Nouakchott City, the Capital of Mauritania.

2025/11/27

Tourism Bosnia and Herzegovina: Visit BiH | The heart

Planning a holiday to BiH? Discover everything you need to know about visiting Bosnia and Herzegovina with the official guide.

2025/11/27

Visit Albania 2018 | Go Your Own Way

Albania retains one of the last unspoiled coastlines in the Mediterranean. Sun-drenched mountains and white-sand beaches spill into the bright blue waters of the Adriatic Sea, while Ancient Greek ruins and historic Ottoman villages punctuate the surrounding rural landscape. You’ll find none of the usual high-rise resorts, crowded shores and high prices typical in the rest of the Med here, with fresh seafood, quality bars and comfortable accommodation available at a fraction of the cost.

2025/11/27

Independence Day of the Republic of Suriname

Suriname, country located on the northern coast of South America. Suriname is one of the smallest countries in South America, yet its population is one of the most ethnically diverse in the region. Its economy is dependent on its extensive supply of natural resources, most notably bauxite, of which it is one of the top producers in the world. The southern four-fifths of the country is almost entirely covered with pristine tropical rainforest. Formerly known as Dutch Guiana, Suriname was a plantation colony of the Netherlands that gained its independence on November 25, 1975. From 1980 to 1987 the country was governed by a succession of military regimes. A new civilian constitution was approved in 1987. Another military coup took place in 1990, but the country returned to civilian rule the following year. The capital, Paramaribo, lies 9 miles (15 km) from the Atlantic Ocean on the Suriname River. Land Suriname is bordered by the Atlantic Ocean to the north, by French Guiana to the east, by Brazil to the south, and by Guyana to the west. Suriname is involved in territorial disputes with both Guyana and French Guiana that are legacies of colonial rule. The dispute with Guyana centres on the New River Triangle, a 6,000-square-mile (15,600-square-km) area between two tributaries of the Courantyne River in southern Guyana. In addition to claiming the New River Triangle, Suriname also contests its border with Guyana along the Courantyne: Suriname claims sovereignty over the entire river and thus views its west bank as the border, while Guyana claims that the thalweg, or deepest channel of the river, is the boundary. In 2007 a United Nations international tribunal settled another long-standing boundary dispute between the two countries, in which Suriname was awarded one-third of a disputed area of the Caribbean Sea. The area in contention with French Guiana is the 5,000-square-mile (13,000-square-km) region between the Itany and Marouini rivers in the southwestern corner of French Guiana. Relief The narrow coastal zone, some 226 miles (364 km) long, consists of sandbanks and mudbanks deposited by the southern equatorial currents from the area surrounding the mouth of the Amazon River (located to the east of Suriname, in Brazil). South of the mudbanks begins the New Coastal Plain, also formed from sand and clay from the mouth of the Amazon. The region, covering some 6,600 square miles (17,000 square km), consists of swampland. The soil of the swamps is clay, in which a great deal of peat has formed. The region is traversed by sandy ridges that run parallel to the coast. South of the New Coastal Plain is the Old Coastal Plain, which covers some 1,550 square miles (4,000 square km). It consists largely of fine clays and sands and contains a variety of topographies, including old ridges, clay flats, and swamps. South of the Old Coastal Plain is the Zanderij formation, a 40-mile- (64-km-) wide landscape of rolling hills. This formation rests on bleached sand sediments, which are rich in quartz. Most of the region is covered by tropical rainforest, but swamps and areas of savanna grassland are also found. Farther to the south, bordering Brazil, is an area consisting largely of a central mountain range, its various branches, and scattered hilly areas; a vast tropical rainforest covers these highlands. The highest summit, at 4,035 feet (1,230 metres), is Juliana Top, in the Wilhelmina Mountains. In the southwest near the