The Syrian Arab Republic Independence Day

Syria, country located on the east coast of the Mediterranean Sea in southwestern Asia. Its area includes territory in the Golan Heights that has been occupied by Israel since 1967. The present area does not coincide with ancient Syria, which was the strip of fertile land lying between the eastern Mediterranean coast and the desert of northern Arabia. The capital is Damascus (Dimashq), on the Baradā River, situated in an oasis at the foot of Mount Qāsiyūn. After Syria gained its independence in 1946, political life in the country was highly unstable, owing in large measure to intense friction between the country’s social, religious, and political groups. In 1970 Syria came under the authoritarian rule of Pres. Hafiz al-Assad, whose foremost goals included achieving national security and domestic stability and recovering the Syrian territory lost to Israel in 1967. Assad committed his country to an enormous arms buildup, which put severe strains on the national budget, leaving little for development. After Assad’s death in 2000, his son Bashar al-Assad became president. Despite some early steps toward political reform, Bashar al-Assad ultimately continued his father’s authoritarian style of government, using Syria’s powerful military and security services to quash political dissent. Long-suppressed internal tensions led to the outbreak of the Syrian Civil War in 2011. Land Syria is bounded by Turkey to the north, by Iraq to the east and southeast, by Jordan to the south, and by Lebanon and Israel to the southwest. Relief Syria has a relatively short coastline, which stretches for about 110 miles (180 km) along the Mediterranean Sea between the countries of Turkey and Lebanon. Sandy bays dent the shore, alternating with rocky headlands and low cliffs. North of Ṭarṭūs, the narrow coastal strip is interrupted by spurs of the northwestern Al-Anṣariyyah Mountains immediately to the east. It then widens into the ʿAkkār Plain, which continues south across the Lebanon border. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe Now The Al-Anṣariyyah mountain range borders the coastal plain and runs from north to south. The mountains have an average width of 20 miles (32 km), and their average height declines from 3,000 feet (900 metres) in the north to 2,000 feet in the south. Their highest point, at 5,125 feet (1,562 metres), occurs east of Latakia. Directly to the east of the mountains is the Ghāb Depression, a 40-mile (64-km) longitudinal trench that contains the valley of the Orontes River (Nahr Al-ʿĀṣī). The Anti-Lebanon Mountains (Jabal Al-Sharqī) mark Syria’s border with Lebanon. The main ridge rises to a maximum height of 8,625 feet (2,629 metres) near Al-Nabk, while the mean height is between 6,000 and 7,000 feet (1,800 to 2,100 metres). Mount Hermon (Jabal Al-Shaykh), Syria’s highest point, rises to 9,232 feet (2,814 metres). Smaller mountains are scattered about the country. Among these are Mount Al-Durūz, which rises to an elevation of some 5,900 feet (1,800 metres) in the extreme south, and the Abū Rujmayn and Bishrī Mountains, which stretch northeastward across the central part of the country. The undulating plains occupying the rest of the country are known as the Syrian Desert. In general their elevation lies between 980 and 1,640 feet (300 and 500 metres); they are seldom less than 820 feet (250 metres) above sea level. The area is not a sand desert but comprises rock and gravel steppe; a mountainous region in the south-central area is known as Al-Ḥamād. Drainage The Euphrates River is the most important water source and the only navigable river in Syria. It originates in Turkey and flows southeastward across the eastern part of Syria (see Tigris-Euphrates river system). The Euphrates Dam, constructed on the river at Ṭabaqah, was completed in the 1970s. The reservoir behind the dam, Lake Al-Asad, began to fill in 1973. The Orontes is the principal river of the mountainous region. It rises in Lebanon, flows northward through the mountains and the Ghāb Depression, and enters the Mediterranean near Antioch, Turkey. The Yarmūk River, a tributary of the Jordan River, drains the Jabal Al-Durūz and Ḥawrān regions and forms part of the border with Jordan in the southwest. Scattered lakes are found in Syria. The largest is Al-Jabbūl, a seasonal saline lake that permanently covers a minimum area of about 60 square miles (155 square km) southeast of Aleppo. Other major salt lakes are Jayrūd to the northeast of Damascus and Khātūniyyah to the northeast of Al-Ḥasakah. Lake Muzayrīb, a small body of fresh water, is located northwest of Darʿā; the larger Lake Qaṭṭīnah (Lake Homs), a reservoir, is west of Homs. Most of the country’s drainage flows underground. On the surface, impervious rocks—consisting of clay, marl (clay, sand, or silt), and greensand—cover a relatively small area. Porous rocks cover about half of the country and are mainly sandstone or chalk. Highly porous rocks consist of basalt and limestone. Water penetrates the porous rocks, forming underground springs, rivers, or subterranean water sheets close to the surface. Although the springs are profuse, the water sheets are quickly exhausted and may turn saline in areas of low precipitation. More … Score: https://www.britannica.com/place/Syria

