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

2025/02/16

Top 10 Places to visit Lithuania | Vilnius, Lithuania, tourist attractions Top 10 |Lithuania Visa

Lithuania, officially the Republic of Lithuania, is a country in the Baltic region of Europe. Lithuania is considered to be one of the Baltic states. The country is situated along the southeastern shore of the Baltic Sea, to the east of Sweden and Denmark.

2025/02/15

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

2025/02/15

Serbia promo video | Drone travel video

Serbia is not a mass-tourism destination but nevertheless has a diverse range of touristic products. In 2018, total of over 3.4 million tourists were recorded in accommodations, of which half were foreign. Foreign exchange earnings from tourism were estimated at $1.5 billion.

2025/02/14

Visit Iran | Official Travel Guide of Iran

Iran owns an enormous wealth of traditional masterpieces remained from old, middle, and modern arenas. The geographical location of Iran, bridging west to ...

2025/02/13

Iran Travel Video——Colorful Persian

Iran is the favorite country I have been to. She is warm, friendly and safe, and has too many colorful scenes. Please don't misunderstand her. She is also an ancient civilization with a history of 5,000 years. You are here, you will fall in love with it. I am grateful to those who have helped me during my trip to Iran, and to all the Iranian friends who have appeared in the picture.

2025/02/10

Pure Grenada: The Official Website of the Grenada Tourism ...

Welcome to Pure Grenada, a hidden gem with unspoiled beauty offering a lifestyle so pure and authentic that you will feel instantly renewed.

2025/02/09

Welcome to New Zealand | Official site for Tourism New Zealand

Welcome to New Zealand. Get official travel information, maps, itineraries, best time to travel & things to do to help you plan your next holiday to New ..

