Ambasador Królestwa Arabii Saudyjskiej odwiedza Kraków

8 lutego 2022 roku Jego Ekscelencja Saad Saleh Alsaleh spotkał się z Prezydentem Jackiem Majchrowskim. Wizyta miała charakter kurtuazyjny i zapoznawczy. Placówkę w Warszawie Ambasador Alsaleh objął zaledwie kilka miesięcy temu – listy uwierzytelniające złożył Prezydentowi RP 21 października 2021 r. Dla Pana Ambasadora, oraz towarzyszącego mu Pierwszego Sekretarza Ambasady Mohammeda Alhedaithy, była to pierwsza wizyta w Krakowie.

2022/02/21

Wizyta Ambasadora Turcji na UAM

Ambasador Turcji Cengiz Kamil Fırat oraz honorowy konsul Turcji w RP Jerzy Kudyński, byli gośćmi JM Rektor UAM, prof. Bogumiły Kaniewskiej. W spotkaniu uczestniczyli także prorektor UAM ds. współpracy międzynarodowej, prof. Rafał Witkowski oraz dziekan Wydziału Neofilologii UAM, prof. Krzysztof Stroński. Podczas spotkania poruszono tematy współpracy pomiędzy UAM a tureckimi uniwersytetami, a także mobilności studenckiej.