2026/04/17

"SYRIA" Top 40 Tourist Places | Syria Tourism

Syria, officially the Syrian Arab Republic, is a country in Western Asia, bordering Lebanon to the southwest, the Mediterranean Sea to the west, Turkey to the north, Iraq to the east, Jordan to the south, and Israel to the southwest.

2026/04/16

Destination Senegal a rich cultural heritage

Destination Senegal a rich cultural heritage

2026/04/06

Independence Day Republic of Senegal

Senegal, country in western Africa. Located at the westernmost point of the continent and served by multiple air and maritime travel routes, Senegal is known as the “Gateway to Africa.” The country lies at an ecological boundary where semiarid grassland, oceanfront, and tropical rainforest converge; this diverse environment has endowed Senegal with a wide variety of plant and animal life. It is from this rich natural heritage that the country’s national symbols were chosen: the baobab tree and the lion. The region today known as Senegal was long a part of the ancient Ghana and Djolof kingdoms and an important node on trans-Saharan caravan routes. It was also an early point of European contact and was contested by England, France, Portugal, and the Netherlands before ultimately coming under French control in the late 19th century. It remained a colony of France until 1960, when, under the leadership of the writer and statesman Léopold Senghor, it gained its independence—first as part of the short-lived Mali Federation and then as a wholly sovereign state. Although Senegal traditionally has been dependent on peanuts (groundnuts), the government has had some success with efforts to diversify the country’s economy. Even so, the country suffered an economic decline in the 20th century, owing in some measure to external forces such as the fall in value of the African Financial Community (Communauté Financière Africaine; CFA) franc and the high cost of debt servicing, as well as to internal factors such as a rapidly growing population and widespread unemployment. Almost two-fifths of Senegal’s people are Wolof, members of a highly stratified society whose traditional structure includes a hereditary nobility and a class of musicians and storytellers called griots. Contemporary Senegalese culture, especially its music and other arts, draws largely on Wolof sources, but the influences of other Senegalese groups (among them the Fulani, the Serer, the Diola, and the Malinke) are also evident. Wolof predominate in matters of state and commerce as well, and this dominance has fueled ethnic tension over time as less-powerful groups vie for parity with the Wolof majority. The most important city in Senegal is its capital, Dakar. This lively and attractive metropolis, located on Cape Verde Peninsula along the Atlantic shore, is a popular tourist destination. Although the government announced plans to eventually move the capital inland, Dakar will remain one of Africa’s most important harbours and an economic and cultural centre for West Africa as a whole. Senegal is home to several internationally renowned musicians and artists. Other aspects of Senegalese culture have traveled into the larger world as well, most notably Senghor’s espousal of Negritude—a literary movement that flourished in the 1930s, ’40s, and ’50s and that emphasized African values and heritage. Through events such as the World Festival of Negro Arts, first held in Senegal in 1966, and institutions such as the Fundamental Institute of Black Africa (Institut Fondamental d’Afrique Noire; IFAN) and the Gorée Island World Heritage site, Senegal honours Senghor’s dictum "We must learn to absorb and influence others more than they absorb or influence us." Land of Senegal Senegal is bounded to the north and northeast by the Sénégal River, which separates it from Mauritania; to the east by Mali; to the south by Guinea and Guinea-Bissau; and to the west by the Atlantic Ocean. The Cape Verde (Cap Vert) Peninsula is the westernmost point of the African continent. The Gambia consists of a narrow strip of territory that extends from the coast eastward into Senegal along the Gambia River and isolates the southern Senegalese area of Casamance. Relief Senegal is a flat country that lies in the depression known as the Senegal-Mauritanian Basin. Elevations of more than about 330 feet (100 metres) are found only on the Cape Verde Peninsula and in the southeast of the country. The country as a whole falls into three structural divisions: the Cape Verde headland, which forms the western extremity and consists of a grouping of small plateaus made of hard rock of volcanic origin; the southeastern and the eastern parts of the country, which consist of the fringes of ancient massifs (mountain masses) contiguous with those buttressing the massif of Fouta Djallon on the Guinea frontier and which include the highest point in the country, reaching an elevation of 1,906 feet (581 metres) near Népen Diakha; and a large but shallow landmass lying between Cape Verde to the west and the edges of the massif to the east. Washed by the Canary Current, the Atlantic coast of Senegal is sandy and surf-beaten. Like the rest of the country, it is low except for the Cape Verde Peninsula, which shelters Dakar, one of the finest ports in Africa. The surf is less heavy on the coast south of the peninsula, whereas the coast south of the Saloum River consists of rias (drowned valleys) and is increasingly fringed with mangroves. More … Score: https://www.britannica.com/place/Senegal/Land  