Brazilian border is the Sipaliwini Plain, another savanna area. Drainage and soils Suriname’s major rivers flow northward into the Atlantic. They include the Courantyne, which forms part of the boundary with Guyana; the Coppename; the Suriname; and the Maroni, which forms part of the border with French Guiana. Suriname’s most fertile soils occur in the inundated lands reclaimed by diking and drainage (polders), which are principally in the New Coastal Plain. Climate Suriname has a tropical climate. The populated area in the north has four seasons: a minor rainy season from early December to early February, a minor dry season from early February to late April, a major rainy season from late April to mid-August, and a major dry season from mid-August to early December. Daytime temperatures in Paramaribo range between 70 and 90 °F (21 and 32 °C). In the interior, diurnal temperature extremes can vary by as much as about 20 degrees. However, the range in average temperatures between the warmest month, September, and the coldest, January, is only about 3 degrees. Rainfall is highest in the central and southeastern parts of the country. Annual rainfall averages about 75 inches (1,900 mm) in the west and 95 inches (2,400 mm) in Paramaribo. Plant and animal life The flora of the coastal area is better known than that of the interior. It consists of some 4,000 species of ferns and seed plants and a large number of mosses, weeds, and mildews. About nine-tenths of Suriname’s area is covered with heterogeneous forest consisting of more than 1,000 species of trees. The baboen (Virola surinamensis), which grows in the coastal area, is used to make plywood. The kapok (Ceiba pentandra) reaches a height of more than 150 feet (45 metres). The Central Suriname Nature Reserve, covering nearly 3,950,000 acres (1,600,000 hectares), was established in June 1998 in west-central Suriname. It is one of the largest protected areas of rainforest in the world and was designated a UNESCO World Heritage site in 2000. There are some 150 species of mammals, including monkeys, wild pigs, deer, manatees, jaguars, ocelots, armadillos, sloths, and anteaters. The tapir is the largest land mammal. Reptiles include caimans, iguanas, and the boa constrictor. The beaches on the eastern part of the coast are breeding grounds for marine turtles, which are protected by law. About 650 species of birds, including hummingbirds, vultures, and parrots, have been identified. Some 350 species of fish occupy coastal and inland waters. People of Suriname - Ethnic groups South Asians, descendants of contract labourers from India, are the largest ethnic group in Suriname, making up more than one-fourth of the population. The second major ethnic group, accounting for about one-fifth of the population, is the Maroons (descendants of escaped slaves of African origin). Creoles, who in Suriname are people of mainly African descent, constitute between one-tenth and one-fifth of the population. The descendants of Javanese (people from the island of Java in Indonesia) contract labourers and people of mixed ethnicity each make up almost one-seventh of the population. Indians, descendants of the original inhabitants of Suriname, make up only a tiny fraction of the population. The coastal groups include the Carib and Arawak, while the Trio (Tiriyo), Wayana-Aparai, Warao (Warrau), Wayarekule (Akuriyo), Tucayana, and Akurio live in the interior. Minor ethnic groups in Suriname include descendants of Chinese, Lebanese, Portuguese, and Dutch immigrants; Creoles from the West Indies; and U.S. citizens. More-recent immigrants include Chinese—known in Suriname as “New Chinese” to distinguish them from the descendants of those Chinese who were brought over as labourers in the 19th century—and Brazilians who arrived in the late 20th and early 21st centuries. Languages Dutch is the official language of Suriname, but the extent to which members of the various ethnic groups are able to use the language differs. Most of the population learns Dutch as a second language. Additional languages include Sranan and other creole languages; English; Sarnami, which originated from Hindi and Urdu; Javanese; and a number of Maroon and South American Indian languages. More … Score: https://www.britannica.com/place/Suriname  

