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Kučaj
Kučaj ( sr, Кучај, ) is a mountain range in eastern Serbia. Its highest peak, ''Velika Tresta'' has an elevation of 1,284 meters above sea level. They belong to the Serbian extension of Carpathians, which separate the valleys of Great Morava and Timok. Geography The area is a plateau in form, of complex tectonic and morphological structure, subdivided by the river valleys. One of the main features is the Resava Cave. North of Resava Cave is the natural monument Lisine, which comprises two waterfalls, Veliko Vrelo and Veliki Buk. The Lisine hydro-complex and Resava Cave are under one administration. In 2017 the Government of Serbia and Institute for Nature Protection began preliminary actions into creating a new national park, which would cover the mountainous Kučaj-Beljanica region. It is supposed to be the sixth and the largest national park in Serbia encompassing the Resava Cave, Lisine complex and some of the oldest, intact forest in the country, like the Vinatova ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Parks Of Serbia
Protected areas cover around 5% of the territory of Serbia. The ''Law on the Protection of the Nature'' defines these categories of protected areas: * Strict nature reserve — Area of unmodified natural features with representative ecosystems set aside for the preservation of its biodiversity and for scientific research and monitoring. * Special nature reserve — Area of unmodified or slightly modified natural features of great importance due to uniqueness and rarity which includes the habitats of endangered species set aside for the preservation of its unique features, education, limited tourism and for scientific research and monitoring. * National park — Area with large number of diverse ecosystems of national value, with outstanding natural features and/or cultural heritage set aside for the preservation of its natural resources and for educational, scientific and tourist use. * Natural monument — Small unmodified or slightly modified natural feature, object or phenomeno ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Serbian Carpathians
Serbian Carpathians ( sr, / ) is a mountain range in eastern Central Serbia, located in Central Europe. It presents an extension of proper Carpathian Mountains across the Danube, connecting them with the Balkan Mountains in the southeast. They stretch in north-south direction in eastern Serbia, east of the Great Morava valley and west of the White Timok Valley and north of the Nišava Valley. The mountains are 800–1500 m high, and dominated by karst limestone geologic features, the highest one being Rtanj Mountain (1,565 m). Definitions Under the strict definition (as defined by the Serbian Academy of Sciences and Arts and adopted by the Carpathian Convention), Serbian part of the Carpathian Mountains covers only 732 km², or less than 1% of the total Carpathian area. That part encompasses the southern bank of the Iron Gate and the area of Đerdap National Park. The extreme points of so defined Carpathian area in Serbia are Tekija in the north, in the south, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Serbia
Serbia is mountainous, with complex geology and parts of several mountain ranges: Dinaric Alps in the southwest, the northwestern corner of the Rila-Rhodope Mountains in the southeast of the country, Carpathian Mountains in the northeast, and Balkan Mountains and the easternmost section of Srednogorie mountain chain system in the east, separated by a group of dome mountains along the Morava river valley. The northern province of Vojvodina lies in the Pannonian plain, with several Pannonian island mountains. Mountains of Kosovo are listed in a separate article. List This is the list of mountains and their highest peaks in Serbia, excluding Kosovo. When a mountain has several major peaks, they are listed separately.http://solair.eunet.rs/~s.ilic/planine.txt (Adopted with author's permission.) Peaks over 2,000 meters The following lists only those mountain peaks which reach over 2,000 meters in height.Statistical Yearbook of Serbia 2007; chapter 1. titled ''Geog ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vinatovača
Vinatovača ( sr-cyr, Винатовача) is an old beech forest in the central-east Serbia. It is the only rainforest in Serbia, left undisturbed for several centuries. It is located in the municipality of Despotovac and is placed under the state protection as the ''strict natural reserve'', which covers an area of . Vinatovača is situated in the central Kučaj mountains in the Upper Resava region, at an altitude between and . It is isolated and hard to reach which helped its preservation. It is believed that trees have not been cut in Vinatovača since c. 1650. Being under strict protection means not only that the trees that die of old age are not being cleared or removed, but even picking herbs or mushrooms is forbidden. It is considered as an example of what central and eastern Serbia's natural look is. Beech trees are up to tall and some specimens are estimated to be over 350 years old. The forest was one of the research locations in the "SERBHIWE" project of the Univers ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Serbia
Serbia is mountainous, with complex geology and parts of several mountain ranges: Dinaric Alps in the southwest, the northwestern corner of the Rila-Rhodope Mountains in the southeast of the country, Carpathian Mountains in the northeast, and Balkan Mountains and the easternmost section of Srednogorie mountain chain system in the east, separated by a group of dome mountains along the Morava river valley. The northern province of Vojvodina lies in the Pannonian plain, with several Pannonian island mountains. Mountains of Kosovo are listed in a separate article. List This is the list of mountains and their highest peaks in Serbia, excluding Kosovo. When a mountain has several major peaks, they are listed separately.http://solair.eunet.rs/~s.ilic/planine.txt (Adopted with author's permission.) Peaks over 2,000 meters The following lists only those mountain peaks which reach over 2,000 meters in height.Statistical Yearbook of Serbia 2007; chapter 1. titled ''Geog ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Resava River
