Rock Formations Of Bulgaria
Bulgaria is a country in south-eastern Europe situated in the north-eastern part of the Balkan Peninsula. The country has a great variety of topographical features and diverse landscape ranging from the Alpine climate, Alpine snow-capped peaks in Rila, Pirin and the Balkan Mountains to the mild and sunny Bulgarian Black Sea Coast, Black Sea coast; from the typically continental climate, continental Danubian Plain (Bulgaria), Danubian Plain in the north to the strong Mediterranean climate, Mediterranean climatic influence in the valleys of Macedonia (region), Macedonia and the lowlands in the southernmost parts of Thrace. The diverse morphological, climatic and hydrological conditions of Bulgaria favour the formation of a large number of geological features. Partial list of rock formations in Bulgaria See also *Geography of Bulgaria *List of protected areas of Bulgaria *List of mountains in Bulgaria *List of caves in Bulgaria *List of islands of Bulgaria *List of lakes of Bul ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Rhodope Mountains
The Rhodopes (; , ; , ''Rodopi''; ) are a mountain range in Southeastern Europe, and the largest by area in Bulgaria, with over 83% of its area in the southern part of the country and the remainder in Greece. Golyam Perelik is its highest peak at . The mountain range gives its name to the terrestrial ecoregion Rodope montane mixed forests that belongs in the temperate broadleaf and mixed forests biome and the Palearctic realm. The region is particularly notable for its karst areas with their deep river gorges, large caves and specific sculptured forms, such as the Trigrad Gorge. A significant part of Bulgaria's hydropower resources are located in the western areas of the range. There are a number of hydro-cascades and dams used for electricity production, irrigation, and as tourist destinations. Name and mythology The name of the Rhodope Mountains is of Thracian origin. Rhod-ope (Род-oпа) is interpreted as the first name of a river, meaning "rusty/reddish river", wher ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Chiren (village)
Chiren () is a village located in northwestern Bulgaria. It is a part of Vratsa Municipality, Vratsa Province. Geography The village is located approximately 15 kilometers to the north of town of Vratsa. Chiren is popular with places "Bojia most" ( 'God's bridge') and "Tigancheto" ( 'little frying pan'). These places are natural forms carved by the rivers. The other natural landmark in this area is the cave "Ponora" ({{langx, bg, Понора). Honour Chiren Heights in Graham Land, Antarctica Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean (also known as the Antarctic Ocean), it contains the geographic South Pole. ... are named after the village. Villages in Vratsa Province ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Vratsa Province
Vratsa Province ( ''Oblast Vraca'', former name Vraca okrug) is a Bulgarian province located in the northwestern part of the country, between Danube river in the north and Stara Planina mountain in the south. It is named after its main town: Vratsa. As of 2016, the province had a population of 170 367, on territory of . Municipalities The Vratsa Province contains ten municipalities (singular: община, ''obshtina'' - plural: общини, ''obshtini''). The following table shows the names of each municipality in English and Cyrillic, the main town (in bold) or village, and the population of each as of 2016. Demographics The Vratsa province had a population of 243,036 according to a 2001 census, of which were male and were female. As of the end of 2009, the population of the province, announced by the Bulgarian National Statistical Institute, numbered 196,829 of which are inhabitants aged over 60 years. [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Natural Arch
A natural arch, natural bridge, or (less commonly) rock arch is a natural landform where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs, Cliffed coast, coastal cliffs, Fin (geology), fins or Stack (geology), stacks are subject to erosion from the sea, rivers or weathering (subaerial processes). Most natural arches are formed from narrow fins and sea stacks composed of sandstone or limestone with steep, often vertical, cliff faces. The formations become narrower due to erosion over geologic time scales. The softer rock stratum erodes away creating rock shelters, or alcoves, on opposite sides of the formation beneath the relatively harder stratum, or caprock, above it. The alcoves erode further into the formation eventually meeting underneath the harder caprock layer, thus creating an arch. The erosional processes exploit weaknesses in the softer rock layers making cracks larger and removing material more quickly than the caprock; ho ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Vidin Province
Vidin Province () is the northwesternmost province of Bulgaria. It borders Serbia to the west and Romania to the northeast, and its administrative centre is the city of Vidin on the Danube river. The area is divided into 11 municipalities. As of 2023, the province had a population of 72,754. There are remains of many castles, including Baba Vida, one of the last Bulgarian strongholds during the Ottoman invasion and the Belogradchik fortress. Municipalities The Vidin Province contains 11 municipalities (singular: община, ''obshtina'' - plural: общини, ''obshtini''). The following table shows the names of each municipality in English and Cyrillic, the main town (in bold) or village, and the population of each as of December 2009. Geography The territory of the province includes the most western parts of the Danubian Plain and Stara Planina, while the Danube forms the border with Romania. The slopes of Stara Planina are covered with dense forests, lush mead ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Belogradchik
Belogradchik (; ) is a town in Vidin Province, northwestern Bulgaria, and is the administrative centre of the homonymous municipality. The town is situated in the foothills of the Balkan Mountains just east of the Serbian border and about 50 km south of the Danube River. The town is close to the Belogradchik Rocks, which are major tourist attraction. , it had a population of 4,601. Geography Belogradchik is situated at an altitude of 520 m in the western part of the Fore-Balkan, a mountainous chain straddling north of and in parallel with the Balkan Mountains. The town lies next to the Belogradchik Rocks, a major rock formation reaching some 30 km in length that contains outcrops reaches up to 100 m in height, which form a dramatic outline of the town. Close to the town is the source of the Gradska reka, a tributary of the Salashka reka, itself a tributary of the Archar of the Danube drainage. Belogradchik falls within the temperate continental cli ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Belogradchik Rocks
The Belogradchik Rocks (, ''Belogradchishki skali'') are a group of strangely shaped sandstone and conglomerate rock formations located on the western slopes of the Balkan Mountains (''Stara Planina'') near the town of Belogradchik in northwest Bulgaria. The rocks vary in color from primarily red to yellow; some of the rocks reach up to 200 m in height. Many rocks have fantastic shapes and are associated with interesting legends. They are often named after people or objects they are thought to resemble. The Belogradchik Rocks have been declared a Natural Landmark by the Bulgarian government and are a major tourist attraction in the region. They are the only habitat of the critically endangered Bulgarian endemic plant '' Hieracium belogradcense''. Geography The Belogradchik Rocks are spread over the western part of the Balkan Mountains and cover an area of . They extend from the village of Rabisha in the west to the village of Belotintsi in the east. The central group of roc ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |