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Crkvice (Zenica)
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, hospi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Sovereign States
The following is a list providing an overview of sovereign states around the world with information on their status and recognition of their sovereignty. The 206 listed states can be divided into three categories based on membership within the United Nations System: 193 UN member states, 2 UN General Assembly non-member observer states, and 11 other states. The ''sovereignty dispute'' column indicates states having undisputed sovereignty (188 states, of which there are 187 UN member states and 1 UN General Assembly non-member observer state), states having disputed sovereignty (16 states, of which there are 6 UN member states, 1 UN General Assembly non-member observer state, and 9 de facto states), and states having a special political status (2 states, both in free association with New Zealand). Compiling a list such as this can be a complicated and controversial process, as there is no definition that is binding on all the members of the community of nations concerni ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mediterranean
The Mediterranean Sea is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin and almost completely enclosed by land: on the north by Western and Southern Europe and Anatolia, on the south by North Africa, and on the east by the Levant. The Sea has played a central role in the history of Western civilization. Geological evidence indicates that around 5.9 million years ago, the Mediterranean was cut off from the Atlantic and was partly or completely desiccated over a period of some 600,000 years during the Messinian salinity crisis before being refilled by the Zanclean flood about 5.3 million years ago. The Mediterranean Sea covers an area of about , representing 0.7% of the global ocean surface, but its connection to the Atlantic via the Strait of Gibraltar—the narrow strait that connects the Atlantic Ocean to the Mediterranean Sea and separates the Iberian Peninsula in Europe from Morocco in Africa—is only wide. The Mediterranean Sea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Military History Of Austria-Hungary
A military, also known collectively as armed forces, is a heavily armed, highly organized force primarily intended for warfare. It is typically authorized and maintained by a sovereign state, with its members identifiable by their distinct military uniform. It may consist of one or more military branches such as an army, navy, air force, space force, marines, or coast guard. The main task of the military is usually defined as defence of the state and its interests against external armed threats. In broad usage, the terms ''armed forces'' and ''military'' are often treated as synonymous, although in technical usage a distinction is sometimes made in which a country's armed forces may include both its military and other paramilitary forces. There are various forms of irregular military forces, not belonging to a recognized state; though they share many attributes with regular military forces, they are less often referred to as simply ''military''. A nation's military may f ... [...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 ( 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Downslope Wind
A katabatic wind (named from the Greek language, Greek word κατάβασις ''katabasis'', meaning "descending") is a drainage wind, a wind that carries high-density air from a higher elevation down a slope under the force of gravity. Such winds are sometimes also called fall winds; the spelling catabatic winds is also used. Katabatic winds can rush down elevated slopes at hurricane speeds, but most are not that intense and many are 10 Knot (unit), knots (18 km/h) or less. Not all downslope winds are katabatic. For instance, winds such as the Foehn wind, föhn and Chinook wind, chinook are rain shadow winds where air driven upslope on the Windward and leeward, windward side of a mountain range drops its moisture and descends Windward and leeward, leeward drier and warmer. Examples of true katabatic winds include the Bora (wind), bora in the Adriatic Sea, Adriatic, the Bohemian Wind or ''Böhmwind'' in the Ore Mountains, the Santa Ana wind, Santa Ana in southern Californi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jugo
