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Troglav (Bosnia And Herzegovina)
Troglav ( sr-Cyrl, Троглав) is the highest peak of the Dinara Mountain Range in the Dinaric Alps (also known as ''Dinarides''). Dinara is the longest massif within karstic mountain chain of the western Balkan peninsula. Troglav is located in the territory of Bosnia and Herzegovina. It is named after Triglav, Slavic god. The name literally means "three headed". The Troglav group is around 30 km long and around 15 km wide, making it the largest in the range. On the northwestern side, it is separated from the Dinara group by the Privija pass (1230 m) and on the southeast from the Kamešnica group by Vaganj (1173 m) road pass, which connects Sinj in Croatia with Livno in Bosnia. On the northeastern, Bosnian side, lies the huge karstic field of Livanjsko Polje (700 m), which is 65 km long. On the southwestern, Croatian side, there is the Cetina river valley with 15 km long Peruća Lake (''Perućko Jezero''), continuing on to the Sinjsko Polje. ...
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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 ...
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Sinjsko Polje
Sinjsko Polje () is a polje (karstic field) in the inner Dalmatia region of Croatia , image_flag = Flag of Croatia.svg , image_coat = Coat of arms of Croatia.svg , anthem = "Lijepa naša domovino"("Our Beautiful Homeland") , image_map = , map_caption = , capit ..., the fifth largest in Croatia, covering an area of . References {{Dinaric Alps' karst fields Plains of Croatia Geology of Croatia ...
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Mountains Of The Federation Of Bosnia And Herzegovina
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Mountains Of Bosnia And Herzegovina
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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List Of Mountains In Bosnia And Herzegovina
List of mountains in Bosnia and Herzegovina: References * {{DEFAULTSORT:List Of Mountains In Bosnia and Herzegovina Mountains in Bosnia and Herzegovina Bosnia and Herzegovina Mountains Bos ''Bos'' (from Latin '' bōs'': cow, ox, bull) is the genus of wild and domestic cattle. ''Bos'' is often divided into four subgenera: ''Bos'', ''Bibos'', ''Novibos'', and ''Poephagus'', but including these last three divisions within the gen ...
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Dinara
Dinara is a long mountain range in the Dinaric Alps, located on the border of Bosnia and Herzegovina and Croatia. It has four major mountains or peaks, from north-west to south-east: * Ilica or Ujilica (1654 m) * Sinjal or Dinara (1831 m), eponym to the range, highest mountain in Croatia * Troglav (1913 m), highest peak in the range * Kamešnica, with peak Konj (1855 m) Note the dual use of the name ''Dinara'', which is also the origin of the name for the whole Dinaric Alps.''Statistical Yearbook of the Republic of Croatia 2015'', p. 48 The range is composed of limestone and dolomite. Etymology The origin of the name is uncertain. It may deliver from a forgotten Illyrian tribe name, or it is named after a settlement in or near the region. Dinara Mountain Sinjal, often marked as ''Dinara'' on maps, is the highest mountain in Croatia and has an impressive south-western cliff, several hundred meters high, that is prominently visible from the Dalmatian plain below. It has ...
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Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ...
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Glaciation
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period ...
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Norway Spruce
''Picea abies'', the Norway spruce or European spruce, is a species of spruce native to Northern, Central and Eastern Europe. It has branchlets that typically hang downwards, and the largest cones of any spruce, 9–17 cm long. It is very closely related to the Siberian spruce (''Picea obovata''), which replaces it east of the Ural Mountains, and with which it hybridizes freely. The Norway spruce has a wide distribution for it being planted for its wood, and is the species used as the main Christmas tree in several countries around the world. It was the first gymnosperm to have its genome sequenced. The Latin specific epithet ''abies'' means “like ''Abies'', Fir tree” Description Norway spruce is a large, fast-growing evergreen coniferous tree growing tall and with a trunk diameter of 1 to 1.5 m. It can grow fast when young, up to 1 m per year for the first 25 years under good conditions, but becomes slower once over tall. The shoots are orange-brown and glabrous. The ...
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Troglav Peruca
Troglav may refer to: *Troglav (mythology), deity in Slavic mythology whose three heads were believed to represent sky, earth and the underworld * Troglav (Bosnia and Herzegovina), a mountain massif and peak in western Bosnia and Herzegovina on the border with Croatia ** NK Troglav Livno NK Troglav 1918 is a football club from Livno, Bosnia and Herzegovina. It is a member of the Second League of the Federation of Bosnia and Herzegovina – group South, third level of football in the country. The club was founded in 1921, as part o ..., a football club named after the aforementioned peak * Troglav (Serbia), a mountain in central Serbia {{geodis ...
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European Beech
''Fagus sylvatica'', the European beech or common beech is a deciduous tree belonging to the beech family Fagaceae. Description ''Fagus sylvatica'' is a large tree, capable of reaching heights of up to tall and trunk diameter, though more typically tall and up to trunk diameter. A 10-year-old sapling will stand about tall. It has a typical lifespan of 150–200 years, though sometimes up to 300 years. In cultivated forest stands trees are normally harvested at 80–120 years of age. 30 years are needed to attain full maturity (as compared to 40 for American beech). Like most trees, its form depends on the location: in forest areas, ''F. sylvatica'' grows to over , with branches being high up on the trunk. In open locations, it will become much shorter (typically ) and more massive. The leaves are alternate, simple, and entire or with a slightly crenate margin, long and 3–7 cm broad, with 6–7 veins on each side of the leaf (as opposed to 7–10 veins in ...
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Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ...
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