Independence Day of Georgia

Georgia, Georgian Sakartvelo, country of Transcaucasia located at the eastern end of the Black Sea on the southern flanks of the main crest of the Greater Caucasus Mountains. It is bounded on the north and northeast by Russia, on the east and southeast by Azerbaijan, on the south by Armenia and Turkey, and on the west by the Black Sea. Georgia includes three ethnic enclaves: Abkhazia, in the northwest (principal city Sokhumi); Ajaria, in the southwest (principal city Batʿumi); and South Ossetia, in the north (principal city Tskhinvali). The capital of Georgia is Tbilisi (Tiflis). The roots of the Georgian people extend deep in history; their cultural heritage is equally ancient and rich. During the medieval period a powerful Georgian kingdom existed, reaching its height between the 10th and 13th centuries. After a long period of Turkish and Persian domination, Georgia was annexed by the Russian Empire in the 19th century. An independent Georgian state existed from 1918 to 1921, when it was incorporated into the Soviet Union. In 1936 Georgia became a constituent (union) republic and continued as such until the collapse of the Soviet Union. During the Soviet period the Georgian economy was modernized and diversified. One of the most independence-minded republics, Georgia declared sovereignty on November 19, 1989, and independence on April 9, 1991. The 1990s were a period of instability and civil unrest in Georgia, as the first postindependence government was overthrown and separatist movements emerged in South Ossetia and Abkhazia. Land - Relief, drainage, and soils With the notable exception of the fertile plain of the Kolkhida Lowland—ancient Colchis, where the legendary Argonauts sought the Golden Fleece—the Georgian terrain is largely mountainous, and more than a third is covered by forest or brushwood. There is a remarkable variety of landscape, ranging from the subtropical Black Sea shores to the ice and snow of the crest line of the Caucasus. Such contrasts are made more noteworthy by the country’s relatively small area. The rugged Georgia terrain may be divided into three bands, all running from east to west. To the north lies the wall of the Greater Caucasus range, consisting of a series of parallel and transverse mountain belts rising eastward and often separated by deep, wild gorges. Spectacular crest-line peaks include those of Mount Shkhara, which at 16,627 feet (5,068 metres) is the highest point in Georgia, and Mounts Rustaveli, Tetnuld, and Ushba, all of which are above 15,000 feet. The cone of the extinct Mkinvari (Kazbek) volcano dominates the northernmost Bokovoy range from a height of 16,512 feet. A number of important spurs extend in a southward direction from the central range, including those of the Lomis and Kartli (Kartalinian) ranges at right angles to the general Caucasian trend. From the ice-clad flanks of these desolately beautiful high regions flow many streams and rivers. The southern slopes of the Greater Caucasus merge into a second band, consisting of central lowlands formed on a great structural depression. The Kolkhida Lowland, near the shores of the Black Sea, is covered by a thick layer of river-borne deposits accumulated over thousands of years. Rushing down from the Greater Caucasus, the major rivers of western Georgia, the Inguri, Rioni, and Kodori, flow over a broad area to the sea. The Kolkhida Lowland was formerly an almost continually stagnant swamp. In a great development program, drainage canals and embankments along the rivers were constructed and afforestation plans introduced; the region has become of prime importance through the cultivation of subtropical and other commercial crops. To the east the structural trough is crossed by the Meskhet and Likh ranges, linking the Greater and Lesser Caucasus and marking the watershed between the basins of the Black and Caspian seas. In central Georgia, between the cities of Khashuri and Mtsʿkhetʿa (the ancient capital), lies the inner high plateau known as the Kartli (Kartalinian) Plain. Surrounded by mountains to the north, south, east, and west and covered for the most part by deposits of the loess type, this plateau extends along the Kura (Mtkvari) River and its tributaries. The southern band of Georgian territory is marked by the ranges and plateaus of the Lesser Caucasus, which rise beyond a narrow, swampy coastal plain to reach 10,830 feet in the peak of Didi-Abuli. A variety of soils are found in Georgia, ranging from gray-brown and saline semidesert types to richer red earths and podzols. Artificial improvements add to the diversity. Climate The Caucasian barrier protects Georgia from cold air intrusions from the north, while the country is open to the constant influence of warm, moist air from the Black Sea. Western Georgia has a humid subtropical, maritime climate, while eastern Georgia has a range of climate varying from moderately humid to a dry subtropical type. There also are marked elevation zones. The Kolkhida Lowland, for example, has a subtropical character up to about 1,600 to 2,000 feet, with a zone of moist, moderately warm climate lying just above; still higher is a belt of cold, wet winters and cool summers. Above about 6,600 to 7,200 feet there is an alpine climatic zone, lacking any true summer; above 11,200 to 11,500 feet snow and ice are present year-round. In eastern Georgia, farther inland, temperatures are lower than in the western portions at the same altitude. Western Georgia has heavy rainfall throughout the year, totaling 40 to 100 inches (1,000 to 2,500 mm) and reaching a maximum in autumn and winter. Southern Kolkhida receives the most rain, and humidity decreases to the north and east. Winter in this region is mild and warm; in regions below about 2,000 to 2,300 feet, the mean January temperature never falls below 32 °F (0 °C), and relatively warm, sunny winter weather persists in the coastal regions, where temperatures average about 41 °F (5 °C). Summer temperatures average about 71 °F (22 °C). In eastern Georgia, precipitation decreases with distance from the sea, reaching 16 to 28 inches in the plains and foothills but increasing to double this amount in the mountains. The southeastern regions are the driest areas, and winter is the driest season; the rainfall maximum occurs at the end of spring. The highest lowland temperatures occur in July (about 77 °F [25 °C]), while average January temperatures over most of the region range from 32 to 37 °F (0 to 3 °C). More … Score: https://www.britannica.com/place/Georgia