2022/02/21

Independence day of the Republic of Gambia

The Gambia, country in western Africa situated on the Atlantic coast and surrounded by the neighbouring country of Senegal. It occupies a long narrow strip of land that surrounds the Gambia River. The land is flat and is dominated by the river, which is navigable throughout the length of the country. The peculiar shape and size of the country are the result of territorial compromises made during the 19th century by Great Britain, which controlled the lower Gambia River, and France, which ruled the neighbouring colony of Senegal. Periodic talks in the 20th century to unite The Gambia and Senegal led to the short-lived Senegambia confederation (1982–89). The Gambia is Africa’s smallest nonisland country. It is also one of Africa’s most densely populated countries. A few towns are located upriver, but most Gambians live in rural villages. The major ethnic groups are similar to those in Senegal and consist of the majority Malinke and also include Wolof, Fulani (Fulbe), Diola (Jola), and Soninke peoples. The Gambian economy is heavily dependent on peanut (groundnut) production and export. The country is known for the beaches along its small Atlantic coastline and for being home to Jufureh (Juffure), the reputed ancestral village of Kunta Kinte, the main character in Alex Haley’s well-known novel Roots. The capital, Banjul (called Bathurst until 1973), is situated where the Gambia River flows into the Atlantic Ocean. Land The Gambia is a strip of land 15 to 30 miles (25 to 50 km) wide on either side of the Gambia River and extends almost 300 miles (480 km) into the interior; except for a short coastline along the Atlantic Ocean, it is entirely surrounded by Senegal. Relief and drainage The Gambia River is the country’s dominant feature. It flows across a plateau of Miocene-Pliocene sandstone consisting of compacted sediment composed predominantly of quartz grains formed from about 23.7 to 1.6 million years ago. In the east, narrow valleys are separated by broad interfluves or flattish hills. In the west, lower and smaller sand hills alternate with depressions filled in with sand to form a flat plain. Soils and climate The Gambia has a wet-and-dry tropical climate characterized by an intense rainy season occurring generally between June and October and by a longer dry season. Near the coast the rainy season lasts longer, and the rainfall is heavier, diminishing eastward. At Yundum the average annual rainfall is about 50 inches (1,300 mm), and the mean monthly temperature tends to be in the upper 70s F (mid-20s C), while at Basse Santa Su, about 270 miles (435 km) inland, the comparable figures are about 40 inches (1,000 mm) and the low 80s F (upper 20s C). The relative humidity is high but drops from December to April, when the dry northeastern wind known as the harmattan is dominant. Plant and animal life The vegetation cover of The Gambia is savanna on the uplands, various kinds of inland swamp in the low-lying areas, and mangrove swamp along the brackish lower Gambia River. Few wild animals are native to the region, and those that survive are under pressure from the human and domestic animal populations. In the middle and upper river areas there are warthogs, monkeys, baboons, antelope, pygmy hippopotamuses, and crocodiles. In addition, more than 500 species of birds live throughout the country. Birds and wildlife can be found in Bijilo Forest Park, along the Atlantic coast, the Abuko Nature Reserve, just upriver from Banjul, Kiang West National Park, farther inland, and River Gambia National Park (also known as Baboon Island National Park), near Kuntaur. People - Ethnic groups The river basin was a focal point for migrating groups of people escaping the turmoil of western Sudanic wars dating from the 12th century. The Diola (Jola) are the people longest resident in the country; they are now located mostly in western Gambia. The largest group is the Malinke, comprising about one-third of the population. The Wolof, who are the dominant group in Senegal, also predominate in Banjul. The Fulani settled the extreme upriver areas, and their kingdom, Fuladu, became a major power in the late 19th century. The Soninke, an admixture of Malinke and Fulani, are also concentrated in the upriver areas. Languages English is the official language, but the most frequently spoken languages are generally of the Atlantic branch of the Niger-Congo family. Mandinka and Wolof constitute the lingua francas of the country, and other languages spoken include Pulaar (Fulbe), Serer, Diola, and Soninke. Some Muslim clerics are literate in Arabic. Religion The population is overwhelmingly Muslim. There are a small number of Christians—predominantly Roman Catholic—and some adherents of traditional beliefs. Settlement patterns Human settlement in The Gambia extends across both banks of the river and is found in three regions: the swamps adjacent to the river, the riverine flats, known as banto faros (from a Mande word meaning “beyond the swamp”), and the sandstone uplands. Most rural settlement is concentrated on the uplands, which have the best-drained soils. A number of settlements are located in the banto faros on the middle course of the river, where there is less danger of flooding than in the swamps. Many villages are built on the boundary between the uplands and the riverine flats. About three-fifths of the population lives in urban areas. The major urban concentration is around Banjul, the capital, and several large urban centres have developed in the vicinity. Urban dwellers retain close ties to their rural relatives, and there is considerable interaction between rural and urban populations. Migration to urban areas has remained steady since the 1970s. Demographic trends The population growth rate and infant mortality rate in The Gambia are among the highest in western Africa. The population is young, with about two-thirds under age 30. Life expectancy is comparable to the regional average but lower than that of the world. Over the years, conflict in other western African countries led to an influx of refugees into The Gambia, most notably those fleeing from fighting in Senegal’s Casamance region as well as those who fled from civil wars in Liberia and Sierra Leone. Economy - Agriculture, forestry, and fishing Gambian agriculture can be described as a classic monoculture; peanuts (groundnuts) are the most valuable agricultural commodity. Land is cleared by the slash-and-burn technique, but farmers practice conservation. Most land is held in common by the villagers. There is a sharp division of labour, with men involved in planting, cultivating, and harvesting cash crops while women cultivate subsistence crops such as cassava (manioc), yams, eggplant, tomatoes, rice, and lentils. There are citrus orchards in the western area near Banjul. The production of peanuts has increased with the wider use of fertilizers and ox-drawn equipment and the introduction of better seeds. In order to diversify the economy, the government has encouraged the production of rice. A pilot scheme was begun in the mid-1960s to introduce plantation oil palm production, but this has had little impact on the national economy. Stock farming, always a factor in the Fulani culture, has also received government support, but factors such as insufficient animal husbandry techniques and the scarcity of suitable pasture and water have limited the size of herds. The drought years of the 1970s and ’80s seriously damaged agricultural production, particularly upriver. The country was not as hard hit as other countries in the region, however, and recovery has been steady. Although the country’s small ocean coastline limits marine fishing, there is some potential for commercial fishing offshore and in the river. Most Gambians are not fishermen, but those who are have been handicapped by inadequate equipment. The government has offered small loans for the purchase of motorized fishing boats and the construction of smoke huts for the processing of bonga (shad, or West African herring), which is exported to other western African states. Resources and power The Gambia has very few exploited mineral deposits. Some amounts of clay, sand, and gravel are excavated for local use. Foreign investors have been granted licenses to explore offshore blocks for potential petroleum and natural gas reserves, but these actions have not yet yielded any production. The Gambia River holds hydroelectric potential, but there are no dams on the river within the country’s borders. Oil is imported to meet the country’s energy needs. Electricity is limited to parts of Banjul and a few interior towns but is sporadic at best; most Gambians do not have access to modern infrastructure. Manufacturing The most significant industry in the country is peanut processing. The crop is sold to agents of The Gambia Groundnut Corporation (until 1993 known as the Gambia Produce Marketing Board), which fixes the season’s price in advance, pays the producers in cash, and sells the crop overseas. The agents arrange for transportation of the peanuts to Banjul or Kuntaur, where the nuts are shelled before being shipped. After shelling, a large part of the crop is pressed into oil at pressing mills. The residue is used as cattle cake. The construction industry has grown in correlation with the growth of the tourism sector. Smaller industries include the manufacture of food products, beverages, textiles, footwear, and wood products. Handicraft and other small-scale local craft production exists in villages throughout the country. More … Source: https://www.britannica.com/place/The-Gambia  