2025/11/25

Bosnia and Herzegovina Statehood Day

Bosnia and Herzegovina, country situated in the western Balkan Peninsula of Europe. The larger region of Bosnia occupies the northern and central parts of the country, and Herzegovina occupies the south and southwest. These historical regions do not correspond with the two autonomous political entities that were established by the internationally brokered Dayton Accords of 1995: the Republika Srpska (Bosnian Serb Republic), located in the north and east, and the Federation of Bosnia and Herzegovina, occupying the western and central areas. The capital of the country is Sarajevo; important regional cities include Mostar and Banja Luka. The land has often felt the influences of stronger regional powers that have vied for control over it, and these influences have helped to create Bosnia and Herzegovina’s characteristically rich ethnic and religious mix. Islam, Orthodox Christianity, and Roman Catholicism are all present, with the three faiths generally corresponding to three major ethnic groups: Bosniaks, Serbs, and Croats, respectively. This multiethnic population, as well as the country’s historical and geographic position between Serbia and Croatia, has long made Bosnia and Herzegovina vulnerable to nationalist territorial aspirations. Ruled by the Ottoman Empire from the 15th century, the region came under the control of Austria-Hungary in 1878 and subsequently played a key role in the outbreak of World War I. In 1918 it was incorporated into the newly created Kingdom of Serbs, Croats, and Slovenes, where it had no formal status of its own. After World War II it became a constituent republic of the Socialist Federal Republic of Yugoslavia. Following the disintegration of that state in 1991, the majority of the population of Bosnia and Herzegovina voted for independence in a 1992 referendum. Much of the country’s Serb population, however, opposed independence and boycotted the referendum. War soon consumed the region, as ethnic nationalists within Bosnia and Herzegovina, with the support of Serbia and Croatia in some cases, tried to take control of territories they claimed as their own. Horrific ethnic cleansing campaigns between 1992 and the end of 1995 killed thousands and violently displaced more than two million people in much of Bosnia and Herzegovina. International intervention into the Bosnian conflict led finally to a peace agreement, the Dayton Accords, in late 1995. The Dayton agreement ended the war in Bosnia and Herzegovina, but it also established the country as a fragile, highly decentralized, and ethnically divided state in which an international civilian representative remains authorized to impose legislation and to remove domestic officials in order to protect the peace. Although the vast majority of citizens continue to desire sustainable peace, they hold to different ideas about the best configuration of the state, and some even question its future existence. Land - Relief The roughly triangular-shaped Bosnia and Herzegovina is bordered on the north, west, and south by Croatia, on the east by Serbia, on the southeast by Montenegro, and on the southwest by the Adriatic Sea along a narrow extension of the country. Bosnia and Herzegovina has a largely mountainous terrain. The Dinaric Alps dominate the western border with Croatia, and numerous ranges, including the Kozara, Vlašic, Plješevica, Grmeč, Cincar, and Raduša, run through the country, generally in a northwest-southeast direction. The highest peak, reaching 7,828 feet (2,386 metres), is Maglić, near the border with Montenegro. In the south and southwest is the Karst, a region of arid limestone plateaus that contain caves, potholes, and underground drainage. The uplands there are often bare and denuded (the result of deforestation and thin soils), but, between the ridges, depressions known as poljes are covered with alluvial soil that is suitable for agriculture. Elevations of more than 6,000 feet (1,800 metres) are common, and the plateaus descend abruptly toward the Adriatic Sea. The coastline, limited to a length of 12 miles (20 km) along the Adriatic Sea, is bounded on both sides by Croatia and contains no natural harbours. In central Bosnia the rocks and soils are less vulnerable to erosion, and the terrain there is characterized by rugged but green and often forested plateaus. In the north, narrow lowlands extend along the Sava River and its tributaries. Geologic fault lines are widespread in the mountainous areas. In 1969 an earthquake destroyed 70 percent of the buildings in Banja Luka. Drainage The principal rivers are the Sava, a tributary of the Danube that forms the northern boundary with Croatia; the Bosna, Vrbas, and Una, which flow north and empty into the Sava; the Drina, which flows north, forms part of the eastern boundary with Serbia, and is also a tributary of the Sava; and the Neretva, which flows from the southeast but assumes a sharp southwestern flow through the Karst region, continues through Croatia, and empties into the Adriatic Sea. Rivers in the Karst flow largely underground. Numerous glacial lakes dot the landscape. Bosnia and Herzegovina is also rich in natural springs, many of which are tapped for bottled mineral water or for popular thermal health spas. Climate Although situated close to the Mediterranean Sea, Bosnia and Herzegovina is largely cut off from its climatic influence by the Dinaric Alps. The weather in the Bosnia region resembles that of the southern Austrian highlands—generally mild, though apt to be bitterly cold in winter. In Banja Luka the coldest month is January, with an average temperature of about 32 °F (0 °C), and the warmest month is July, which averages about 72 °F (22 °C). During January and February Banja Luka receives the least amount of precipitation, and in May and June it experiences the heaviest rainfall. Herzegovina has more affinity to the Croatian region of Dalmatia, which can be oppressively hot in summer. In Mostar, situated along the Neretva River, the coldest month is January, averaging about 42 °F (6 °C), and the warmest month is July, averaging about 78 °F (26 °C). Mostar experiences a relatively dry season from June to September. The remainder of the year is wet, with the heaviest precipitation between October and January. More … Score: https://www.britannica.com/place/Bosnia-and-Herzegovina

2025/11/25

Incredible drone footage of Suriname: an introduction by All Suriname Tours

Incredible drone footage of a magnificent country in South America: Suriname. Filmed by Ronny Bhoelai and edited by Vincent van Grondelle.