2025/05/26

About Visit Eritrea

Website aimed at presenting Eritrea to everyone interested to visit, discover and get to know the real Eritrea.

2025/05/26

Interesting Facts About Georgia

Georgia is a new travel destination on the world map. Come and see for yourself.

2025/05/25

Independence Day of the Hashemite Kingdom of Jordan

Jordan is a young state that occupies an ancient land, one that bears the traces of many civilizations. Separated from ancient Palestine by the Jordan River, the region played a prominent role in biblical history. The ancient biblical kingdoms of Moab, Gilead, and Edom lie within its borders, as does the famed red stone city of Petra, the capital of the Nabatean kingdom and of the Roman province of Arabia Petraea. British traveler Gertrude Bell said of Petra, “It is like a fairy tale city, all pink and wonderful.” Part of the Ottoman Empire until 1918 and later a mandate of the United Kingdom, Jordan has been an independent kingdom since 1946. It is among the most politically liberal countries of the Arab world, and, although it shares in the troubles affecting the region, its rulers have expressed a commitment to maintaining peace and stability. The capital and largest city in the country is Amman—named for the Ammonites, who made the city their capital in the 13th century bce. Amman was later a great city of Middle Eastern antiquity, Philadelphia, of the Roman Decapolis, and now serves as one of the region’s principal commercial and transportation centres as well as one of the Arab world’s major cultural capitals. Land Slightly smaller in area than the country of Portugal, Jordan is bounded to the north by Syria, to the east by Iraq, to the southeast and south by Saudi Arabia, and to the west by Israel and the West Bank. The West Bank area (so named because it lies just west of the Jordan River) was under Jordanian rule from 1948 to 1967, but in 1988 Jordan renounced its claims to the area. Jordan has 16 miles (26 km) of coastline on the Gulf of Aqaba in the southwest, where Al-ʿAqabah, its only port, is located. Relief Jordan has three major physiographic regions (from east to west): the desert, the uplands east of the Jordan River, and the Jordan Valley (the northwest portion of the great East African Rift System). The desert region is mostly within the Syrian Desert—an extension of the Arabian Desert—and occupies the eastern and southern parts of the country, comprising more than four-fifths of its territory. The desert’s northern part is composed of volcanic lava and basalt, and its southern part of outcrops of sandstone and granite. The landscape is much eroded, primarily by wind. The uplands east of the Jordan River, an escarpment overlooking the rift valley, have an average elevation of 2,000–3,000 feet (600–900 metres) and rise to about 5,755 feet (1,754 metres) at Mount Ramm, Jordan’s highest point, in the south. Outcrops of sandstone, chalk, limestone, and flint extend to the extreme south, where igneous rocks predominate. The Jordan Valley drops to about 1,410 feet (430 metres) below sea level at the Dead Sea, the lowest natural point on Earth’s surface. Drainage The Jordan River, approximately 186 miles (300 km) in length, meanders south, draining the waters of Lake Tiberias (better known as the Sea of Galilee), the Yarmūk River, and the valley streams of both plateaus into the Dead Sea, which occupies the central area of the valley. The soil of its lower reaches is highly saline, and the shores of the Dead Sea consist of salt marshes that do not support vegetation. To its south, Wadi al-ʿArabah (also called Wadi al-Jayb), a completely desolate region, is thought to contain mineral resources. In the northern uplands several valleys containing perennial streams run west; around Al-Karak they flow west, east, and north; south of Al-Karak intermittent valley streams run east toward Al-Jafr Depression. Soils The country’s best soils are found in the Jordan Valley and in the area southeast of the Dead Sea. The topsoil in both regions consists of alluvium—deposited by the Jordan River and washed from the uplands, respectively—with the soil in the valley generally being deposited in fans spread over various grades of marl. …. Climate of Jordan Jordan’s climate varies from Mediterranean in the west to desert in the east and south, but the land is generally arid. The proximity of the Mediterranean Sea is the major influence on climates, although continental air masses and elevation also modify it. Average monthly temperatures at Amman in the north range between 46 and 78 °F (8 and 26 °C), while at Al-ʿAqabah in the far south they range between 60 and 91 °F (16 and 33 °C). The prevailing winds throughout the country are westerly to southwesterly, but spells of hot, dry, dusty winds blowing from the southeast off the Arabian Peninsula frequently occur and bring the country its most uncomfortable weather. Known locally as the khamsin, these winds blow most often in the early and late summer and can last for several days at a time before terminating abruptly as the wind direction changes and much cooler air follows. Precipitation occurs in the short, cool winters, decreasing from 16 inches (400 mm) annually in the northwest near the Jordan River to less than 4 inches (100 mm) in the south. In the uplands east of the Jordan River, the annual total is about 14 inches (355 mm). The valley itself has a yearly average of 8 inches (200 mm), and the desert regions receive one-fourth of that. Occasional snow and frost occur in the uplands but are rare in the rift valley. As the population increases, water shortages in the major towns are becoming one of Jordan’s crucial problems. More …. Score: https://www.britannica.com/place/Jordan