2022/02/18

The Day of the Restoration of the State of the Republic of Lithuania

Lithuania, country of northeastern Europe, the southernmost and largest of the three Baltic states. Lithuania was a powerful empire that dominated much of eastern Europe in the 14th–16th centuries before becoming part of the Polish-Lithuanian confederation for the next two centuries. Aside from a brief period of independence from 1918 to 1940, Lithuania was occupied by Russia beginning in 1795, was controlled by Germany for a brief period during World War II, and was incorporated into the U.S.S.R. in 1944 as one of its constituent republics. On March 11, 1990, Lithuania declared its independence by a unanimous vote of its newly elected parliament. The new Soviet parliament acknowledged Lithuania’s independence on September 6, 1991. Lithuania was admitted into the European Union (EU) and the North Atlantic Treaty Organization in 2004. The capital is Vilnius. Land Lithuania is bounded by Latvia to the north, Belarus to the east and south, Poland and the detached Russian oblast of Kaliningrad to the southwest, and the Baltic Sea to the west. Relief Underlying rock structures are of little significance for the contemporary Lithuanian terrain, which basically is a low-lying plain scraped by Ice Age glaciers that left behind thick, ridgelike terminal deposits known as moraines. The Baltic coastal area is fringed by a region characterized by geographers as the maritime depression, which rises gradually eastward. Sand dunes line an attractive coast; the Curonian Lagoon (Lithuanian: Kuršiu Marios), almost cut off from the sea by the Curonian Spit, a thin 60-mile (100-km) sandspit, forms a distinctive feature. It is bounded by the Žemaičiai Upland to the east, which gives way to the flat expanses of the Middle Lithuanian Lowland. The lowland, consisting of glacial lake clays and boulder-studded loams, stretches in a wide band across the country from north to south; some portions of it are heavily waterlogged. The elevated Baltic Highlands, adjacent to the central lowland, thrust into the eastern and southeastern portions of the country; their rumpled glacial relief includes a host of small hills and numerous small lakes. The Švenčioniai and the Ašmena highlands—the latter containing Mount Juozapinė, at 957 feet (292 metres) above sea level the highest point in Lithuania—are located in the extreme east and southeast. Drainage Lithuanian rivers drain to the Baltic and generally have the slow, meandering characteristics of lowland rivers. The Neman River (Nemunas), cutting north and then west through the heart of the country, is the largest. Its main tributaries are the Merkys, Neris, Nevėžis, Dubysa, Jūra, Minija, and Šešupė. A distinctive feature of the Lithuanian landscape is the presence of about 3,000 lakes, mostly in the east and southeast. The boggy regions produce large quantities of peat that, dried by air, is used in both industry and agriculture. Soils Lithuanian soils range from sands to heavy clays. In the northwest the soil is either loamy or sandy (and sometimes marshy) and is quite heavily podzolized, or leached out. In the central region, weakly podzolized loamy peats predominate, and it is there that the most fertile, and hence most cultivated, soils are found. In the southeast there are sandy soils, somewhat loamy and moderately podzolized. Sandy soils in fact cover one-fourth of Lithuania, and most of these are blanketed by woodlands. Climate The climate of the country is transitional between the maritime type of western Europe and the continental type found farther east. As a result, damp air masses of Atlantic origin predominate, alternating with continental Eurasian and, more rarely, colder Arctic air or air with a southern, tropical origin. Baltic Sea influences dominate a comparatively narrow coastal zone. The mean temperature for January, the coldest month, is in the low 20s F (about −5 °C), while July, the warmest month, has an average temperature in the 60s F (about 17 °C). Average annual rainfall usually exceeds 30 inches (about 800 mm), diminishing inland. Rainfall reaches a peak in August, except in the maritime strip, where the maximum is reached two to three months later. Plant and animal life Lithuanian vegetation falls into three separate regions. In the maritime regions, pine forests predominate, and wild rye and various bushy plants grow on the sand dunes. Spruce trees are prevalent in the hilly eastern portion. The central region is characterized by large tracts of oak trees, with elegant birch forests in the northern portions, as well as distinctive black alder and aspen groves. Pine forests prevail in the south. Indeed, about one-third of the country is forested, and about another one-fifth is taken up by meadowlands. Swamps and marshlands account for only a small percentage of the total land. Wildlife is very diverse and includes numerous mammalian species. There are wolves, foxes, otters, badgers, ermine, wild boars, and many rodents. The deep forests harbour elk, stags, deer, beavers, mink, and water rats. Lithuania is also home to hundreds of species of birds, including white storks, ducks, geese, swans, cormorants, herons, hawks, and even an occasional bald eagle. There are many types of grouse and partridge as well. People Ethnic groups, languages, and religion Ethnic Lithuanians make up more than four-fifths of the country’s population; there are also Russians and Poles and lesser numbers of Belarusians, Ukrainians, Latvians, Tatars, Roma (Gypsies), and others. There was a significant Jewish community in Lithuania prior to World War II, and an influx of Jews from German-controlled Poland in 1941 boosted this population to nearly 250,000. By 1944, however, the majority of the population had been murdered, deported, or sent to concentration camps (see Holocaust). The official language of Lithuania is Lithuanian. Russian, Polish, Belarusian, Ukrainian, and other languages are spoken in the larger cities. Yiddish is commonly spoken by members of the tiny remaining Jewish community in Lithuania. Lithuania was the last pagan country in Europe, accepting Roman Catholicism in the late 14th century. About four-fifths of the population is Roman Catholic; there are smaller groups of Evangelical Lutherans and other Protestants, as well as people of other faiths. Elements of the pagan religion have survived in the countryside. Settlement patterns There has been a modest but steady movement of people to the cities since the 1990s, encouraged by the planning of regional centres, such as Alytus, Marijampolė, Utena, Plungė, and Mažeikiai. By the early 21st century about two-thirds of the total population lived in urban areas. Demographic trends Natural increase, rather than immigration, has accounted for most of Lithuania’s population growth in the early 21st century. The high birth rate distinguishes Lithuania from its Baltic neighbours, which have struggled to offset the aging of their populations. The comparatively high level of ethnic homogeneity in Lithuania and the persistence of Roman Catholicism in the face of decades of Soviet promulgation of atheism as the official state ideology further distinguish Lithuania from Latvia and Estonia, where historically German-Scandinavian religious and cultural values have predominated. Economy Even before independence from the U.S.S.R. was formally established, the Lithuanian government had embarked on a program of dismantling the Soviet economic system. Beginning in February 1991, laws were passed to facilitate privatization. Complications marred the government’s aspirations, however. Foremost, the bulk of Lithuania’s trade was still closely linked to the former republics of the U.S.S.R., which were themselves in the throes of economic collapse. Second, Lithuania was dependent on critically important foreign oil and natural gas and industrial raw materials. Finally, the transition to a market economy had caused high rates of inflation and unemployment. Nevertheless, the succeeding governments continued to implement stringent stabilization policies; by 1995 inflation had been reduced, and the country’s trade balance was positive for the first time since independence. Lithuania was admitted to the EU in 2004. More … Source: https://www.britannica.com/place/Lithuania

