Serbia.svg , national_anthem = () , image_map = , map_caption = Location of Serbia (green) and the claimed but uncontrolled territory of Kosovo (light green) in Europe (dark grey) , image_map2 = , capital = Belgrade , coordinates = , largest_city = capital , official_languages = Serbian language, Serbian , ethnic_groups = , ethnic_groups_year = 2022 , religion = , religion_year = 2022 , demonym = Serbs, Serbian , government_type = Unitary parliamentary republic , leader_title1 = President of Serbia, President , leader_name1 = Aleksandar Vučić , leader_title2 = Prime Minister of Serbia, Prime Minister , leader_name2 = Đuro Macut , leader_title3 = Pres ...
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Serbian Carpathians
Serbian Carpathians () is a mountain range in eastern Central Serbia, located in Central Europe. It presents an extension of proper Carpathian Mountains across the Danube, connecting them with the Balkan Mountains in the southeast. They stretch in north–south direction in eastern Serbia, east of the Great Morava valley and west of the White Timok Valley and north of the Nišava Valley. The mountains are 800–1500 m high, and dominated by karst limestone geologic features, the highest one being Rtanj Mountain (1,565 m). Definitions Under the strict definition (as defined by the Serbian Academy of Sciences and Arts and adopted by the Carpathian Convention), Serbian part of the Carpathian Mountains covers only 732 km2, or less than 1% of the total Carpathian area. That part encompasses the southern bank of the Iron Gate and the area of Đerdap National Park. The extreme points of so defined Carpathian area in Serbia are Tekija in the north, in the south, Golubac ...
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Mountains Of Serbia
Serbia is mountainous, with complex Geology of Serbia, geology and parts of several mountain ranges: Dinaric Alps in the southwest, the northwestern corner of the Rila-Rhodope Mountains in the southeast of the country, Serbian Carpathians, Carpathian Mountains in the northeast, and Balkan Mountains and the Vlaška planina, easternmost section of Sredna gora, Srednogorie Mountain range, mountain chain system in the east, separated by a group of dome mountains along the Great Morava, Morava river valley. The northern province of Vojvodina lies in the Pannonian plain, with several Pannonian island mountains. Mountains of Kosovo are listed in a list of mountains in Kosovo, separate article. List This is a list of mountains and their highest peaks in Serbia, excluding Kosovo. Mountains that have several major peaks are listed separately.http://solair.eunet.rs/~s.ilic/planine.txt (Adopted with author's permission.) Peaks over 2,000 meters The following lists only those m ...
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Liškovac
Liškovac (Serbian Cyrillic: Лишковац) is a mountain in eastern Serbia, between towns of Majdanpek and Donji Milanovac. Its highest peak ''Veliki Liškovac'' has an elevation of 803 meters above sea level. Along with Miroč, Liškovac is part of the Iron Gate of the Danube river. It is located in the Đerdap national park Đerdap National Park () stretches along the right bank of the Danube River from the Golubac Fortress () to the dam near Novi Sip, Serbia. It was established in 1974 and spreads on . The park management office is in the town of Donji Milanovac o .... References Mountains of Serbia Serbian Carpathians {{serbia-geo-stub ...
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Veliki Krš
Veliki Krš ( sr-Cyrl, Велики Крш) is a mountain in eastern Serbia, near the city of Bor. Its highest peak ''Veliki Krš'' has an elevation of 1,148 meters above sea level. Like nearby Mali Krš and Stol, it is dominated by karst Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. Ther ... formations, and they are collectively known as "Gornjanski Kras". Veliki Krš has an elongated karst ridge at the top section. References Mountains of Serbia Serbian Carpathians {{serbia-geo-stub ...
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Stol (Serbian Carpathians)
Stol ( sr-Cyrl, Стол) is a mountain in eastern Serbia, near the town of Bor. Its highest peak has an elevation of 1,156 meters above sea level. Like nearby Veliki Krš and Mali Krš, Stol has a number of pronounced karst Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. Ther ... formations. There is a mountain hut with around 35 beds, maintained by the mountaineering society Crni Vrh from Bor. Rock climbing on Stol Stol is a developed climbing spot, with 68 bolted routes, difficulties from 4c to 8a+. References External links Tamo gde se Boru vraća oduzeto TK Info Bor, Serbia Mountains of Serbia Serbian Carpathians {{serbia-geo-stub ...
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Karst
Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering-resistant rocks such as quartzite given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. In regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's Oil and gas reserves and resource quantification, hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology ...
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Mountains Of Serbia
Serbia is mountainous, with complex Geology of Serbia, geology and parts of several mountain ranges: Dinaric Alps in the southwest, the northwestern corner of the Rila-Rhodope Mountains in the southeast of the country, Serbian Carpathians, Carpathian Mountains in the northeast, and Balkan Mountains and the Vlaška planina, easternmost section of Sredna gora, Srednogorie Mountain range, mountain chain system in the east, separated by a group of dome mountains along the Great Morava, Morava river valley. The northern province of Vojvodina lies in the Pannonian plain, with several Pannonian island mountains. Mountains of Kosovo are listed in a list of mountains in Kosovo, separate article. List This is a list of mountains and their highest peaks in Serbia, excluding Kosovo. Mountains that have several major peaks are listed separately.http://solair.eunet.rs/~s.ilic/planine.txt (Adopted with author's permission.) Peaks over 2,000 meters The following lists only those m ...
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