2025/05/25

Patriotic Revolution Day Argentine Republic

Argentina, country of South America, covering most of the southern portion of the continent. The world’s eighth largest country, Argentina occupies an area more extensive than Mexico and the U.S. state of Texas combined. It encompasses immense plains, deserts, tundra, and forests, as well as tall mountains, rivers, and thousands of miles of ocean shoreline. Argentina also claims a portion of Antarctica, as well as several islands in the South Atlantic, including the British-ruled Falkland Islands (Islas Malvinas). Argentina has long played an important role in the continent’s history. Following three centuries of Spanish colonization, Argentina declared independence in 1816, and Argentine nationalists were instrumental in revolutionary movements elsewhere, a fact that prompted 20th-century writer Jorge Luis Borges to observe, “South America’s independence was, to a great extent, an Argentine enterprise.” Torn by strife and occasional war between political factions demanding either central authority (based in Buenos Aires) or provincial autonomy, Argentina tended toward periods of caudillo, or strongman, leadership, most famously under the presidency of Juan Perón. The 1970s ushered in a period of military dictatorship and repression during which thousands of presumed dissidents were “disappeared,” or murdered; this ended in the disastrous Falklands Islands War of 1982, when Argentina invaded the South Atlantic islands it claimed as its own and was defeated by British forces in a short but bloody campaign. Defeat led to the fall of the military regime and the reestablishment of democratic rule, which has since endured despite various economic crises. The country’s name comes from the Latin word for silver, argentum, and Argentina is indeed a great source of valuable minerals. More important, however, has been Argentina’s production of livestock and cereals, for which it once ranked among the world’s wealthiest nations. Much of this agricultural activity is set in the Pampas, rich grasslands that were once the domain of nomadic Native Americans, followed by rough-riding gauchos, who were in turn forever enshrined in the nation’s romantic literature. As Borges describes them in his story The South, the Pampas stretch endlessly to the horizon, dwarfing the humans within them; traveling from the capital toward Patagonia, the story’s protagonist, Señor Dahlmann, “saw horsemen along dirt roads; he saw gullies and lagoons and ranches; he saw long luminous clouds that resembled marble; and all these things were casual, like dreams of the plain.... The elemental earth was not perturbed either by settlements or other signs of humanity. The country was vast, but at the same time it was intimate and, in some measure, secret. The limitless country sometimes contained only a solitary bull. The solitude was perfect and perhaps hostile, and it might have occurred to Dahlmann that he was traveling into the past and not merely south.” Despite the romantic lure of the Pampas and of vast, arid Patagonian landscapes, Argentina is a largely urban country. Buenos Aires, the national capital, has sprawled across the eastern Pampas with its ring of modern, bustling suburbs. It is among South America’s most cosmopolitan and crowded cities and is often likened to Paris or Rome for its architectural styles and lively nightlife. Its industries have drawn colonists from Italy, Spain, and numerous other countries, millions of whom immigrated in the late 19th and early 20th centuries. Greater Buenos Aires is home to about one-third of the Argentine people. Among the country’s other major cities are Mar del Plata, La Plata, and Bahía Blanca on the Atlantic coast and Rosario, San Miguel de Tucumán, Córdoba, and Neuquén in the interior. Land Argentina is shaped like an inverted triangle with its base at the top; it is some 880 miles (1,420 km) across at its widest from east to west and stretches 2,360 miles (3,800 km) from the subtropical north to the subantarctic south. The country is bounded by Chile to the south and west, Bolivia and Paraguay to the north, and Brazil, Uruguay, and the Atlantic Ocean to the east. Its undulating Atlantic coastline stretches some 2,900 miles (4,700 km). Argentina’s varied geography can be grouped into four major regions: the Andes, the North, the Pampas, and Patagonia. The Andean region extends some 2,300 miles (3,700 km) along the western edge of the country from Bolivia to southern Patagonia, forming most of the natural boundary with Chile. It is commonly subdivided into two parts: the Northwest and the Patagonian Andes, the latter of which is discussed below under Patagonia. The North is commonly described in terms of its two main divisions: the Gran Chaco, or Chaco, comprising the dry lowlands between the Andes and the Paraná River; and Mesopotamia, an area between the Paraná and Uruguay rivers. The centrally located plains, or Pampas, are grasslands subdivided into arid western and more humid eastern parts called, respectively, the Dry Pampa and the Humid Pampa. Patagonia is the cold, parched, windy region that extends some 1,200 miles (1,900 km) south of the Pampas, from the Colorado River to Tierra del Fuego. Relief - The Northwest This part of the Andes region includes the northern half of the main mountain mass in Argentina and the transitional terrain, or piedmont, merging with the eastern lowlands. The region’s southern border is the upper Colorado River. Within the region the Andean system of north-south–trending mountain ranges varies in elevation from 16,000 to 22,000 feet (4,900 to 6,700 metres) and is interrupted by high plateaus (punas) and basins ranging in elevation from about 10,000 to 13,400 feet (3,000 to 4,080 metres). The mountains gradually decrease in size and elevation southward from Bolivia. South America’s highest mountain, Aconcagua (22,831 feet [6,959 metres]), lies in the Northwest, together with a number of other peaks that reach over 21,000 feet (6,400 metres). Some of these mountains are volcanic in origin. To the southeast, where the parallel to subparallel ranges become lower and form isolated, compact units trending north-south, the flat valleys between are called bolsones (basins). This southeastern section of the Northwest is often called the Pampean Sierras, a complex that has been compared to the Basin and Range region of the western United States. It is characterized by west-facing escarpments and gentler east-facing backslopes, particularly those of the spectacular Sierra de Córdoba. The Pampean Sierras have variable elevations, beginning at 2,300 feet (700 metres) in the Sierra de Mogotes in the east and rising to 20,500 feet (6,250 metres) in the Sierra de Famatina in the west. only in the extreme south, where there are now large moraines. More … Score https://www.britannica.com/place/Argentina

