13. Maj
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13. Maj
Batajnica ( sr-Cyrl, Батајница, ) is an urban neighborhood of Belgrade, the capital city of Serbia. It is located in the Belgrade municipality of Zemun. Location and geography Batajnica is located in the Syrmia region, in the northern part of the municipality, close to the administrative border of the province of Vojvodina and it is both the northernmost and the westernmost part of the Belgrade's urban area. It is close to the Danube's right bank, but not on the river itself, due to the floodings. A small, 114 metre-high hillock separates the settlement from the river. It is some 15 kilometres away from downtown Belgrade, but only 6 kilometres away from Nova Pazova and Novi Banovci, fast growing settlements in the Vojvodina's municipality of Stara Pazova, to which it almost makes a continuous built-up area. : it extends to the southwest in the direction of Ugrinovci's neighborhood of Busije and southeast in the direction of other Zemun's neighborhoods: Zemun Polj ...
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List Of Belgrade Neighbourhoods And Suburbs
Belgrade, the capital city of Serbia, is divided into seventeen municipalities, of which ten are urban and seven suburban. In this list, each neighbourhood or suburb is categorised by the municipality in which it is situated. Six of these ten urban municipalities are completely within the bounds of Belgrade City Proper, while the remaining four have both urban and suburban parts. The seven suburban municipalities, on the other hand, are completely located within suburban bounds. Municipalities of the City of Belgrade are officially divided into local communities ( Serbian: месна заједница / ''mesna zajednica''). These are arbitrary administrative units which on occasion correspond to the neighbourhoods and suburbs located in a municipality, though usually they don't. Their boundaries often change as the communities merge with each other, split from one another, or change names, so the historical and traditional names of the neighbourhoods survive. In the majority ...
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Nova Pazova
A nova (plural novae or novas) is a transient astronomical event that causes the sudden appearance of a bright, apparently "new" star (hence the name "nova", which is Latin for "new") that slowly fades over weeks or months. Causes of the dramatic appearance of a nova vary, depending on the circumstances of the two progenitor stars. All observed novae involve white dwarfs in close binary systems. The main sub-classes of novae are classical novae, recurrent novae (RNe), and dwarf novae. They are all considered to be cataclysmic variable stars. Classical nova eruptions are the most common type. They are likely created in a close binary star system consisting of a white dwarf and either a main sequence, subgiant, or red giant star. When the orbital period falls in the range of several days to one day, the white dwarf is close enough to its companion star to start drawing accreted matter onto the surface of the white dwarf, which creates a dense but shallow atmosphere. This atmosp ...
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Europe
Europe is a large peninsula conventionally considered a continent in its own right because of its great physical size and the weight of its history and traditions. Europe is also considered a Continent#Subcontinents, subcontinent of Eurasia and it is located entirely in the Northern Hemisphere and mostly in the Eastern Hemisphere. Comprising the westernmost peninsulas of Eurasia, it shares the continental landmass of Afro-Eurasia with both Africa and Asia. It is bordered by the Arctic Ocean to the north, the Atlantic Ocean to the west, the Mediterranean Sea to the south and Asia to the east. Europe is commonly considered to be Boundaries between the continents of Earth#Asia and Europe, separated from Asia by the drainage divide, watershed of the Ural Mountains, the Ural (river), Ural River, the Caspian Sea, the Greater Caucasus, the Black Sea and the waterways of the Turkish Straits. "Europe" (pp. 68–69); "Asia" (pp. 90–91): "A commonly accepted division between Asia and E ...
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Paleoclimatic
Paleoclimatology (British spelling, palaeoclimatology) is the study of climates for which direct measurements were not taken. As instrumental records only span a tiny part of Earth's history, the reconstruction of ancient climate is important to understand natural variation and the evolution of the current climate. Paleoclimatology uses a variety of proxy methods from Earth and life sciences to obtain data previously preserved within rocks, sediments, boreholes, ice sheets, tree rings, corals, shells, and microfossils. Combined with techniques to date the proxies, the paleoclimate records are used to determine the past states of Earth's atmosphere. The scientific field of paleoclimatology came to maturity in the 20th century. Notable periods studied by paleoclimatologists are the frequent glaciations that Earth has undergone, rapid cooling events like the Younger Dryas, and the rapid warming during the Paleocene–Eocene Thermal Maximum. Studies of past changes in the environm ...
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Interglacial
An interglacial period (or alternatively interglacial, interglaciation) is a geological interval of warmer global average temperature lasting thousands of years that separates consecutive glacial periods within an ice age. The current Holocene interglacial began at the end of the Pleistocene, about 11,700 years ago. Pleistocene During the 2.5 million years of the Pleistocene, numerous glacials, or significant advances of continental ice sheets, in North America and Europe, occurred at intervals of approximately 40,000 to 100,000 years. The long glacial periods were separated by more temperate and shorter interglacials. During interglacials, such as the present one, the climate warms and the tundra recedes polewards following the ice sheets. Forests return to areas that once supported tundra vegetation. Interglacials are identified on land or in shallow epicontinental seas by their paleontology. Floral and faunal remains of species pointing to temperate climate and indicating a s ...