2026/04/04

Senegal is beautiful and well organized

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2026/04/03

Beautiful Bangladesh

Bangladesh, a tourist attraction in south-central Asia with the world's largest beaches, historical monuments, resorts, picnic spots, forests and tribal ..

2026/03/28

Visit Greece

If you are looking for travel inspiration, visitgreece.gr has everything you need to know. Travel ideas, Events, guides, what to do, where to go in Greece.

2026/03/27

Bangladesh Independence Day

Bangladesh, country of South Asia, located in the delta of the Padma (Ganges [Ganga]) and Jamuna (Brahmaputra) rivers in the northeastern part of the Indian subcontinent. The riverine country of Bangladesh (“Land of the Bengals”) is one of the most densely populated countries in the world, and its people are predominantly Muslim. As the eastern portion of the historical region of Bengal, the area once formed, along with what is now the Indian state of West Bengal, the province of Bengal in British India. With the partition of India in 1947, it became the Pakistani province of East Bengal (later renamed East Pakistan), one of five provinces of Pakistan, separated from the other four by 1,100 miles (1,800 km) of Indian territory. In 1971 it became the independent country of Bangladesh, with its capital at Dhaka. Land Bangladesh is bordered by the Indian states of West Bengal to the west and north, Assam to the north, Meghalaya to the north and northeast, and Tripura and Mizoram to the east. To the southeast, it shares a boundary with Myanmar (Burma). The southern part of Bangladesh opens into the Bay of Bengal. Relief Stretching northward from the Bay of Bengal, Bangladesh constitutes roughly the eastern two-thirds of the deltaic plain of the Padma (Ganges [Ganga]) and Jamuna (Brahmaputra) rivers. Except for small higher areas of jungle-covered old alluvium (rising to about 100 feet [30 metres]) in the northwest and north-centre—in the Barind and the Madhupur Tract, respectively—the plain is a flat surface of recent alluvium, having a gentle slope and an elevation of generally less than 30 feet (9 metres) above sea level. In the northeast and southeast—in the Sylhet and Chittagong Hills areas, respectively—the alluvial plains give place to ridges, running mainly north-south, that form part of the mountains that separate Bangladesh from Myanmar and India. In its southern region, Bangladesh is fringed by the Sundarbans, a huge expanse of marshy deltaic forest. The Barind is a somewhat elevated triangular wedge of land that lies between the floodplains of the upper Padma and Jamuna rivers in northwestern Bangladesh. A depression called the Bhar Basin extends southeast from the Barind for about 100 miles (160 km) to the confluence of the Padma and Jamuna. This area is inundated during the summer monsoon season, in some places to a depth exceeding 10 feet (3 metres). The drainage of the western part of the basin is centred in the vast marshy area called the Chalan wetlands, also known as Chalan Lake. The floodplains of the Jamuna, which lie north of the Bhar Basin and east of the Barind, stretch from the border with Assam in the north to