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.

2024/02/15

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

2024/02/15

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.

2024/02/14

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.

2024/02/09

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 ..

2024/02/08

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

2024/02/07

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.

2024/02/06

Waitangi Day New Zealand

New Zealand, Māori Aotearoa, island country in the South Pacific Ocean, the southwesternmost part of Polynesia. New Zealand is a remote land—one of the last sizable territories suitable for habitation to be populated and settled—and lies more than 1,000 miles (1,600 km) southeast of Australia, its nearest neighbour. The country comprises two main islands—the North and the South Island—and a number of small islands, some of them hundreds of miles from the main group. The capital city is Wellington and the largest urban area Auckland; both are located on the North Island. New Zealand administers the South Pacific island group of Tokelau and claims a section of the Antarctic continent. Niue and the Cook Islands are self-governing states in free association with New Zealand. New Zealand is a land of great contrasts and diversity. Active volcanoes, spectacular caves, deep glacier lakes, verdant valleys, dazzling fjords, long sandy beaches, and the spectacular snowcapped peaks of the Southern Alps/Kā Tiritiri o te Moana on the South Island—all contribute to New Zealand’s scenic beauty. New Zealand also has a unique array of vegetation and animal life, much of which developed during the country’s prolonged isolation. It is the sole home, for example, of the long-beaked, flightless kiwi, the ubiquitous nickname for New Zealanders. New Zealand was the largest country in Polynesia when it was annexed by Great Britain in 1840. Thereafter it was successively a crown colony, a self-governing colony (1856), and a dominion (1907). By the 1920s it controlled almost all of its internal and external policies, although it did not become fully independent until 1947, when it adopted the Statute of Westminster. It is a member of the Commonwealth. The ascent of Mount Everest by New Zealander Sir Edmund Hillary with Sherpa Tenzing Norgay in 1953 was one of the defining moments of the 20th century. “In some ways,” Hillary suggested, “I believe I epitomise the average New Zealander: I have modest abilities, I combine these with a good deal of determination, and I rather like to succeed.” Despite New Zealand’s isolation, the country has been fully engaged in international affairs since the early 20th century, being an active member of a number of intergovernmental institutions, including the United Nations. It has also participated in several wars, including World Wars I and II. Economically the country was dependent on the export of agricultural products, especially to Great Britain. The entry of Britain into the European Community in the early 1970s, however, forced New Zealand to expand its trade relations with other countries. It also began to develop a much more extensive and varied industrial sector. Tourism has played an increasingly important role in the economy, though this sector has been vulnerable to global financial instability. The social and cultural gap between New Zealand’s two main groups—the indigenous Māori of Polynesian heritage and the colonizers and later immigrants from the British Isles and their descendants—has decreased since the 1970s, though educational and economic differences between the two groups remain. Immigration from other areas—Asia, Africa, and eastern Europe—has also made a mark, and New Zealand culture today reflects these many influences. Minority rights and race-related issues continue to play an important role in New Zealand politics. Land New Zealand is about 1,000 miles (1,600 km) long (north-south) and about 280 miles (450 km) across at its widest point. The country has slightly less surface area than the U.S. state of Colorado and a little more than the United Kingdom. About two-thirds of the land is economically useful, the remainder being mountainous. Because of its numerous harbours and fjords, the country has an extremely long coastline relative to its area. Relief of New Zealand Although New Zealand is small, its geologic history is complex. Land has existed in the vicinity of New Zealand for most of the past 500 million years. The earliest known rocks originated as sedimentary deposits some 545 million to 540 million years ago, at the close of Precambrian time (4.6 billion to 541 million years ago) and the beginning of the Cambrian Period (541 million to 485 million years ago); their source area was probably the continental forelands of Australia and Antarctica, then part of a nearby single supercontinent. Continental drift (the movement of large plates of Earth’s crust) created a distinct island arc and oceanic trench structure by the Carboniferous Period (about 359 to 299 million years ago), when deposition began in the downwarps (trenches) of the sedimentary rocks that today make up some three-fourths of New Zealand. This environment