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Logar Valley, Slovenia
The Logar Valley ( sl, Logarska dolina, ''Logarjeva dolina''Mišič, Franc. 1938. "O ledinskih in hišnih imenih okoli Solčave." ''Časopis za zgodovino in narodopisje'' 33(3/4): 191–201, p. 197.) is a valley in the Kamnik Alps, in the Municipality of Solčava, Slovenia. The Slovene name for the valley is of relatively recent coinage and is derived from the Logar Farm, which in turn is derived from ''log'' (literally, 'swampy meadow'). In 1987, the valley received protected status as a Landscape Park (protected area), landscape park encompassing . Geography The Logar Valley is a typical U-shaped glacial valley. It is divided into three parts. The lower part is named ''Log'', the middle part ''Plest'' or ''Plestje'' (it is a mostly wooded area), and the upper part ''Kot'' (literally 'cirque') or ''Ogradec'' (it is a wooded area with scree slopes). Altogether 35 people live on the isolated farmsteads in the valley. Peaks The Logar Valley is ringed by the following peaks: Strelo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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, and the Adriatic Sea to the southwest. Slovenia is mostly mountainous and forested, covers , and has a population of 2.1 million (2,108,708 people). Slovenes constitute over 80% of the country's population. Slovene, a South Slavic language, is the official language. Slovenia has a predominantly temperate continental climate, with the exception of the Slovene Littoral and the Julian Alps. A sub-mediterranean climate reaches to the northern extensions of the Dinaric Alps that traverse the country in a northwest–southeast direction. The Julian Alps in the northwest have an alpine climate. Toward the northeastern Pannonian Basin, a continental climate is more pronounced. Ljubljana, the capital and largest city of Slovenia, is geogr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brana (mountain)
Brana () is a ridge mountain of the Kamnik Alps in northern Slovenia. It is located between the Logar Valley to the north and the Kamnik Bistrica Valley to the south. The mountain is part of the central Kamnik group, a long ridge that includes the highest peaks of the range such as Grintovec, Kočna, and Skuta. Brana is sometimes climbed as part of a long traverse of the entire Kamnik ridge. Starting points * Kamnik, the Kamnik Bistrica Valley * Solčava, the Logar Valley Routes * 2½ hrs from the Frischauf Lodge at Okrešelj at * 1 hr from the Kamnik Saddle Lodge The Kamnik Saddle Lodge ( sl, Koča na Kamniškem sedlu; ) is a mountain hostel located just below Kamnik Saddle (), with Mount Brana to its west and Mount Planjava to its east, and the Kamnik Bistrica Valley to its south. On its north is a ste ... at References External links * Brana on hribi.net Route Description and Photos (slo) Mountains of the Kamnik–Savinja Alps Mountains of Upper Carniola ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys In The Kamnik–Savinja Alps
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landscape Parks In Slovenia
A landscape is the visible features of an area of Terrestrial ecoregion, land, its landforms, and how they integrate with Nature, natural or man-made features, often considered in terms of their aesthetic appeal.''New Oxford American Dictionary''. A landscape includes the physical elements of geophysically defined landforms such as (ice-capped) mountains, hills, water bodies such as rivers, lakes, Pond, ponds and the sea, living elements of land cover including indigenous vegetation, human elements including different forms of land use, buildings, and structures, and transitory elements such as lighting and weather conditions. Combining both their physical origins and the Culture, cultural overlay of human presence, often created over millennia, landscapes reflect a living synthesis of people and place that is vital to local and national identity. The character of a landscape helps define the self-image of the people who inhabit it and a sense of place that differentiates one ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys In Styria (Slovenia)
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. For ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Logar Valley (Slovenia)
The Logar Valley ( sl, Logarska dolina, ''Logarjeva dolina''Mišič, Franc. 1938. "O ledinskih in hišnih imenih okoli Solčave." ''Časopis za zgodovino in narodopisje'' 33(3/4): 191–201, p. 197.) is a valley in the Kamnik Alps, in the Municipality of Solčava, Slovenia. The Slovene name for the valley is of relatively recent coinage and is derived from the Logar Farm, which in turn is derived from ''log'' (literally, 'swampy meadow'). In 1987, the valley received protected status as a landscape park encompassing . Geography The Logar Valley is a typical U-shaped glacial valley. It is divided into three parts. The lower part is named ''Log'', the middle part ''Plest'' or ''Plestje'' (it is a mostly wooded area), and the upper part ''Kot'' (literally 'cirque') or ''Ogradec'' (it is a wooded area with scree slopes). Altogether 35 people live on the isolated farmsteads in the valley. Peaks The Logar Valley is ringed by the following peaks: Strelovec (), Krofička (), Ojstric ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burl
