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Polje
A polje, also karst polje or karst field, is a large flat plain found in karstic geological regions of the world, with areas usually . The name derives from the Slavic languages and literally means 'field', whereas in English ''polje'' specifically refers to a karst plain or karst field. In geology A polje, in geological terminology, is a large, flat-floored depression within karst limestone, whose long axis develops in parallel with major structural trends and can become several miles (tens of kilometers) long. Superficial deposits tend to accumulate along the floor. Drainage may be either by surface watercourses (as an ''open polje'') or by swallow holes (as a ''closed polje'') or ponors. Usually, the ponors cannot transmit entire flood flows, so many poljes become wet-season lakes. The structure of some poljes is related to the geological structure, but others are purely the result of lateral dissolution and planation. The development of poljes is fostered by any blockage i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Polje Inundado 02
A polje, also karst polje or karst field, is a large flat plain found in karstic geological regions of the world, with areas usually . The name derives from the Slavic languages and literally means 'field', whereas in English ''polje'' specifically refers to a karst plain or karst field. In geology A polje, in geological terminology, is a large, flat-floored depression within karst limestone, whose long axis develops in parallel with major structural trends and can become several miles (tens of kilometers) long. Superficial deposits tend to accumulate along the floor. Drainage may be either by surface watercourses (as an ''open polje'') or by swallow holes (as a ''closed polje'') or ponors. Usually, the ponors cannot transmit entire flood flows, so many poljes become wet-season lakes. The structure of some poljes is related to the geological structure, but others are purely the result of lateral dissolution and planation. The development of poljes is fostered by any blockage in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Popovo Polje
Popovo field ( sh-Latn-Cyrl, separator=" / ", Popovo polje, Попово поље, , ) is a ''polje'' (karstic field) in Bosnia and Herzegovina, located in a southernmost region of the country, near the Adriatic coast. Its size is . Popovo polje is one of the largest ''polje'' (karstic plains) in Bosnia and Herzegovina and the world, famous for its karstic phenomenons and features, and particularly the Trebišnjica river, which flows through the polje as the largest sinking river (also ''losing stream'', or ''influent stream'') in the world, as well as the Vjetrenica cave system, located to the west/south-western parts of the valley. History The Nikolić noble family and Sanković noble family held Popovo polje in the late Middle Ages. The Vojnović noble family hailed from Popovo polje. The Zavala Monastery was first mentioned in the 16th century. At the end of Ottoman rule in Herzegovina, the Muslibegović family had properties in Popovo polje. The Zavala Monastery is located ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Livanjsko Polje
Livanjsko polje (), located in Bosnia and Herzegovina, is the largest ''polje'' (karstic field) in the world. A typical example of karst polje encircled by tall peaks and mountain ranges, the field is characterized by many unique natural phenomenons and karstic features. Geography The field has an area of 45,868 hectare, 458.7 km², and an average width of 6 km. It is located at an average height of 720 m above sea level. The field is located in region of Tropolje, in the southwest of Bosnia and Herzegovina, and lies between the karstic mountains of Dinara and Kamešnica on the south, Tušnica mountain on the east, Cincar and Golija mountain on the north and Šator and Staretina mountain on the west. Buško Blato ''( Buško lake)'' lies to the southeast, and Ždralovac to the northwest. Ždralovac is a narrow corridor by which the Livno field is connected to the Grahovsko field, between the slopes of mountains Dinara, Kamešnica and Šator. Climate In th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Logatec Polje
The Logatec Karst Field or Logatec Polje (; sl, Logaško polje) is a karst field near Logatec in southwestern Slovenia (the traditional region of Inner Carniola). Geographically, it corresponds to the floor of the Logatec Basin ( sl, Logaška kotlina).Oblak-Polajnar, Majda. 1959Logaška kotlina kot geografska individualnost ''Geografski vestnik'' 31: 19–44. It lies at an elevation between and Mihevc, Pavle. 1992. Logaško polje. ''Enciklopedija Slovenije'', vol. 6, p. 312. Ljubljana: Mladinska knjiga. and encompasses about of mostly grassy terrain. Logaščica Creek, a losing stream, runs across the karst field and collects ambient water. The karst field often flooded in the past, and so land improvement was carried out. The northern part of the Logatec Karst Field is called the Empty Karst Field () and the main road from Logatec to Vrhnika runs across it, passing through the linden-lined section known as the Napoleon Avenue (). The southern part of the karst field is known as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karstic
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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glamoč
