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Pivka Basin
The Pivka Basin or the Pivka Valley, also simply Pivka, is a varied basin in southwestern Slovenia, lying between high Dinaric plateaus, the Karst Plateau, and the Brkini Hills. It covers an area of . To the northwest, it is bordered by Mt. Nanos, to the north, by Hrušica, to the east by the Javornik Hills and Mt. Snežnik, and to the west by the lower Slavina Plain and Tabor Hills. The lower part of the basin between Nanos and the Postojna Gate is known as the Lower Pivka Basin, and the upper part between Prestranek and Snežnik as the Upper Pivka Basin. Hydrology The Black Sea–Adriatic Sea drainage divide crosses the Pivka Basin, with the majority of water flowing to the Ljubljanica Basin. The Pivka River with its tributary the Nanoščica sinks in Postojna Cave. Part of the water flows to the Lokva River, which sinks below Predjama Castle, merges with the sinking rivers Belščica, Stranske Ponikve, and Šmihelske Ponikve, and flows into the sources of the Vipava Ri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the ''drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Divide
A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern. A triple divide is a point, often a summit, where three drainage basins meet. A ''valley floor divide'' is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides. The term ''height of land'' is used in Canada and the United States to refer to a drainage divide. It is frequently used in border descriptions, which are set according to the "doctrine of natural boundaries". In glaciated areas it often refers to a low point on a divide where it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Continental Climate
Continental climates often have a significant annual variation in temperature (warm summers and cold winters). They tend to occur in the middle latitudes (40 to 55 north), within large landmasses where prevailing winds blow overland bringing some precipitation, and temperatures are not moderated by oceans. Continental climates occur mostly in the Northern Hemisphere due to the large landmasses found there. Most of northern and northeastern China, eastern and southeastern Europe, Western and north western Iran, central and southeastern Canada, and the central and northeastern United States have this type of climate. Continentality is a measure of the degree to which a region experiences this type of climate. In continental climates, precipitation tends to be moderate in amount, concentrated mostly in the warmer months. Only a few areas—in the mountains of the Pacific Northwest of North America and in Iran, northern Iraq, adjacent Turkey, Afghanistan, Pakistan, and Central Asia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mediterranean Climate
A Mediterranean climate (also called a dry summer temperate climate ''Cs'') is a temperate climate sub-type, generally characterized by warm, dry summers and mild, fairly wet winters; these weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location. This climate type's name is in reference to the coastal regions of the Mediterranean Sea within the Mediterranean Basin, where this climate type is most prevalent. The "original" Mediterranean zone is a massive area, its western region beginning with the Iberian Peninsula in southwestern Europe and coastal regions of northern Morocco, extending eastwards across southern Europe, the Balkans, and coastal Northern Africa, before reaching a dead-end at the Levant region's coastline. Mediterranean climate zones are typically located along the western coasts of landmasses, between roughly 30 and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ponor
A ponor is a natural opening where surface water enters into underground passages; they may be found in karst landscapes where the geology and the geomorphology is typically dominated by porous limestone rock. Ponors can drain stream or lake water continuously or can at times work as springs, similar to estavelles. Morphologically, ponors come in forms of large pits and caves, large fissures and caverns, networks of smaller cracks, and sedimentary, alluvial drains. Etymology The name for the karst formation ponor comes from Croatian and Slovene. It derives from the proto-Slavic word ''nora'', meaning ''pit'', ''hole'', ''abyss''; the English word ''narrow'' probably has the same origin. Several places in southeast Europe (Bulgaria, Croatia, Czech Republic, Hungary, Romania, Montenegro, Slovenia) bear the name ''Ponor'' due to associated karst openings. Description Whereas a sinkhole (doline) is a depression of surface topography with a pit or cavity directly underneath, a pon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst Field
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 earlie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bifurcation Lake