A burl (American English) or burr (British English) is a tree growth in which the grain has grown in a deformed manner. It is commonly found in the form of a rounded outgrowth on a tree trunk or branch that is filled with small knots from dormant buds. Burl formation is typically a result of some form of stress such as an injury or a viral or fungal infection. Burls yield a very peculiar and highly figured wood sought after in woodworking, and some items may reach high prices on the wood market. Poaching of burl specimens and damaging the trees in the process poses a problem in some areas. Description A burl results from a tree undergoing some form of stress. It may be caused by an injury, virus or fungus. Most burls grow beneath the ground, attached to the roots as a type of malignancy that is generally not discovered until the tree dies or falls over. Such burls sometimes appear as groups of bulbous protrusions connected by a system of rope-like roots. Almost all burl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Black Creek (Logar Valley)
Black Creek may refer to: Communities In Canada * Black Creek, British Columbia, on Vancouver Island * A neighborhood in Fort Erie, Ontario * Black Creek, Toronto * Black Creek Pioneer Village, a historic site in Toronto In the United States * Black Creek, New York, a hamlet in Allegany County * Black Creek, North Carolina, a town in Wilson County * Black Creek Township, Mercer County, Ohio * Black Creek Township, Luzerne County, Pennsylvania * Black Creek, Wisconsin, a village in Outagamie County * Black Creek (town), Wisconsin, a town in Outagamie County Streams In Canada * Black Creek (Ontario), one of 37 creeks of that name in Ontario, including: **Black Creek (Toronto), a tributary of the Humber River In the United States * Black Creek (Arizona), a tributary of the Puerco River, northeast Arizona * Black Creek (Florida), a tributary of the St. Johns River in Clay County * Black Creek (Ogeechee River tributary), a stream in Georgia * Black Creek (Savannah River tributary), a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anticyclone
An anticyclone is a weather phenomenon defined as a large-scale circulation of winds around a central region of high atmospheric pressure, clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere as viewed from above (opposite to a cyclone). Effects of surface-based anticyclones include clearing skies as well as cooler, drier air. Fog can also form overnight within a region of higher pressure. Mid-tropospheric systems, such as the subtropical ridge, deflect tropical cyclones around their periphery and cause a temperature inversion inhibiting free convection near their center, building up surface-based haze under their base. Anticyclones aloft can form within warm-core lows such as tropical cyclones, due to descending cool air from the backside of upper troughs such as polar highs, or from large-scale sinking such as a subtropical ridge. The evolution of an anticyclone depends upon variables such as its size, intensity, and extent of moist con ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inversion (meteorology)
In meteorology, an inversion is a deviation from the normal change of an atmosphere, atmospheric property with altitude. It almost always refers to an inversion of the air temperature lapse rate, in which case it is called a temperature inversion. Normally, air temperature decreases with an increase in altitude, but during an inversion warmer air is held above cooler air. An inversion traps air pollution, such as smog, close to the ground. An inversion can also suppress Atmospheric convection, convection by acting as a "cap". If this cap is broken for any of several reasons, convection of any moisture present can then erupt into violent thunderstorms. Temperature inversion can notoriously result in freezing rain in cold climates. Normal atmospheric conditions Usually, within the lower atmosphere (the troposphere) the air near the surface of the Earth is warmer than the air above it, largely because the atmosphere is heated from below as solar radiation warms the Earth's su ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rinka Falls
Rinka Falls (; sl, slap Rinka) is a waterfall in the Logar Valley, in the Municipality of Solčava in northern Slovenia. It is the source of the Savinja River. It has been proclaimed a natural heritage feature. Rinka Falls is one of the most beautiful and best-known waterfalls in Slovenia. It is also a popular tourist destination. With its drop of , it is the highest of the 20 waterfalls in the Logar Valley. The longest step has a length of . It is visited in all seasons of the year. In the winter it is popular with ice-climbers. The best view of the waterfall is from Kamnik Saddle (). There are also four mountains in the vicinity called Rinka: Carniola Mount Rinka (''Kranjska Rinka''; ), Carinthia Mount Rinka (''Koroška Rinka''; ), Styria Mount Rinka (''Štajerska Rinka''; ), and Little Mount Rinka (''Mala Rinka''; ). The name ''Rinka'' comes from the Slovene common noun ''rinka'' 'ring, hoop, link of a chain'. It is a borrowing from German (cf. ''Ringel'', ''Ringl'', etc.) an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Savinja
The Savinja () is a river in northeast Slovenia which flows mostly in the Upper and Lower Savinja Valley ( sl, Zgornja in Spodnja Savinjska dolina) and through the cities of Celje and Laško. The Savinja is the main river of the Savinja Alps (Sln. ''Savinjske Alpe''). It flows into the Sava River at the town of Zidani Most. It has often flooded, such as in the 1960s, 1990, and 1995. The Savinja has a length of and a catchment area of . Sources The stream is created by Rinka Falls, which flows along a regulated riverbed to the lower end of the Logar Valley, where it flows into Jezera Creek, from which point it becomes the Savinja River. This spring has been proclaimed a natural heritage object, and Rinka Falls is one of the most beautiful and best-known waterfalls in Slovenia. It is the highest waterfall of the 20 waterfalls in the Logar Valley and is visited throughout the year. In the winter it is popular for ice-climbers. The best view of the waterfall is from Kamnik Saddl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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