2022/02/16

GRENADA - THE SPICE ISLAND (TRAVEL VIDEO)

We travelled through Grenada and Carriacou for two and a half weeks mainly by bus. We stayed at a couple of great places and really enjoyed our stay on Carriacou. Luckily the tropical storm Bret lost power and only a bit of rain reached us.

2022/02/15

Fundacja Żydoteka zaprasza - Klub książki żydowskiej

Rozmowy o książkach to jedna z naszych ulubionych czynności, dlatego wraz z Żydoteka organizujemy we Wrocławiu literacki klub dyskusyjny! Spotkajmy się 23 lutego 2022 roku w Przejściu Dialogu, by się poznać i porozmawiać o literaturze żydowskiej. Spotkania będą się odbywać w kameralnej atmosferze i w miłej przestrzeni, dodatkowo zimowy czas umili nam kawa, herbata i coś słodkiego.

2022/02/15

Belgia - kraj komiksu

Belgium is considered as the country of the comic strip, also called the “Ninth Art Form”. Tintin, the Smurfs, Lucky Luke, Spirou and many other popular characters are known all over the world – but were born in Belgium. Our friends have now made it into the new Belgian passports, which from this year on will feature a “comic strip” theme. Belgian passports allows our citizens to travel to 149 countries (110 without visa) and are considered one of the best secured travel documents.

