- Geography of Serbia
Serbiais country located in the Balkans(a historical and geographical region of southeastern Europe) and in the Pannonian Plain(a region of central Europe). It shares borders with Bosnia-Herzegovina, Bulgaria, Croatia, Hungary, the Republic of Macedonia, Montenegro, and Romania. Serbia claims a border with Albaniaas well through its disputed territory of Kosovo, although it has no "de facto" control over this border. It is landlocked, although access to the Adriaticis available through Montenegro, and the Danube Riverprovides shipping access to inland Europe and the Black Sea.
Serbia covers a total of 88,361
km², which places it at 113th place in the world. Its total border length amounts to 2,027 km (Albania 115 km, Bosnia and Herzegovina 302 km, Bulgaria 318 km, Croatia 241 km, Hungary 151 km, Macedonia 221 km, Montenegro 203 km and Romania 476 km) [https://www.cia.gov/library/publications/the-world-factbook/geos/sr.html CIA World Factbook:Serbia] ] . All of Serbia's border with Albania, and parts of the borders with Macedonia, Montenegro, are under control of the disputed province of Kosovo, with which Serbia has 352km of border (although note that Kosovo does not control 100% of its claimed territory, either). It has 6,167 registered settlements, 207 urban and 5960 others (rural). [sr icon [http://webrzs.statserb.sr.gov.yu/axd/teritorija.htm Republički zavod za statistiku Srbije] , Administrativna i teritorijalna podela Republike Srbije] Arable landcovers 19,194 km² [ [http://webrzs.statserb.sr.gov.yu/axd/godisnjak/god2005pog13.pdf, Republic Statistical Office of Serbia, Annual book] , Chapter 13-Agriculture] , and woods cover 19,499 km² [sr icon [http://webrzs.statserb.sr.gov.yu/axd/teritorija.htm Republički zavod za statistiku Srbije] , Prikaz stanja šuma po površini] of the territory of Serbia without Kosovo.
* North: 46°11'N (near
* South: 41°52' N (near
* East: 23°01'E (Senokos near
* West: 18°51'E (near
Serbia's terrain ranges from rich, fertile plains of the northern
Vojvodinaregion, limestone ranges and basins in the east, and in the southeast ancient mountains and hills. The north is dominated by the Danube River. A tributary, the Morava River flows through the more mountainous southern regions.
Central Serbia, the terrain consists chiefly of hills, low and medium-high mountains, interspersed with numerous rivers and creeks. The main communication and development line stretches southeast of Belgrade, towards Nišand Skopje(in Republic of Macedonia), along the valley of Great and South Morava river. Most major cities are located on or around that line, as well as the main railroad and highway. On the East of it, the terrain quickly rises to limestone ranges of Stara Planinaand Homolje, relatively sparsely populated. On the West, height of mountains slowly rises towards southwest, but they do not form real ridges. The highest mountains of that area are Zlatiborand Kopaonik.
Mountains cover the largest parts of Central Serbia and Kosovo. Four mountain systems meet in Serbia:
Dinaric Alpsin the west cover the greatest territory, and stretch from northwest to southeast. Carpathian Mountainsand Balkan Mountainsstretch in north-south direction in the eastern Serbia, west of the Morava valley. Ancient mountains along the South Moravabelong to Rilo-Rhodope Mountain system.
The most significant mountains in Serbia are:
The highest peak in Serbia is
Midžoron Stara Planina(2,169 m), while Vršački breg (641 m) tops Vojvodina.
Practically the entire territory (92%) of Serbia belongs to the
Danube( Black Sea) drainage basin, an area in Kosovo (5%) belongs to the Adriaticdrainage basin, chiefly through the White Drinriver, and the rest (3%) in Kosovo and southern Serbia belongs to Aegean basin, chiefly via the Vardarriver.
Apart from the Danube, which flows 588 km through Serbia or as a border river (with
Croatiaon its northwestern flow and Romaniaon southeast), the chief rivers are its tributaries Sava(incoming from West), Tisa(incoming from North), Drina(incoming from South, forming a natural borderwith Bosnia and Herzegovina) and Morava; only the latter flowing (almost) entirely through Serbia. Their tributaries form a dense network of smaller rivers and creeks, covering most of the Central Serbia and Kosovo.