The Resava ( sr-Cyrl, Ресава) is a river in central Serbia, a 65 km-long right tributary to the Velika Morava. It also gives the name to the surrounding Resava region, the Resava Monastery, the coal mines in its valley and a popular tourist destination of Resava Cave. River The Resava originates from the Homolje region in eastern Serbia. It springs out at an altitude of 1,100 m and flows westward between the mountains of Beljanica (on the north) and Kučaj (on the south). In its upper course, the Resava runs parallel to its left tributary, the ''Kločanica'', and area around the villages of Strmosten, Vodna and Stenjevac is known for many caves ('' Resava Cave'', ''Sokolica'', ''Crystal'', etc.). The Resava carved a 25 km-long and 400 m-deep gorge, with a central part of it representing a typical canyon valley, the ''Sklop''. In the gorge, the river becomes a sinking river for a while and creates a 25 m-high waterfall, until recently, the highest one in cen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Resava (river)
The Resava ( sr-Cyrl, Ресава) is a river in central Serbia, a 65 km-long right tributary to the Velika Morava. It also gives the name to the surrounding Resava region, the Resava Monastery, the coal mines in its valley and a popular tourist destination of Resava Cave. River The Resava originates from the Homolje region in eastern Serbia. It springs out at an altitude of 1,100 m and flows westward between the mountains of Beljanica (on the north) and Kučaj (on the south). In its upper course, the Resava runs parallel to its left tributary, the ''Kločanica'', and area around the villages of Strmosten, Vodna and Stenjevac is known for many caves ('' Resava Cave'', ''Sokolica'', ''Crystal'', etc.). The Resava carved a 25 km-long and 400 m-deep gorge, with a central part of it representing a typical canyon valley, the ''Sklop''. In the gorge, the river becomes a sinking river for a while and creates a 25 m-high waterfall, until recently, the highest one in cent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Resava Cave
Resava Cave ( sr, Ресавска пећина, Resavska pećina) or Resavska Cave is a cave near Jelovac in eastern Serbia, about from Despotovac. It is one of the largest cave systems in Serbia, with the corridors about long. Geography The cave is located in the Upper Resava region. The cave is estimated to be 80 million years old while the oldest speleothems date from 45 million years ago. It has four halls on two levels each and the speleothems are colored in red, yellow and white. Altitude at the entrance into the cave is and the lowest point inside is at . The cave was formed by the sinking river in the limestone substrate. Cave formations are right at the entry. They are formed through the dissolving of the calcium carbonate. The color depends on the mineral through which the water flows: red from the iron oxide, white from the crystallized calcium and yellow from the traces of clay. The symbol of the cave is a massive stalagmite, tall and wide. After its appe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Temperate Rainforest
Temperate rainforests are coniferous or broadleaf forests that occur in the temperate zone and receive heavy rain. Temperate rain forests occur in oceanic moist regions around the world: the Pacific temperate rain forests of North American Pacific Northwest as well as the Appalachian temperate rainforest of the Eastern U.S. Sun Belt; the Valdivian temperate rain forests of southwestern South America; the rain forests of New Zealand and southeastern Australia; northwest Europe (small pockets in Great Britain and larger areas in Ireland, southern Norway and northern Iberia); southern Japan; the Black Sea–Caspian Sea region from the southeasternmost coastal zone of the Bulgarian coast, through Turkey, to Georgia, and northern Iran. The moist conditions of temperate rain forests generally support an understory of mosses, ferns and some shrubs and berries. Temperate rain forests can be temperate coniferous forests or temperate broadleaf and mixed forests. Definition For temperat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mlava
The Mlava (Serbian Cyrillic: Млава) is a river in Serbia, 158 km long right tributary of the Danube. Origin Mlava originates as the ''Tisnica'', from the Kučaj mountains in eastern Serbia, under the ''Veliki Krš'' peak. It flows to the north and curves around the eastern slopes of the mountain Beljanica, through an almost uninhabited area. Reaching the Homolje region, the Tisnica receives from the right a very powerful outflow of the karst well of Žagubičko vrelo (Žagubica well), at an altitude of 320 meters, and from that point the river is known as the Mlava. Measured from the Žagubičko vrelo, the river is 118 km long. Upper course (Homolje region) Originally, the Mlava flows to the northwest, but soon turns to the north, which is the general direction it follows for the rest of its course. It flows next to the Žagubica, the main center of Homolje valley, and the villages of Izvarica (where it receives from the right the ''Jošanička reka''), Ribar ... [...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] |
Karst Spring
A karst spring or karstic spring is a spring (outflow of groundwater) that is part of a karst hydrological system. Description Because of their often conical or inverted bowl shape, karst springs are also known in German-speaking lands as a ''Topf'' ("pot") which is reflected in names such as Aachtopf (the source of the Radolfzeller Aach) or Blautopf (the source of the Blau river in Blaubeuren). Karst springs often have a very high yield or discharge rate, because they are often fed by underground drainage from a large catchment basin. Because the springs are usually the terminus of a cave drainage system at the place where a river cave reaches the Earth's surface, it is often possible to enter the caves from karst springs for exploration. Large karst springs are located in many parts of the world; the largest ones are believed to be in Papua New Guinea, with others located in Mediterranean countries such as Bosnia and Herzegovina, Croatia, Turkey, Slovenia, and Italy. Types ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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