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Devetero Vrela
Devetero vrela (English ''Nine Sources'') is a short right tributary of the Ilomska river, below Petrovo Polje.Vojnogeografski institut, Ed. (1962): Šiprage (List karte 1:25.000, Izohipse na 20 m). Vojnogeografski institut, Beograd / Military Geographical Institute, Ed. (1962): Šiprage (map sheet 1: 25.000, Contour lines at 20 m). Military Geographical Institute, Belgrade. Although only a few hundred meters long, it is very rich in watercourse A stream is a continuous body of surface water flowing within the bed and banks of a channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are ...s, especially springs. This body of water is named after the nine sources at the same place, although it is difficult to confirm visually. References External links *https://www.google.ba/search?q=ilomska+maps&ie=utf-8&oe=utf-8&gws_rd=cr&ei=WU2VVPn5LYHkUpykhKgL *http://itouchmap.com/?r=b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ilomska
Ilomska is right tributary of the Ugar river in ( Bosnia). It is about in length, and its source is Vlašić Mountain. It is an essential body of water for surrounding wildlife. Ilomska flows between the Žežnička Greda (altitude ) and Javorak () mountains. It has a curved flow around Lisina () and Runjavica () mountains, through coniferous ( fir and spruce) and mixed spruce- beech woods. Its flow below Petrovo polje ( en, Peter's plain) has sharp curves. The richest right contributors are Manatovac (large stream), Mala Ilomska (Little Ilomska) and Devetero vrela (Nine springs), and left tributary Crna rijeka (Black River). At the Ravni Omar (mountain meadows), below Lisina Mountain, it enters a narrow highland continuing to “Korićanski most” (Korićani's Bridge), and a deep canyon below Korićanske stijene and Marića stijene (Marići's Rocks). After two attractive Ilomska waterfalls, the river flows into the Ugar, a few kilometers downstream from Vitovl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
English Language
English is a West Germanic language of the Indo-European language family, with its earliest forms spoken by the inhabitants of early medieval England. It is named after the Angles, one of the ancient Germanic peoples that migrated to the island of Great Britain. Existing on a dialect continuum with Scots, and then closest related to the Low Saxon and Frisian languages, English is genealogically West Germanic. However, its vocabulary is also distinctively influenced by dialects of France (about 29% of Modern English words) and Latin (also about 29%), plus some grammar and a small amount of core vocabulary influenced by Old Norse (a North Germanic language). Speakers of English are called Anglophones. The earliest forms of English, collectively known as Old English, evolved from a group of West Germanic (Ingvaeonic) dialects brought to Great Britain by Anglo-Saxon settlers in the 5th century and further mutated by Norse-speaking Viking settlers starting in the 8th and 9th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Petrovo Polje (Bosnia)
Petrovo field ( bs, Petrovo polje / Петрово поље, "Peter's Field") is a small field on Podvlašić plateau, as part of Vlašić mountain group, and it's positioned at an altitude of about 1140 meters to 1220 meters a.s.l. On the plateau there is the eponymous village, Petrovo Polje (), with several hamlets, including registered Đurđevina, Nikodinovići (east) and Petrovo Polje village in narrower sense, once the center of the local community. It stretches from Đurđevina (elevation 1243 m), with the Mala Ilomska (Small Ilomska) (east) to the proximity intersection of paved local roads of this village crossroad to Kneževo, Turbe and Imljani (west). To the north is bounded by a line beginning a steep slope into the valley of Vrbanja river, on the line of the peaks 1220 – 1140 m, and on south − Ilomska valley. Ravne nadbojine (Straight nadbojine) is the protruding part of the plateau towards Ilomska, with Nikodinovići. On the plateau there are a dozen perman ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Watercourse
A stream is a continuous body of surface water flowing within the bed and banks of a channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighted subterranean water, and surfaced groundwater (spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes that respond to geological, geomorphological, hydrological and biotic controls. Streams are important as conduits in the water cycle, instruments in groundwater ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring (hydrology)
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 through ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_nahe_dem_Weiherdamm_in_Wildbergerhütte.jpg "Click for more on -> Watercourse")