Due to the configuraton of the terrain, natural
lakes are sparse and small; most of them are located in Vojvodina, like the glacial lakePalić or numerous oxbow lakes along river flows. However, there are numerous artificial lakes, mostly due to hydroelectric dams, the biggest being Đerdapon the Danube, Perućacon the Drina and Vlasina Lake.
Abundance of relatively unpolluted surface waters and numerous underground natural and mineral water sources of high
water qualitypresents a chance for export and economy improvement; however, more extensive exploitation and production of bottled water has began only recently. Despite this, many Serbian cities still suffer from water supply problems, due to mismanagement and low investments in the past, as well as water pollution (like the pollution of the Ibar Riverfrom the Trepča zinc- leadcombinate, affecting the city of Kraljevo, or the presence of natural arsenicin underground waters in Zrenjanin).
The hydroenergetic potential of Serbia is around 17,000
GWh, of which around 10,000 GWh (60%) is utilized in power plants, chiefly big ones. The remaining unused potential can be realized using small and medium power plants (<25 MW), whose building by the private sector is seen as a chance for improvement of Serbia's economy and energy reliability. [ [http://www.eps.co.yu/razvoj/e_potencijali.htm Energetski potencijali Srbije, Elektroprivreda Srbije] sr icon]
Serbia also has a huge geothermal potential, which is only partially and sporadically utilized. The use of geothermal waters is chiefly for
balneologicalpurposes: there are around 60 spas, which are seen as a great chance for improvement of the tourismsector. [ [http://www.os.is/Apps/WebObjects/Orkustofnun.woa/swdocument/1898/19+Milivojevic+IGC+2003.pdf Utilization of Geothermal Hydrology in Serbia"] , M. Milivojević and M. Martinović, International Geothermal Conference, Reykjavik 2003.]
Climate of Serbia is moderate continental with a diversity on local level, caused by geographic location, relief, terrain exposition, presence of river and lake systems, vegetation, urbanization etc. Proximity of the mountain ranges of
Alps, Carpathians, Rhodopes, as well as Adriatic Seaand Pannonian plainaffect the climate. Location of river ravines and plains in the northern area of the country enable occasional deep southward protrusion of polar air masses on winters, while hot Saharan air often intrudes over the Mediterranean Seaon summers.
Average annual air temperature for the period 1961-1990 for the area with the altitude of up to 300 m amounts to 10.9
°C. The areas with the altitudes of 300 to 500 m have average annual temperature of around 10.0 °C, and over 1000 m of altitude around 6.0 °C.
Annual precipitation, generally, rises with
altitude. In lower regions, it ranges in the interval from 540 to 820 mm, areas on altitude over 1000 m receive in average 700 to 1000 mm, and some mountainous summits in southwestern Serbia up to 1500 mm. Major part of Serbia has continental precipitation regimen, with peak in the summer period, except for southwest, which receives highest precipitation autumn. June is the rainiest month, with the average of 12 to 13% of total annual amount. February and October have the least precipitation. Snow cover can occurs from November to March, and majority of days with snow cover is in January.
Annual sums of
solar radiationare in the interval from 1500 to 2200 hours annually.
Surface air circulation is largely influenced by
orographic lift. In warmer part of the year, winds from northwest and west prevail. In Vojvodina and Northern Serbia, east-southeast wind, Košava, dominates over autumn and winter. Southwestern winds prevail in mountainous part of southwestern Serbia. [http://www.hidmet.sr.gov.yu/eng/meteorologija/klimatologija_srbije.php Hydrometeorologic Service of Serbia] ]
Serbia has four
national parks and many national nature reserves.
Fruška Gora(250 km²)
* Tara (220 km²)
Đerdap(Iron Gate) (640 km²)
Gornje Podunavlje(100 km²)
* Stara Planina (1420 km²)
Kučajske planine(1150 km²)
Special nature reservations:
Deliblato Sands(300 km²)
Ludaš Lake(5.93 km²)
Obedska Pond(175.01 km²)
Stari Begej – Carska Bara(17.67 km²)
Đavolja Varoš(0.64 km²)
Geography of Europe
Geography of Vojvodina
Regions of Serbia
* [http://www.jcerni.co.yu/english/vos.htm Institute for the development of water resources "Jaroslav Černi"]
* [http://icpdr01.danubeday.org/icpdr-files/12877 Danube Facts and Figures: Serbia]
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