2025/11/24

Life in Bosnia and Herzegovina - Promotional video | visitbosnia.eu

Promotional video of life in Bosnia and Herzegovina

2025/11/24

Visit Lebanon - Leisure Website

Cultural Tourism Religious Tourism Gastronomy & Oenology Nature, Sports & Adventure Ski Resorts Seaside & Beaches Weddings & Honeymoon Wellness Tourism

2025/11/24

Independence Day of the Republic of Lebanon

Lebanon, country located on the eastern shore of the Mediterranean Sea; it consists of a narrow strip of territory and is one of the world’s smaller sovereign states. The capital is Beirut. Though Lebanon, particularly its coastal region, was the site of some of the oldest human settlements in the world—the Phoenician ports of Tyre (modern Ṣūr), Sidon (Ṣaydā), and Byblos (Jubayl) were dominant centres of trade and culture in the 3rd millennium bce—it was not until 1920 that the contemporary state came into being. In that year France, which administered Lebanon as a League of Nations mandate, established the state of Greater Lebanon. Lebanon then became a republic in 1926 and achieved independence in 1943. Lebanon shares many of the cultural characteristics of the Arab world, yet it has attributes that differentiate it from many of its Arab neighbours. Its rugged, mountainous terrain has served throughout history as an asylum for diverse religious and ethnic groups and for political dissidents. Lebanon is one of the most densely populated countries in the Mediterranean area and has a high rate of literacy. Notwithstanding its meagre natural resources, Lebanon long managed to serve as a busy commercial and cultural centre for the Middle East. This outward image of vitality and growth nevertheless disguised serious problems. Not only did Lebanon have to grapple with internal problems of social and economic organization, but it also had to struggle to define its position in relation to Israel, to its Arab neighbours, and to Palestinian refugees living in Lebanon. The delicate balance of Lebanese confessionalism (the proportional sharing of power between the country’s religious communities) was eroded under the pressures of this struggle; communal rivalries over political power, exacerbated by the complex issues that arose from the question of Palestinian presence and from a growing “state within a state,” led to the outbreak of an extremely damaging civil war in 1975 and a breakdown of the governmental system. After the end of the civil war in 1990, Lebanon gradually reclaimed a degree of relative socioeconomic and political stability; because of the continued problems of external intervention and troubled confessional relations, however, many of Lebanon’s challenges persisted into the early 21st century. Land Lebanon is bounded to the north and east by Syria, to the south by Israel, and to the west by the Mediterranean Sea. Relief As in any mountainous region, the physical geography of Lebanon is extremely complex and varied. Landforms, climate, soils, and vegetation undergo some sharp and striking changes within short distances. Four distinct physiographic regions may be distinguished: a narrow coastal plain along the Mediterranean Sea, the Lebanon Mountains (Jabal Lubnān), Al-Biqāʿ (Bekaa) valley, and the Anti-Lebanon and Hermon ranges running parallel to the Lebanese Mountains. The coastal plain is narrow and discontinuous, almost disappearing in places. It is formed of river-deposited alluvium and marine sediments, which alternate suddenly with rocky beaches and sandy bays, and is generally fertile. In the far north it expands to form the ʿAkkār Plain. The snowcapped Lebanon Mountains are one of the most prominent features of the country’s landscape. The range, rising steeply from the coast, forms a ridge of limestone and sandstone, cut by narrow and deep gorges. It is approximately 100 miles (160 km) long and varies in width from 6 to 35 miles (10 to 56 km). Its maximum elevation is at Qurnat al-Sawdāʾ (10,131 feet [3,088 metres]) in the north, where the renowned cedars of Lebanon grow in the shadow of the peak. The range then gradually slopes to the south, rising again to a second peak, Jabal Ṣannīn (8,842 feet [2,695 metres]), northeast of Beirut. To the south the range branches westward to form the Shūf Mountains and at its southern reaches