A bifurcation lake is a lake that has outflows into two different drainage basins and thus the drainage divide cannot be defined exactly because it is situated in the middle of the lake. Examples Vesijako (the name ''Vesijako'' actually means "drainage divide") and Lummene in the Finnish Lakeland are two nearby lakes in Finland. Both drain in two directions: into the Kymijoki basin that drains into the Gulf of Finland and into the Kokemäenjoki basin that drains into the Gulf of Bothnia. Similarly the lakes Isojärvi (Satakunta), Isojärvi and Inhottu in the Karvianjoki basin in the Satakunta region of western Finland both have two outlets: from Inhottu the waters flow into the Gulf of Bothnia through the Eteläjoki River in Pori and into lake Isojärvi through the Pomarkunjoki River. From lake Isojärvi the waters flow to the Gulf of Bothnia through the Pohjajoki river in Pori and through the Merikarvianjoki river in Merikarvia. In the Karvianjoki basin there have formerly been ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sajevče
Sajevče () is a small village in the hills south of Hruševje in the Municipality of Postojna in the Inner Carniola region of Slovenia Slovenia ( ; sl, Slovenija ), officially the Republic of Slovenia (Slovene: , abbr.: ''RS''), is a country in Central Europe. It is bordered by Italy to the west, Austria to the north, Hungary to the northeast, Croatia to the southeast, an .... References External linksSajevče on Geopedia Populated places in the Municipality of Postojna {{Postojna-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reka (river)
The Reka (literally, 'river' in Slovene), also the Inner Carniola Reka ( sl, Notranjska Reka), is a river that starts as Big Creek ( hr, Vela voda) in Croatia, on the southern side of Mount Snežnik, and flows through western Slovenia, where it is also initially known as Big Creek (). The river is long, of which is in Slovenia. At the village of Škocjan it disappears underground through Škocjan Caves (a UNESCO World Heritage Site), flowing underneath the Slovenian Karst. The river continues as part of the Timavo The Timavo River, known in Slovene as the ' or ', is a two-kilometre stream in the Province of Trieste. It has four sources near San Giovanni ( sl, Štivan) near Duino ( sl, Devin) and outflows in the Gulf of Panzano (part of the Gulf of Trieste ... in Italy. Tracer studies have shown that it also feeds springs elsewhere on the Adriatic Coast between Trieste and Monfalcone. It has a pluvial regime. References External links * * Condition of Reka aCerkvenikov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vipava (river)
The Vipava (in Slovene) or Vipacco (in Italian) or ''Wipbach'' / ''Wippach'' (in German) is a river that flows through western Slovenia and north-eastern Italy. The river is in length, of which 45 km in Slovenia. After entering Italy Italy ( it, Italia ), officially the Italian Republic, ) or the Republic of Italy, is a country in Southern Europe. It is located in the middle of the Mediterranean Sea, and its territory largely coincides with the homonymous geographical ... it joins the Isonzo/Soča in the Municipality of Savogna d'Isonzo. This is a rare river with a delta source, formed by nine main springs. The Battle of the Frigidus was fought near the river, which was named ''Frigidus'' ('cold') by the Romans. It has a pluvial-nival regime in its upper course and a pluvial regime in its lower course. See also * List of rivers of Slovenia References External links * * Condition of Vipava aDolenje [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Predjama Castle
300px, Predjama Castle Predjama Castle ( sl, Predjamski grad or , German: '' Höhlenburg Lueg'', it, Castel Lueghi) is a Renaissance castle built within a cave mouth in south-central Slovenia, in the historical region of Inner Carniola. It is located in the village of Predjama, approximately 11 kilometres from the town of Postojna and 9 kilometres from Postojna Cave. History of the castle The castle was first mentioned in 1274 with the German name ''Luegg'', when the Patriarch of Aquileia built the castle in Gothic style. The castle was built under a natural rocky arch high in the stone wall to make access to it difficult. It was later acquired and expanded by the Luegg noble family, also known as the Knights of Adelsberg (the German name of Postojna). Legend of Erasmus of Lueg The castle became known as the seat of the knight Erasmus of Lueg (or Luegg, Luegger), lord of the castle in the 15th century and a renowned robber baron. He was the son of the imperial governor of T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lokva
Lokva ( sr, Локва) is a village in the municipality of Knjaževac, Serbia Serbia (, ; Serbian language, Serbian: , , ), officially the Republic of Serbia (Serbian language, Serbian: , , ), is a landlocked country in Southeast Europe, Southeastern and Central Europe, situated at the crossroads of the Pannonian Bas .... According to the 2002 census, the village has a population 69 people.Popis stanovništva, domaćinstava i Stanova 2002. Knjiga 1: Nacionalna ili etnička pripadnost po naseljima. Republika Srbija, Republički zavod za statistiku Beograd 2003. References Populated places in Zaječar District {{ZaječarRS-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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