the confluence of the Padma and Jamuna in the south. The area is dominated by the Jamuna, which frequently overflows its banks in devastating floods. South of the Bhar Basin is the floodplain of the lower Padma. In north-central Bangladesh, east of the Jamuna floodplains, is the Madhupur Tract. It consists of an elevated plateau on which hillocks ranging in height from 30 to 60 feet (9 to 18 metres) give contour to cultivated valleys. The Madhupur Tract contains sal trees, whose hardwood is comparable in value and utility to teak. East of the Madhupur Tract, in northeastern Bangladesh, is a region called the Northeastern Lowland. It encompasses the southern and southwestern parts of the Sylhet area (including the valley plain of the Surma River) and the northern part of the Mymensingh area and has a large number of lakes. The Sylhet Hills in the far northeast of the region consist of a number of hillocks and hills ranging in elevation from about 100 feet (30 metres) to more than 1,100 feet (330 metres). In east-central Bangladesh the Brahmaputra River in its old course (the Old Brahmaputra River) built up the flood basin of the Meghna River, the region that includes the low and fertile Meghna-Sitalakhya Doab (the land area between those rivers). This area is enriched by the Titas distributary, and land areas are formed and changed by the deposition of silt and sand in the riverbeds of the Meghna River, especially between Bhairab Bazar and Daudkandi. Dhaka is located in this region. In southern Bangladesh the Central Delta Basins include the extensive lakes in the central part of the Bengal Delta, to the south of the upper Padma. The basin’s total area is about 1,200 square miles (3,100 square km). The belt of land in southwestern Bangladesh bordering the Bay of Bengal constitutes the Immature Delta. A lowland of some 3,000 square miles (7,800 square km), the belt contains, in addition to the vast mangrove forest known as the Sundarbans, the reclaimed and cultivated lands to the north of it. The area nearest the Bay of Bengal is crisscrossed by a network of streams that flow around roughly oblong islands. The Active Delta, located north of the Central Delta Basins and east of the Immature Delta, includes the Dhaleswari-Padma Doab and the estuarine islands of varying sizes that are found from the Pusur River in the southwest to the island of Sandwip near Chittagong in the southeast. Lying to the south of the Feni River in southeastern Bangladesh is the Chittagong region, which has many hills, hillocks, valleys, and forests and is quite different in aspect from other parts of the country. The coastal plain is partly sandy and partly composed of saline clay; it extends southward from the Feni River to the town of Cox’s Bazar and varies in width from 1 to 10 miles (1.6 to 16 km). The region has a number of offshore islands and one coral reef, St. Martin’s, off the coast of Myanmar. The hilly area known as the Chittagong Hill Tracts, in the far southeast, consists of low hills of soft rocks, mainly clay and shale. The north-south ranges are generally below 2,000 feet (600 metres) in elevation. More … Score: https://www.britannica.com/place/Bangladesh