gives way to the hills of Galilee, which are lower.Al-Biqāʿ valley lies between the Lebanon Mountains in the west and the Anti-Lebanon Mountains in the east; its fertile soils consist of alluvial deposits from the mountains on either side. The valley, approximately 110 miles (180 km) long and from 6 to 16 miles (10 to 26 km) wide, is part of the great East African Rift System. In the south Al-Biqāʿ becomes hilly and rugged, blending into the foothills of Mount Hermon (Jabal al-Shaykh) to form the upper Jordan Valley. The Anti-Lebanon range (Al-Jabal al-Sharqī) starts with a high peak in the north and slopes southward until it is interrupted by Mount Hermon (9,232 feet [2,814 metres]). Drainage Lebanese rivers, though numerous, are mostly winter torrents, draining the western slopes of the Lebanon Mountains. The only exception is the Līṭānī River (90 miles [145 km] long), which rises near the famed ruins of Baalbek (Baʿlabakk) and flows southward in Al-Biqāʿ to empty into the Mediterranean near historic Tyre. The two other important rivers are the Orontes (Nahr al-ʿĀṣī), which rises in the north of Al-Biqāʿ and flows northward, and the Kabīr. Soils Soil quality and makeup in Lebanon vary by region. The shallow limestone soil of the mountains provides a relatively poor topsoil. The lower and middle slopes, however, are intensively cultivated, the terraced hills standing as a scenic relic of the ingenious tillers of the past. On the coast and in the northern mountains, reddish topsoils with a high clay content retain moisture and provide fertile land for agriculture, although they are subject to considerable erosion. Climate of Lebanon There are sharp local contrasts in the country’s climatic conditions. Lebanon is included in the Mediterranean climatic region, which extends westward to the Atlantic Ocean. Winter storms formed over the ocean move eastward through the Mediterranean, bringing precipitation at that season; in summer, however, the Mediterranean receives little or no precipitation. The climate of Lebanon is generally subtropical and is characterized by hot, dry summers and mild, humid winters. Mean daily maximum temperatures range from the low 90s F (low 30s C) in July to the low 60s F (mid-10s C) on the coast and low 50s F (low 10s C) in Al-Biqāʿ in January. Mean minimum temperatures in January are in the low 50s F on the coast and the mid-30s F (about 2 °C) in Al-Biqāʿ. At 5,000 feet (1,524 metres), the elevation of the highest settlements, these are reduced by about 15 °F (8 °C). Nearly all precipitation falls in winter, averaging 30 to 40 inches (750 to 1,000 mm) on the coast and rising to more than 50 inches (1,270 mm) in higher altitudes. Al-Biqāʿ is drier and receives 15 to 25 inches (380 to 640 mm). On the higher mountaintops, this precipitation falls as heavy snow that remains until early summer. Plant and animal life Lebanon was heavily forested in ancient and medieval times, and its timber—particularly its famed cedar—was exported for building and shipbuilding. The natural vegetation, however, has been grazed, burned, and cut for so long that little of it is regenerated. What survives is a wild Mediterranean vegetation of brush and low trees, mostly oaks, pines, cypresses, firs, junipers, and carobs. Few large wild animals survive in Lebanon, though bears are occasionally seen in the mountains. Among the smaller animals, deer, wildcats, hedgehogs, squirrels, martens, dormice, and hares are found. Numerous migratory birds from Africa and Europe visit Lebanon. Flamingos, pelicans, cormorants, ducks, herons, and snipes frequent the marshes; eagles, buzzards, kites, falcons, and hawks inhabit the mountains; and owls, kingfishers, cuckoos, and woodpeckers are common. Although Lebanon’s diverse and abundant plant and animal life suffered a heavy toll during the country’s lengthy civil war and subsequent conflicts, the post-civil war period was marked by the rise of fledgling environmental groups and movements that worked toward the creation of protected areas and parks in Lebanon’s sensitive ecological areas. A layer of crude oil covering the Ramlat al-Bayḍāʾ public beach in Beirut, Lebanon, following the 2006 warfare between Hezbollah and Israel. More … Score: https://www.britannica.com/place/Lebanon  

2025/11/22