Sirocco ( ), scirocco, or, rarely, siroc (see below) is a Mediterranean wind that comes from the Sahara and can reach hurricane speeds in North Africa and Southern Europe, especially during the summer season. Names ''Sirocco'' derives from '' šurūq'' (), verbal noun of '' šaraqa'', related to the East, ''aš-šarq''. Various names for this wind in other languages include: * it, scirocco * scn, sciroccu * es, siroco * ca, xaloc * mt, xlokk * oc, siròc or * el, σορόκος, sorókos, or romanized: sirókos * sq, Jugu (south) * hr, jugo, lit=southern, or rarely ''širok'' * lij, sciöco or * Libyan Arabic: , romanized: , which means 'coming from the Qibla' * arz, خمسين, Ḫamsīn, which means 'fifty' ('fifty-day wind') * aeb, شلوق, šlūq, probably from with the same meaning as ; or * ary, شرقي, lit=eastern, šarquiyy, pronounced širguī Development Siroccos arise from warm, dry, tropical air masses that are pulled northward by low- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bora (wind)
The bora is a northerly to north-easterly katabatic wind in areas near the Adriatic Sea. Similar nomenclature is used for north-eastern winds in other littoral areas of eastern Mediterranean and Black Sea basins. Name It is known in Greek as (''mpóra'', pronounced ''bora'') and Italian as . In English, the name ''bora'' is used. The Serbo-Croatian name and Slovene are not etymologically related to ''bora''; they derive from Common Slavic ''burja'' 'storm' (from the verb ''*burĭti''), and the meaning 'bora' developed later. The same root as ''bora'' is found in the name of the Greek mythological figure of Boreas (Βορέας), and the Modern Greek word for the north wind . Historical linguists speculate that the name may derive from a Proto-Indo-European root *''gworhx-'' 'mountain', which gave rise to Slavic ''gora'' and Sanskrit ''giri-'', both 'mountain'. Features The changeable bora can often be felt all over Adriatic Croatia, Montenegrin Littoral, the Slovenian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wind
Wind is the natural movement of air or other gases relative to a planet's surface. Winds occur on a range of scales, from thunderstorm flows lasting tens of minutes, to local breezes generated by heating of land surfaces and lasting a few hours, to global winds resulting from the difference in absorption of solar energy between the climate zones on Earth. The two main causes of large-scale atmospheric circulation are the differential heating between the equator and the poles, and the rotation of the planet (Coriolis effect). Within the tropics and subtropics, thermal low circulations over terrain and high plateaus can drive monsoon circulations. In coastal areas the sea breeze/land breeze cycle can define local winds; in areas that have variable terrain, mountain and valley breezes can prevail. Winds are commonly classified by their spatial scale, their speed and direction, the forces that cause them, the regions in which they occur, and their effect. Winds have various asp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bay Of Kotor
The Bay of Kotor ( Montenegrin and Serbian: , Italian: ), also known as the Boka, is a winding bay of the Adriatic Sea in southwestern Montenegro and the region of Montenegro concentrated around the bay. It is also the southernmost part of the historical region of Dalmatia. The bay has been inhabited since antiquity. Its well-preserved medieval towns of Kotor, Risan, Tivat, Perast, Prčanj and Herceg Novi, along with their natural surroundings, are major tourist attractions. The Natural and Culturo-Historical Region of Kotor was designated a UNESCO World Heritage Site in 1979. Its numerous Orthodox and Catholic churches and monasteries attract numerous religious pilgrims and other visitors. Geography The bay is about long with a shoreline extending . It is surrounded by two massifs of the Dinaric Alps: the Orjen mountains to the west, and the Lovćen mountains to the east. The narrowest section of the bay, the long Verige Strait, is only wide at its narrowest point. The bay ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Risan
Risan ( Montenegrin: Рисан, ) is a town in the Bay of Kotor, Montenegro. It traces its origins to the ancient settlement of Rhizon, the oldest settlement in the Bay of Kotor. Lying in the innermost portion of the bay, the settlement was protected from the interior by inaccessible limestone cliffs of the Orjen mountain, the highest range of eastern Adriatic, and through several following narrow straits in the Bay of Kotor from the open sea. While the Krivošije karst plateau that hangs steep above the narrow shores of Risan bay receives over 5000 mm rain annually (European record), several strong karst springs that form a short brook collect in the narrow cultivable belt at Risan. Etymology It possibly stands in connection with the modern Albanian term "rrahe", meaning "forest clearing". History The earliest mention of Rhizon dates back to the 4th century BC, as the main fortress in the Illyrian state where Queen Teuta took refuge during the Illyrian Wars. The de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring (hydrosphere)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels throu ... [...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] |
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