2022/02/15

Statehood Day of the Republic of Serbia

Serbia, country in the west-central Balkans. For most of the 20th century, it was a part of Yugoslavia. The capital of Serbia is Belgrade (Beograd), a cosmopolitan city at the confluence of the Danube and Sava rivers; Stari Grad, Belgrade’s old town, is dominated by an ancient fortress called the Kalemegdan and includes well-preserved examples of medieval architecture and some of eastern Europe’s most-renowned restaurants. Serbia’s second city, Novi Sad, lies upstream on the Danube; a cultural and educational centre, it resembles the university towns of nearby Hungary in many respects. Beginning in the 1920s, Serbia was an integral part of Yugoslavia (meaning “Land of the South Slavs”), which included the modern countries of Serbia, Croatia, Slovenia, Bosnia and Herzegovina, Kosovo, North Macedonia, and Montenegro. Long ruled in turn by the Ottoman Empire and Austria-Hungary, these component nations combined in 1918 to form an independent federation known as the Kingdom of Serbs, Croats, and Slovenes. In 1929 that federation was formally constituted as Yugoslavia. Serbia was the dominant part in this multiethnic union, though after World War II the nonaligned communist government of Josip Broz Tito accorded some measure of autonomy to the constituent republics and attempted to balance contending interests by dividing national administrative responsibilities (e.g., for intelligence and defense) along ethnic lines. After Tito’s death in 1980 and the collapse of communism in eastern Europe over the course of the following decade, resurgent nationalism reopened old rifts in Yugoslav society. Serbian (and later Yugoslav) leader Slobodan Milošević attempted to craft a “Greater Serbia” from the former union, but his policies instead led to the secession of Slovenia, Croatia, Bosnia and Herzegovina, and Macedonia and civil war in the early 1990s. The civil war caused the death or displacement of hundreds of thousands of people and prompted international sanctions against the country. In the late 1990s more blood was spilled when the Albanian-Muslim-dominated Serbian province of Kosovo declared independence, resulting in the intervention of the North Atlantic Treaty Organization (NATO) and the United Nations, the bombing of Belgrade, and the placement of Kosovo under UN administration from mid-1999. Milošević was later defeated in presidential elections and arrested and tried before the International Court of Justice for war crimes, but the rump Yugoslavia remained unstable, as Montenegro threatened to declare independence before negotiating an agreement that maintained the country’s unification in a loose federation. In 2003, after the ratification of the pact by the parliaments of Serbia, Montenegro, and Yugoslavia, the renamed Serbia and Montenegro replaced Yugoslavia on the European map. In 2006 this loose federation came to an end, as Montenegro and Serbia were recognized as independent nations. Meanwhile, multilateral talks to determine Kosovo’s future status failed to yield a solution acceptable to both Serbs and Kosovars. Despite Serbia’s opposition, Kosovo formally seceded in February 2008. Likening the strife and dissolution that ravaged the country during the 1990s to a children’s game, Serbian poet Vasko Popa once wrote: By the early 21st century, Serbia was putting behind it the tragedy of its recent past to rebuild as a singular, independent country on a new Balkan Peninsula. Land Bounding the country to the west are the Republic of Bosnia and Herzegovina and the Slavonian region of the Republic of Croatia. Serbia adjoins Hungary to the north, Romania and Bulgaria to the east, North Macedonia to the south, and Montenegro to the southwest. Kosovo, which Serbia does not recognize as an independent country, lies to the south as well, along the northeastern border of Albania. Relief The landforms of Serbia, a landlocked country, fall into regional groupings that roughly parallel the republic’s major political divisions. The plains of the northern Vojvodina region generally lie at elevations between 200 and 350 feet (60 to 100 metres) above sea level. The Fruška Gora hills interrupt these plains on the west, stretching along a triangle of land between the Danube and Sava rivers. Their highest point is 1,765 feet (540 metres). Much of the Vojvodina is blanketed by portions of a former plateau that rose up to 100 feet (30 metres) above the territory’s floodplains; the remnants are composed of fine particles of loess deposited by winds during the last glacial period in Europe. Hills and high mountains characterize the central body of Serbia. Its western margins include sections of the Dinaric Alps, and its eastern borderlands are part of the Carpathian and Rhodope mountain systems. Between these flanking mountains lie the Šumadija hills, the core of the medieval Serbian state. The granite ridge of the Kopaonik Mountains, in Serbia’s southwestern Dinaric zone, reaches 6,617 feet (2,017 metres). This is a tectonically active region notable for earthquakes. To the east the Carpathians are nearly as high; one peak in the Balkan Mountains (Stara