2025/02/08

Granada's Independence Day

Grenada, byname Isle of Spice, island country of the West Indies. It is the southernmost island of the north-south arc of the Lesser Antilles, lying in the eastern Caribbean Sea about 100 miles (160 km) north of the coast of Venezuela. Oval in shape, the island is approximately 21 miles (34 km) long and 12 miles (19 km) wide. The southern Grenadines—the largest of which is Carriacou, about 20 miles (32 km) north-northeast, with an area of 13 square miles (34 square km)—are a dependency. The capital, St. George’s, on the southwest coast, is also the main port, having a fine natural harbour, and its picturesque pastel-coloured houses rise up the hillsides from the waterfront. The waterfront itself is known as the Carenage because island schooners were once careened (beached for cleaning or repair) there. St. George’s is the yachting and charter-boat centre of the eastern Caribbean. Land - Relief Grenada is volcanic in origin, with a ridge of mountains running north and south—the steeper slopes to the west and a more gradual incline to the east and southeast. The highest point is Mount St. Catherine (2,757 feet [840 metres]) in the northern part of the interior. The landscape is scenic, with fairly deep steep-sided valleys and about 10,000 acres (4,000 hectares) of forest. Drainage and soils Several short, swiftly flowing streams supply all towns and most villages with piped clean water. A further source of water is Grand Etang, a lake covering 36 acres in the crater of an extinct volcano at an elevation of 1,740 feet (530 metres). The fertile soils are chiefly volcanic, with some limestone in the north. Climate The island has equable temperatures, varying with altitude and averaging 82 °F (28 °C). Rainfall is adequate, except in the Point Salines area in the southwest; it varies from an average of 60 inches (1,500 mm) in coastal districts to more than 150 inches (3810 mm) in the mountainous regions. The rainy season lasts from June to December. November is the wettest month, but showers occur frequently during the other months. Grenada lies south of the usual track of hurricanes, but when they do occur, as in 1955, 1979, and 1980, they often cause extensive damage. Plant and animal life The island is verdant, with a year-round growing season and a wide variety of tropical fruits, flowering shrubs, and ferns. There are also forests of teak, mahogany, saman (known as the rain tree), and blue mahoe (a strong-fibred tree) in the interior. The animal life is varied and includes such wild animals as the mona monkey (a small, long-tailed, West African species that was introduced by slaves), the manicou (a species of opossum), the agouti (a rabbit-sized rodent, which is brown or grizzled in colour), the iguana, the mongoose, and a variety of turtles and land crabs. People Most of the population is black, having descended from African slaves, and there is a large minority of mulattoes and other mixtures. There are also small minorities of East Indians, descendants of indentured labourers brought to replace the freed slaves; descendants of the old French and British settlers; and more-recent immigrants from North America and Europe. Although English is the accepted language, a form of patois is still spoken by older people in the villages. Nearly one-half of the population is Protestant. More than one-third is Roman Catholic, and small but significant portions of the population adhere to the Rastafarian and Jehovah’s Witnesses’ faiths. Although Grenada is densely populated, its population grew slowly during the 20th century. Economy Agriculture and tourism are the most important sectors of the economy, although fishing and agriculturally based industries are becoming more significant. Grenada relies on financial support from the United Kingdom and other sources to bolster the economy. Agriculture, forestry, and fisheries To a greater extent than in most West Indian islands, Grenada’s arable land is divided into small holdings on which peasant proprietors cultivate diversified crops. Because of these small holdings and the generally hilly terrain, mechanical tilling is rare. The major agricultural export crops—cocoa, bananas, nutmeg, and mace—in the past were controlled by cooperative associations, but these associations have begun to come under greater government control. Banana exports depend upon preferential terms given by the United Kingdom and are affected by the policies of the European Union. Exports of mace and lime juice provide substantial earnings. Copra and, increasingly, other products processed from the coconut are also exported, and a wide variety of tropical fruits—mangoes, passion fruit, guavas, tamarind, and citrus fruits—are grown. The government has encouraged increased production of staple vegetables, such as peas, tomatoes, sweet potatoes, pumpkins, and corn (maize). The island’s forests yield mostly teak and mahogany, and the government has worked to upgrade fishing. Manufacturing, services, and trade Tourism, a major factor in the island’s economy, has been encouraged by the government. Air transport facilities have been improved, and the harbour is visited by numerous cruise ships. Other sources of employment are such secondary industries as clothing manufacture, sugar milling, brewing, rum distilling (a strong white rum being made for local consumption), food canning, copra processing, cigarette manufacturing, and soapmaking. There is a cotton ginnery on Carriacou. Grenada’s principal trading partner is the United States. Exports go largely to the United States, Germany, Malaysia, the Netherlands, and Egypt and to other Caribbean countries. Most imports come from the United States, China, the United Kingdom, Malaysia, and Barbados. Transportation of Grenada Bus service is available between the larger towns and villages. An international airport at Point Salines was inaugurated in 1984. Pearls Airport—providing service to nearby islands with connecting flights to Venezuela—is located on the northeastern coast. An airport on Carriacou also provides flights to nearby islands. The harbour at St. George’s has berths for oceangoing vessels, as well as a yacht basin and service facilities. Several shipping lines maintain regular passenger and cargo services to North America, the United Kingdom, Europe, and neighbouring West Indian islands. Government and society - Constitutional framework Grenada is governed as a constitutional monarchy, with the British monarch represented by a governor-general as the nominal head of state. Executive authority is vested in a prime minister, who is the head of the majority party in the elected House of Representatives, the lower house of the two-chamber legislature. The Senate is appointed by the governor-general on the advice of the prime minister and the opposition leader. Health and welfare Grenada has several main health centres, as well as district medical stations. Medical and dental treatment in government hospitals and clinics is free. The government has launched a program to eradicate malaria and mongoose-spread rabies. Education School attendance is not compulsory, although primary and secondary education is free. Grenada has vocational and technical schools as well as the St. George’s University School of Medicine and a branch of the University of the West Indies. Cultural life The Grenada National Museum in St. George’s is dedicated to archaeology and history and houses the Grenada Historical Society. Two Grenadian artists, Elinus Cato and Canute Caliste, have achieved international recognition for their primitive-style paintings. Several weekly newspapers are published, and islandwide radio and television broadcasting is available. History Grenada was sighted by Christopher Columbus on August 15, 1498, when he sailed past the island without landing and gave it the name Concepción. The origin of the name Grenada remains obscure. After Europeans first encountered it, Grenada was dominated for 150 years by the warlike Carib people, who had earlier killed off the more peaceful Arawak. In 1609 British merchants attempted to form a settlement, but the Caribs forced them to leave. More … Source: https://www.britannica.com/place/Grenada

2025/02/07