2026/03/26

Independence Day Greek Republic

Greece, the southernmost of the countries of the Balkan Peninsula. Geography has greatly influenced the country’s development. Mountains historically restricted internal communications, but the sea opened up wider horizons. The total land area of Greece (one-fifth of which is made up of the Greek islands) is comparable in size to England or the U.S. state of Alabama. Greece has more than 2,000 islands, of which about 170 are inhabited; some of the easternmost Aegean islands lie just a few miles off the Turkish coast. The country’s capital is Athens, which expanded rapidly in the second half of the 20th century. Attikí (ancient Greek: Attica), the area around the capital, is now home to about one-third of the country’s entire population. A Greek legend has it that God distributed soil through a sieve and used the stones that remained to build Greece. The country’s barren landscape historically caused the people to migrate. The Greeks, like the Jews and the Armenians, traditionally have been a people of diaspora, and several million people of Greek descent live in various parts of the world. Xeniteia, or sojourning in foreign lands, with its strong overtones of nostalgia for the faraway homeland, has been a central element in the historical experience of the Greek people. Greece is a country that is at once European, Balkan, Mediterranean, and Near Eastern. It lies at the juncture of Europe, Asia, and Africa and is heir to the heritages of Classical Greece, the Byzantine Empire, and nearly four centuries of Ottoman Turkish rule. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe Now Land Greece is bordered to the east by the Aegean Sea, to the south by the Mediterranean Sea, and to the west by the Ionian Sea. Only to the north and northeast does it have land borders (totaling some 735 miles [1,180 km]), with, from west to east, Albania, the Republic of North Macedonia (see Researcher’s Note: Macedonia: the provenance of the name), Bulgaria, and Turkey. The Greek landscape is conspicuous not only for its rugged beauty but also for its complexity and variety. Three elements dominate: the sea, the mountains, and the lowland. The Greek mainland is sharply indented; arms and inlets of the sea penetrate so deeply that only a small, wedge-shaped portion of the interior is more than 50 miles (80 km) from the coast. The rocky headlands and peninsulas extend outward to the sea where there are many island arcs and archipelagoes. The southernmost part of mainland Greece, the Pelopónnisos (ancient Greek: Peloponnese) peninsula, connects to the mainland only by the narrow isthmus at the head of the Gulf of Korinthiakós (Corinth). Greece’s mountainous terrain covers some four-fifths of the country, much of which is deeply dissected. A series of mainland mountain chains running northwest-southeast enclose narrow parallel valleys and numerous small basins that once held lakes. With riverine plains and thin, discontinuous strips of coastal plain, these interior valleys and basins constitute the lowland. Although it accounts for only about one-fifth of the country’s land area, the lowland has played an important role in the life of the country. Relief Three characteristics of geology and structure underlie these landscape elements. First, northeastern Greece is occupied by a stable block of ancient (Hercynian) hard rock. Second, younger and weaker rocks, the majority of which are of limestone origin, make up western and southern Greece. These were heavily folded during the Alp-building phase of the Paleogene and Neogene periods (about 66 to 2.6 million years ago), when Earth movements thrust the softer sediments east-northeast against the unyielding Hercynian block and produced a series of roughly parallel tectonic zones that gave rise to the mountain-and-valley relief. Third, both the Hercynian block and the Hellenidic (Alpine) ranges were subsequently raised and fractured by tectonic movements. These dislocations created the sunken basins of the Ionian and Aegean seas as well as the jagged edges so typical of Greece’s landscape. Earthquakes are frequent reminders that similar earth movements continue, particularly along the major fault lines. One result of the region’s geologic instability is the widespread presence of marble, which is limestone that has been altered by pressure and heat. Seismic disturbances are sometimes associated with volcanic explosions, especially those involving the island of Thíra (ancient Greek: Thera; also called Santoríni), which was virtually destroyed by a major eruption in the 2nd millennium bce. The vents of the Kaméni islands in the sea-filled explosion crater of Thíra remain active. The island of Mílos (Melos), which rises to 2,465 feet (751 metres) above sea level, is composed of young volcanic rocks. Relief and geology provide the basis for describing the Greek landscape in terms of six major regions: central, northeastern, eastern, southern, and western mainland Greece, along with the islands. More … Score: https://www.britannica.com/place/Greece

2026/03/25