Planina) bordering Bulgaria attains an elevation of more than 7,000 feet (2,100 metres). Summits of the Šumadija hills range from 2,000 to 3,500 feet (600 to 1,100 metres). Serbia’s northeastern border follows the Iron Gate (Ðerdap) gorge of the Danube River, the most spectacular such feature in Europe. For a distance of 60 miles (100 km), the Danube flows across the Carpathian range, its bed dropping 90 feet (30 metres). The gorge consists of four narrow constrictions connected by three basins. Before the flooding that followed completion of the joint Yugoslav-Romanian Ðerdap hydroelectric dam in 1972, rocky outcrops confined the river at one point to a width of only 300 feet (90 metres). Upstream, in the Vojvodina plains, the Danube attains widths of up to 2 miles (3 km) and depths of 45 feet (14 metres) or more. Drainage of Serbia Serbia’s drainage is primarily to the Danubian system and flows into the Black Sea. The Tisa River is the most prominent tributary of the Danube in the Vojvodina, entering the province from Hungary south of the city of Szeged. Runoff from the southern slopes of the Fruška Gora flows into the Sava River, a major western tributary of the Danube. The Morava, or Velika Morava, River is the largest stream entirely within Serbia. It has a length of 290 miles (470 km) and flows northward into the Danube, draining two-fifths of Serbian territory. Tributaries of the Vardar River tap a small section of southeastern Serbia; the river itself flows southward across North Macedonia to the Aegean Sea. The valleys of the Morava and Vardar rivers have constituted a major route between central Europe and the eastern Mediterranean since prehistoric times. A railroad and modern highway now follow this ancient path. Other than reservoirs behind hydroelectric dams, Serbia has no appreciable lakes. Its largest natural body of water is Lake Palić in the Vojvodina, with a surface area of less than 2 square miles (5 square km). Soils Three principal soil types characterize the region, corresponding to its major divisions in landforms and climate. The subhumid plains and tablelands of the Vojvodina north and east of the Danube are characterized by organically rich black earth soils (chernozems) derived from the decaying root systems of countless generations of native grasses. In the forested hills and mountains south of the Danube, the soils tend to be less-fertile and weakly acidic brown podzolics. In cultivated areas these have been enriched by the incorporation of nutrients from fodder crops and animal manures. Infertile podzol soils predominate in the mountains and are characterized by an ash-coloured upper layer resulting from the leaching of all but their insoluble quartz particles by the acids generated in the slow decay of pine needles and other litter of the forest floors. Climate Differences in elevation, proximity to the sea, and exposure to wind lead to significant climatic differences within Serbia. In general, however, the climate is continental, with cold, relatively dry winters and warm, humid summers. The difference between average temperatures in January and July in Belgrade is 40 °F (22 °C). The Vojvodina most clearly exhibits characteristics of the continental climate. July temperatures average about 71 °F (22 °C), and January temperatures hover around 30 °F (−1 °C). Summer temperatures in mountainous areas of Serbia are notably cooler, averaging about 64 °F (18 °C). Air masses from eastern and northern Europe predominate throughout the year. Only occasionally do Mediterranean air masses reach Serbia from the southeast or south. Precipitation in Serbia ranges from 22 to 75 inches (560 to 1,900 mm) per year, depending on elevation and exposure. The lowest amounts are found in the Vojvodina. Most precipitation falls during the warm half of the year, with maximums occurring in late spring and late autumn. Winter precipitation tends to fall as snow, with 40 days of snow cover in northern lowlands and 120 days in the mountains. Plant and animal life The vegetation of Serbia forms a transition between central European and Mediterranean types. Before Austrian agricultural colonization began in the 18th century, the dry Vojvodina plains were a grassland steppe. However, it is evident that forests at one time dominated the region. Only about 5 percent of the area is now covered by trees, mostly in the higher parts of the Fruška Gora and in wetlands adjacent to the Danube and Sava. Up to one-third of Serbia proper is in broad-leaved forest, mostly oak and beech. The regional name Šumadija literally means “forested area,” but large areas that were formerly wooded long have been cleared and put to cultivation. In mountainous areas trees cover two-fifths or more of the territory, depending on elevation and soil thickness. Serbia has a rich diversity of wild animals. Among larger mammals, deer and bear abound in forested areas. Wild pigs (Sus scrofa) are a distinctive feature of beech forests in the mountains. More … Source: https://www.britannica.com/place/Serbia

2022/02/15

New Zealand Promotion

For more canoe, kayak and paddle sport news visit http://www.sportscene.tv

2022/02/11