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Reovačka Greda
Reovačka greda ( sr-cyrl, Реовачка греда) is a ridge of Mount Orjen located in Krivošije, in southwestern Montenegro, separating the Bijela Gora plateau from the rest of the Orjen range. The ridge stretches for 17 kilometres from Vučji zub peak on the west, at the border of Montenegro and Bosnia and Herzegovina, and the villages of Crkvice and Malov Do on the east. Its highest peak is Pazua, which is 1,769 metres high. Situated in the heavily karst, karstified Orjen range, Reovačka greda consists mostly of limestone. Southern side of the ridge is used for trad climbing. References {{Montenegro-geo-stub Krivošije Dinaric Alps Kotor Municipality Orjen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Montenegro
, image_flag = Flag of Montenegro.svg , image_coat = Coat of arms of Montenegro.svg , coa_size = 80 , national_motto = , national_anthem = () , image_map = Europe-Montenegro.svg , map_caption = , image_map2 = , capital = Podgorica , coordinates = , largest_city = capital , official_languages = Montenegrin language, Montenegrin , languages2_type = Languages in official use , languages2 = , ethnic_groups = , ethnic_groups_ref = , ethnic_groups_year = 2023 census , religion = , religion_ref = , religion_year = 2023 census , demonym = Montenegrins, Montenegrin , government_type = Unitary parliamentary republic , leader_title1 = President of Montenegro, President , leader_name1 = Jakov Milatović , leader_title2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orjen
Orjen (Serbian Cyrillic: Орјен, ) is a transboundary Dinaric Mediterranean limestone mountain range, located between southernmost Bosnia and Herzegovina and southwestern Montenegro. Its highest peak is Veliki kabao, which stands at . The Orjen Peak is the highest peak in the ''Sub-Adriatic'' Dinarides. The massif of Orjen lies east to south-east of Trebinje in Bosnia and Herzegovina and north-west of Risan in Bay of Kotor (Boka Kotorska). From the town of Risan, situated at the innermost protected part of the bay, a well-engineered road, at first metalled, with many hairpin bends climbs to about 1600 m, over to the interior. At the main summit of Orjen and the surrounding ridges and high plateaus the action of quaternary glaciation is evident. During the Ice Age, long valley glaciers receded from Orjen to the Bay of Kotor and surrounding poljes. Hollowing U-shaped valleys and cirques in their course. Glaciers also shaped jagged peaks and ridges. Glacial and karst t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ridge
A ridge is a long, narrow, elevated geomorphologic landform, structural feature, or a combination of both separated from the surrounding terrain by steep sides. The sides of a ridge slope away from a narrow top, the crest or ridgecrest, with the terrain dropping down on either side. The crest, if narrow, is also called a ridgeline. Limitations on the dimensions of a ridge are lacking. Its height above the surrounding terrain can vary from less than a meter to hundreds of meters. A ridge can be either depositional, erosional, tectonic, or a combination of these in origin and can consist of either bedrock, loose sediment, lava, or ice depending on its origin. A ridge can occur as either an isolated, independent feature or part of a larger geomorphological and/or structural feature. Frequently, a ridge can be further subdivided into smaller geomorphic or structural elements. Classification As in the case of landforms in general, there is a lack of any commonly agreed clas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Orjen
Orjen (Serbian Cyrillic: Орјен, ) is a transboundary Dinaric Alps, Dinaric Mediterranean limestone mountain range, located between southernmost Bosnia and Herzegovina and southwestern Montenegro. Its highest peak is Veliki kabao, which stands at . The Orjen Peak is the highest peak in the ''Sub-Adriatic'' Dinaric Alps, Dinarides. The massif of Orjen lies east to south-east of Trebinje in Bosnia and Herzegovina and north-west of Risan in Bay of Kotor (Boka Kotorska). From the town of Risan, situated at the innermost protected part of the bay, a well-engineered road, at first metalled, with many hairpin bends climbs to about 1600 m, over to the interior. At the main summit of Orjen and the surrounding ridges and high plateaus the action of quaternary glaciation is evident. During the Last Glacial Period, Ice Age, long valley glaciers receded from Orjen to the Bay of Kotor and surrounding karst field, poljes. Hollowing U-shaped valleys and cirques in their course. Glacier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Krivošije