lasted about 250 million years and is typified by both downwarped oceanic sedimentary rocks and terrestrial volcanic rocks. This period was terminated in the west at the beginning of the Cretaceous Period (about 145 million years ago) by the Rangitata Orogeny (mountain-building episode), although downwarp deposition continued in the east. These mountains were slowly worn down by erosion, and the sea transgressed, eventually covering almost all of the land. At the end of the Oligocene Epoch (about 23 million years ago), the Kaikōura Orogeny began, raising land above the sea again, including the Southern Alps/Kā Tiritiri o te Moana of the South Island. Many of the great earth movements associated with this final orogeny took place (and take place today) along faults, which divide the landscape into great blocks, chief of which is the Alpine Fault of the South Island. The erosion and continued movement of these faulted blocks, together with the continuing volcanism of the North Island, define to a large extent the landscape of the country. New Zealand is part of the Ring of Fire—the circum-Pacific seismic belt marked by frequent earthquakes and considerable volcanic activity. The North Island and the western part of the South Island are on the Indian-Australian Plate, and the remainder of the South Island is on the Pacific Plate. Their collision creates violent seismic activity in subduction zones and along faults. Numerous earthquakes occur annually, including hundreds that can be felt by New Zealanders. A number of these temblors have been disastrous, such as one that devastated the towns of Napier and Hastings in 1931 and a series of quakes that did likewise in Christchurch in 2010–11. Both the North and the South islands are roughly bisected by mountains. Swift snow-fed rivers drain from the hills, although only in the east of the South Island have extensive alluvial plains been built up. The alluvial Canterbury Plains contrast sharply with the precipitous slopes and narrow coastal strip of the Westland region on the west coast of the South Island. The Southern Alps/Kā Tiritiri o te Moana are a 300-mile- (480-km-) long chain of fold mountains containing New Zealand’s highest mountain—Aoraki/Mount Cook at 12,316 feet (3,754 metres)—and some 20 other peaks that rise above 10,000 feet (3,000 metres), as well as an extensive glacier system with associated lakes. There are more than 360 glaciers in the Southern Alps/Kā Tiritiri o te Moana. The Tasman Glacier, the largest in New Zealand, with a length of 18 miles (29 km) and a width of more than 0.5 mile (0.8 km), flows down the eastern slopes of Aoraki/Mount Cook. Other important glaciers on the eastern slopes of the Southern Alps/Kā Tiritiri o te Moana are the Murchison, Mueller, and Godley; the Fox and Franz Josef are the largest on the western slopes. The North Island has seven small glaciers on the slopes of Mount Ruapehu. In the north of the South Island, the Alps break up into steep upswelling ridges. On their western face there are mineral deposits, and to the east they continue into two parallel ranges, terminating in a series of sounds. To the south the Alps break up into rugged, dissected country of difficult access and magnificent scenery, particularly toward the western tip of the island (called Fiordland). On its eastern boundary this wilderness borders a high central plateau called Central Otago, which has an almost continental climate. The terrain of the North Island is much less precipitous than that of the South and has a more benign climate and greater economic potential. In the centre of the island, the Volcanic Plateau rises abruptly from the southern shores of Lake Taupō, New Zealand’s largest natural lake, itself an ancient volcanic crater. To the east, ranges form a backdrop to rolling country in which pockets of highly fertile land are associated with the river systems. To the south, more ranges run to the sea. On the western and eastern slopes of these ranges, the land is generally poor, although the western downland region is fertile until it fades into a coastal plain dominated by sand dunes. To the west of the Volcanic Plateau, fairly mountainous country merges into the undulating farmlands of the Taranaki region, where the mild climate favours dairy farming even on the slopes of Mount Taranaki (Mount Egmont), a volcano that has been dormant since the 17th century. North of Mount Taranaki are the spectacular Waitomo caves, where stalactites and stalagmites are illuminated by thousands of glowworms. The northern shores of Lake Taupō bound a large area of high economic activity, including forestry. Even farther north there are river terraces sufficiently fertile for widespread dairy and mixed farming. The hub of this area is Auckland, which is situated astride an isthmus with a deep harbour on the east and a shallow harbour on the west. The peninsular region north of Auckland, called Northland, becomes gradually subtropical in character, marked generally by numerous deep-encroaching inlets of the sea bordered by mangrove swamps. More … Source: https://www.britannica.com/place/New-Zealand

2024/02/06

New Zealand Promotion

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

2024/02/05