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Glacial
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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List Of Natural Monuments In Belgrade
List of the protected natural heritage on the administrative territory of Belgrade, the capital of Serbia. Protected areas Landscapes of outstanding features Natural monuments Protected habitats Internationally important areas Ecologically important areas The surroundings of some protected area are declared ecologically important areas, a wider, super-areas which may comprise more, territorially disconnected, singular protected areas. Together, they all form the proclaimed ecological network An ecological network is a representation of the biotic interactions in an ecosystem, in which species (nodes) are connected by pairwise interactions (links). These interactions can be trophic or symbiotic. Ecological networks are used to describ ... of Serbia, and are based on some internationally declared important areas. Internationally important ecological corridors Future and former protected areas Planned and proposed protected areas Areas which have be ...
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Loess
Loess (, ; from german: Löss ) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits. Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay and a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs. Properties Loess is homogeneous, porous, friable, pale yellow or buff, slightly coherent, typically non- stratified and often calcareous. Loess grains are angular, with little polishing or rounding, and composed of crystals of quartz, feldspar, mica and other minerals. Loess can be described as a rich, dust-like soil. Loess deposits may become very thick, more than ...
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Goveđi Brod
Goveđi Brod (Serbian Cyrillic: Говеђи брод) is an urban neighborhood of Belgrade, the capital of Serbia. It is located in Belgrade's municipality of Zemun. Location Goveđi Brod is the northwestern extension of urban Zemun proper, located on the right bank of the Danube. It occupies roughly the area between the Danube and the road which connects Zemun and the outer suburb of Batajnica (''Batajnički drum''). The only other urban neighborhood that it borders is Galenika, but it extends in the direction of Zemun Polje (northwest) and Gornji Grad (south, through Galenika). Characteristics Goveđi Brod is almost entirely a non-residential area. Some major facilities in the neighborhood are the Mining Institute and the Veterinarian Institute. The neighborhood also includes a large area of storehouses, and two gravel and concrete processing plants, "DIA" and "Anicom", both on the Danube's bank. Romani However, the publicly best known characteristic of Goveđi Brod ...
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Galenika, Zemun
Galenika ( sr-cyr, Галеника) or Nova Galenika ( sr-cyr, Нова Галеника) is an urban neighborhood of Belgrade, the capital of Serbia. It is located in Belgrade's municipality of Zemun. Location Nova Galenika is located on the north-western outskirts of Zemun. Elongated mixed residential-commercial-industrial neighborhood, mostly bounded by the roads of ''Batajnički drum'' (Батајнички друм) and ''Novosadski put'' (Новосадски пут), borders the neighborhoods of Goveđi Brod on the north, Gornji Grad on the east, Zemun Bačka on the south-east, Altina on the south, while in the west, the industrial zone extends into the directions of Zemun Polje, Kamendin and Batajnica. Characteristics The neighborhood consists of several parts, including old Galenika section. The ''Nova'' (New) Galenika section and the surrounding industrial and commercial areas. The neighborhood of Galenika originated from the 1960s as a separate neighborhood, ou ...
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Zemun Polje
Zemun Polje ( sr, Земун поље) is an urban neighborhood of Belgrade, the capital of Serbia. It is located in the municipality of Zemun. Location Zemun Polje is located on both railway and highway Belgrade-Novi Sad, halfway between the western section of urban Zemun (Nova Galenika) and Batajnica. For decades completely outside the urban section of Belgrade, since the late 1990s it made urban connection with the extended industrial zone of Nova Galenika on the east (through the neighborhood of Kamendin and the fast developing neighborhood of Plavi Horizonti on the south. Characteristics Despite even originally being built outside the urban zone of Belgrade (in the 1970s, even the name, Zemun Polje, means Zemun field) it was intended as a neighborhood of Belgrade, not as a separate settlement. The neighborhood of Kamendin was built in the late 1990s, directly adjoining the western section of Zemun Polje. The geometrically shaped neighborhood is mostly residential, with ...
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Busije
Busije ( Serbian Cyrillic: Бусије) is a suburban neighborhood of Belgrade, the capital of Serbia. It is located in Belgrade's municipality of Zemun. Location Busije is a sub-neighborhood of Ugrinovci, the only separate settlement in the municipality (urban section of Zemun is administratively part of the Belgrade proper). It is located halfway between Ugrinovci and Batajnica, westernmost section of the Belgrade proper. History Just like the other similar settlement, Grmovac, origins of Busije (Serbian for 'ambush') date from 1997 when the Zemun's municipal leadership decided to sell empty lots to the refugees from Croatia who were forced out after the Operation Storm in 1995. Prices were relatively low and many people bought the land, regardless of the fact that area has not been designated for urban development and the lack of any infrastructure. Area and population Originally. Busije covered an area of 42 hectares, divided into 1.300 lots for individual houses ...
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