Reovačka Greda
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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 karstified Orjen range, Reovačka greda consists mostly of limestone. Southern side of the ridge is used for trad climbing Traditional climbing (or Trad climbing) is a style of rock climbing in which the climber places all the necessary protection gear required to arrest any falls as they are climbing, and then removes it when the pitch is complete (often done b .... References {{Montenegro-geo-stub Krivošije Dinaric Alps Kotor Municipality Orjen ...
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Montenegro
) , image_map = Europe-Montenegro.svg , map_caption = , image_map2 = , capital = Podgorica , coordinates = , largest_city = capital , official_languages = Montenegrin , languages2_type = Languages in official use , languages2 = , ethnic_groups = , ethnic_groups_year = 2011 , religion = , religion_year = 2011 , demonym = Montenegrin , government_type = Unitary parliamentary republic , leader_title1 = President , leader_name1 = Milo Đukanović , leader_title2 = Prime Minister , leader_name2 = Dritan Abazović (acting) , leader_title3 = Speaker , leader_name3 = Danijela Đurović , legislature = Skupština , sovereignty_type = Establishment history , established_event1 = Principality of Duklja , established_date1 ...
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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 type ...
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Ridge
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed or other chance occurrences. This type of ridge is generally somewhat random in orientation, often ...
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Mount 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 ty ...
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Krivošije
Krivošije ( sr-cyrl, Кривошије, ) are a historical tribe and 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. Name It is speculated that the name of the region is derived from the last name Krivošić, which is mentioned in 15th century Ragusan sources. In Serbo-Croatian language, ''krivi'' (neutral form ''krivo'') means "bent" or "crooked" оr "guilty", while ''šije'' (singular: ''šija'') means "necks", and it may be derived from some ancestor with a deformity. It might also be derived from the word ''krv'' meaning blood, as in linked by blood relationships. Origin During William James Stillman's travels, an American Journalist, in 1904, he listed the Krivošije (''Crivoscians'') as a Slavonic tribe. Geogra ...
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Bijela Gora
Bijela Gora (Montenegrin Cyrillic , Бијела Гора, , 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 The chamois (''Rupicapra rupicapra'') or Alpine chamois is a species of goat-antelope native to mountains in Europe, from west to east, including the Alps, the Dinarides, the Tatra and the Carpathian Mountains, the Balkan Mountains, the Ril .... Bijela Gora is inhabited by Montenegrin tribes who belong to the Katun clans. Fir trees of Bijela Gora are ...
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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 ...
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Bosnia And Herzegovina
Bosnia and Herzegovina ( sh, / , ), abbreviated BiH () or B&H, sometimes called Bosnia–Herzegovina and often known informally as Bosnia, is a country at the crossroads of south and southeast Europe, located in the Balkans. Bosnia and Herzegovina borders Serbia to the east, Montenegro to the southeast, and Croatia to the north and southwest. In the south it has a narrow coast on the Adriatic Sea within the Mediterranean, which is about long and surrounds the town of Neum. Bosnia, which is the inland region of the country, has a moderate continental climate with hot summers and cold, snowy winters. In the central and eastern regions of the country, the geography is mountainous, in the northwest it is moderately hilly, and in the northeast it is predominantly flat. Herzegovina, which is the smaller, southern region of the country, has a Mediterranean climate and is mostly mountainous. Sarajevo is the capital and the largest city of the country followed by Banja Luka, Tu ...
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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. Nowadays virtually uninhabited, Crkvice was most notable as 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, post office, stables, an ...
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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 ( sr-cyrl, Кривошије, ) are a historical tribe and 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 tr ... References {{coord, 42, 34, N, 18, 38, E, type:city_region:ME_source:dewiki, display=title Krivošije Populated places in Kotor Municipality ...
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Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, 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 hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals 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, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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