Krivošije ( cyrl, Кривошије, ) is a microregion in southwestern Montenegro, located on a high plateau belonging to the Orjen mountain range, north of the Bay of Kotor. Krivošije was historically located at a tripoint between the Principality of Montenegro, Austro-Hungarian (formerly Venetian) Bay of Kotor and Ottoman Sanjak of Herzegovina. Geography Krivošije are a mountainous karst region above Risan, located at around 1000 metres above the sea level, spanning on 114 km2 of land. It is a high plateau on the northern and eastern branches of Mount Orjen (1894 m) in southwest Montenegro, near in the hinterland of the Bay of Kotor. A significant geological and geomorphological feature of the region are the glacial deposits distributed across the whole of the plateau. They were deposited by valley glaciers coming from Orjen during the Ice Age. Krivošije is the region with the greatest rainfall in Europe. Reovačka greda is a mountain ridge located near C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bijela Gora
Bijela Gora (Montenegrin Cyrillic , Бијела Гора, , literal translation, lit. "White Mountain") is a karstic high plateau between 1200–1500 m on the northern side of Mount Orjen in Montenegro. At 1862 m, Velika Jastrebica is the highest summit. It bears heavy glacial traces as a huge ice cap covered it during the last ice age. Sparsely inhabited pastures and vast virgin beech-fir forests are major resources. Also, endemic Dinaric calcareous Silver Fir forests are found at Bijela Gora with rare endemic plants, such as Bosnian pine. Fauna of Bijela Gora includes brown bears, wolves, deer, boars, and a small population of chamois. Bijela Gora is inhabited by Montenegrin tribes who belong to the Katun clans. Fir trees of Bijela Gora are sung about in local folk songs. References Mountains of Montenegro Orjen {{Montenegro-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vučji Zub
Vučji zub (trans. "Wolf's tooth") is at 1805 m one of the higher peaks in the Orjen masif. The boundary between the Ottoman Empire, Austro-Hungarian Empire and the principality of Montenegro ran across Vučji zub until 1879. Vučji zub is still today the border stone between Montenegro and Bosnia and Herzegovina. Vučji zub resembles a horn and is an interesting climbing destination in the Orjen range. See also * Orjen Orjen (Serbian Cyrillic: Орјен, ) is a transboundary Dinaric Mediterranean limestone mountain range, located between southernmost Bosnia and Herzegovina and southwestern Montenegro. Its highest peak is Veliki kabao, which stands at ... {{DEFAULTSORT:Vucji Zub Mountains of Montenegro Bosnia and Herzegovina–Montenegro border Orjen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bosnia And Herzegovina
Bosnia and Herzegovina, sometimes known as Bosnia-Herzegovina and informally as Bosnia, is a country in Southeast Europe. Situated on the Balkans, Balkan Peninsula, it borders Serbia to the east, Montenegro to the southeast, and Croatia to the north and southwest, with a coast on the Adriatic Sea in the south. Bosnia (region), Bosnia has a moderate continental climate with hot summers and cold, snowy winters. Its geography is largely mountainous, particularly in the central and eastern regions, which are dominated by the Dinaric Alps. Herzegovina, the smaller, southern region, has a Mediterranean climate and is mostly mountainous. Sarajevo is the capital and the largest city. The area has been inhabited since at least the Upper Paleolithic, with permanent human settlement traced to the Neolithic cultures of Butmir culture, Butmir, Kakanj culture, Kakanj, and Vučedol culture, Vučedol. After the arrival of the first Proto-Indo-Europeans, Indo-Europeans, the area was populated ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crkvice
Crkvice ( sr-cyrl, Црквице, ) is a village in Krivošije, on the outskirts of Mount Orjen in Montenegro, and the wettest inhabited place in Europe. Despite the fact that it is nowadays virtually uninhabited, Crkvice was most notable the location of a large Austro-Hungarian military base which was active until the end of World War I, when Montenegro regained control of the area. History During the rule of the Austria-Hungary over the Krivošije region, Crkvice was used up as the base military camp. The fortifications, including Fort Kom (''Crkvice Ostfort'') and Fort Stražnik (''Crkvice Westfort''), were built by the Austro-Hungarian soldiers in the first half of the 19th century, and represented the furthest fortification towards the border with Montenegro. During that period, over 150 objects were built in Crkvice, including military training grounds, hotel, tennis courts, bowling alley, football pitch with stands for 1,000 spectators, cinema, church, bakery, hospital, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Malov Do
Malov Do (Montenegrin Cyrillic: Малов До) is a village in Krivošije in southwestern Montenegro, located near the former settlement and Austro-Hungarian military base of Crkvice. According to the 2011 census, the village had 8 inhabitants. The village church, Church of the Nativity of the Virgin Mary, was built in 1831. See also * Crkvice * Krivošije Krivošije ( cyrl, Кривошије, ) is a microregion in southwestern Montenegro, located on a high plateau belonging to the Orjen mountain range, north of the Bay of Kotor. Krivošije was historically located at a tripoint between the Prin ... References {{coord, 42, 34, N, 18, 38, E, type:city_region:ME_source:dewiki, display=title Krivošije Populated places in Kotor Municipality ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