Glamoč ( sr-cyrl, Гламоч) is a town and municipality located in Canton 10 of the Federation of Bosnia and Herzegovina, an entity of Bosnia and Herzegovina. It is situated in southwestern Bosnia and Herzegovina, at the foothills of Staretina and Velika Golija mountains, and on the edge of the central part of the Glamoč Field. The municipality encompasses the town of Glamoč as a seat of the municipality and more than 50 villages and hamlets situated along the Field. It mainly covers an area of the historical and geographical region of Tropolje. Name During the Ottoman Empire, Ottoman era the town was recorded as Biograd (White town), Belgradčik and Biogradaz. Geography Climate The climate of Glamoč is classified as an oceanic climate (''Cfb'' in Köppen climate classification#GROUP C: Temperate/mesothermal climates, Köppen climate classification system), near the boundary of the humid continental climate. Glamoč has four separate seasons. Summers are warm, and winte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ličko Polje (Lika)
Ličko Polje () is a polje (karstic field) in the Lika region, located in Croatia. Being the largest in Croatia, the field covers an area of 465 km2, and consists of five smaller fields: Lipovo, Kosinjsko, Pazariško, Brezovo and Gospićko. The field is characterized by some inselbergs, among them Zir (852 m), Otež (745 m) and Debeljak (882 m). The population is engaged in crops and farming. Largest settlement is Gospić Gospić () is a town in the mountainous and sparsely populated region of Lika, Croatia. It is the administrative centre of Lika-Senj County. Gospić is located near the Lika River in the middle of a karst field ( Ličko Polje). Gospić is the .... References {{Dinaric Alps' karst fields Plains of Croatia Geology of Croatia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cerknica Polje
Lake Cerknica (; sl, Cerkniško jezero, german: Zirknitzer See) is an intermittent lake in the southern part of the Cerknica Polje, a karst polje in Inner Carniola, a region in southwestern Slovenia. The lake, oriented in the Dinaric direction from northwest to southeast, is present for the most part of the year. When full, it is the largest lake in the country. The plain is surrounded by the Javornik Hills () to the south and Slivnica () to the north, both belonging to Dinaric Alps. The area of the lake mainly reaches , but can reach up to and the surface level varies from to above sea level. The lake is an important wildlife resort, especially as a nesting place for many bird species. Botanically, it is distinguished by amphibious plants. It is therefore a part of two Natura 2000 areas of protection and the focus of the Inner Carniola Regional Park, which covers additional Natura 2000 areas in the broader region. The climate in the area is continental, with a mean temperature ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nevesinje
Nevesinje ( sr-cyrl, Невесиње) is a town and municipality located in the Republika Srpska entity of Bosnia and Herzegovina. As of 2013, the town has a population of 5,162 inhabitants, while the municipality has 12,961 inhabitants. Geography and climate Geography The municipality of Nevesinje covers and is located in southern part of Bosnia and Herzegovina. A large polje called Nevesinjsko polje dominates the municipality, and is encircled by mountains of Crvanj at the north-northeast, Prenj at the northwest, and Velež (Bosnia and Herzegovina), Velež at the south-southwest. The entire municipality, as well as the entire region of eastern Herzegovina beyond municipal borders, is an elevate at the average above the sea level. History The annals of the Patriarchal Monastery of Peć mentioned Nevesinje in 1219, which is the earliest appearance of Nevesinje in preserved historical sources. The ''župa'' (county) of Nevesinje was held by Serbian prince Stefan Konstantin betw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Duvno
Tomislavgrad (), also known by its former name Duvno (), is a town and municipality located in Canton 10 of the Federation of Bosnia and Herzegovina, an entity of Bosnia and Herzegovina. It mainly covers an area of the historical and geographical region of Tropolje. As of 2013, it has a population of 33,032 inhabitants. In the Roman Empire, Roman times it was known as Delminium. During the middle ages when it was part of Kingdom of Croatia (925–1102), Croatia and Kingdom of Bosnia, Bosnia, the town was known as Županjac, a name that remained until 1928, when it was changed to Tomislavgrad. In 1946, the town's name was again changed to Duvno, and in 1990, the name was returned to Tomislavgrad. Name The town name means literally "Tomislav town". The name was changed from Županjac to Tomislavgrad in 1928 by King of Yugoslavia, King Alexander I of Yugoslavia in tribute to his son Prince Tomislav of Yugoslavia, Prince Tomislav and also Tomislav of Croatia, the first King of Croat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dinaric Alps
The Dinaric Alps (), also Dinarides, are a mountain range in Southern and Southcentral Europe, separating the continental Balkan Peninsula from the Adriatic Sea. They stretch from Italy in the northwest through Slovenia, Croatia, Bosnia and Herzegovina, Serbia, Montenegro, and Kosovo to Albania in the southeast. The Dinaric Alps extend for approximately along the western Balkan peninsula from the Julian Alps of the northeast Italy, downwards to the Šar and Korab massif, where their direction changes. The Accursed Mountains, is the highest section of the entire Dinaric Alps; this section stretches from Albania to Kosovo and eastern Montenegro. Maja Jezercë is the highest peak and is located in Albania, standing at Metres above the Adriatic, above the Adriatic. The Dinaric Alps are one of the most rugged and extensive mountainous areas of Europe, alongside the Caucasus Mountains, Alps, Pyrenees, Carpathian Mountains and Scandinavian Mountains. They are formed largely of Mesoz ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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