2025/05/25

Welcome to Jordan!

Welcome to Jordan! Explore the awe-inspiring sites that Jordan has to offer through this illuminating video. Thanks to Columbia Omniten for making footage for this video possible.

2025/05/24

Independence Day of the State of Eritrea

Eritrea, country of the Horn of Africa, located on the Red Sea. Eritrea’s coastal location has long been important in its history and culture—a fact reflected in its name, which is an Italianized version of Mare Erythraeum, Latin for “Red Sea.” The Red Sea was the route by which Christianity and Islam reached the area, and it was an important trade route that such powers as Turkey, Egypt, and Italy hoped to dominate by seizing control of ports on the Eritrean coast. Those ports promised access to the gold, coffee, and slaves sold by traders in the Ethiopian highlands to the south, and, in the second half of the 20th century, Ethiopia became the power from which the Eritrean people had to free themselves in order to create their own state. In 1993, after a war of independence that lasted nearly three decades, Eritrea became a sovereign country. During the long struggle, the people of Eritrea managed to forge a common national consciousness, but, with peace established, they faced the task of overcoming their ethnic and religious differences in order to raise the country from a poverty made worse by years of drought, neglect, and war. Eritrea’s capital and largest city is Asmara (Asmera). Land Eritrea’s coastline, forming the northeastern edge of the country, extends for roughly 600 miles (1,000 km) from Cape Kasar, in the north, to the Strait of Mandeb, separating the Red Sea from the Gulf of Aden in the south. The country is bounded to the southeast by Djibouti, to the south by Ethiopia, and to the west by Sudan. Relief Eritrea’s land is highly variegated. Running on a north-south axis through the middle of the country are the central highlands, a narrow strip of country some 6,500 feet (2,000 metres) above sea level that represents the northern reaches of the Ethiopian Plateau. The highest point is Mount Soira, at 9,885 feet (3,013 metres). Geologically, the plateau consists of a foundation of crystalline rock (e.g., granite, gneiss, and mica schist) that is overlain by sedimentary rock (limestone and sandstone) and capped by basalt (rock of volcanic origin). The upper layers have been highly dissected by deep gorges and river channels, forming small, steep-sided, flat-topped tablelands known as ambas. Encouraged by the steady expansion of cultivation, soil erosion on the plateau has left few wooded areas. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe Now In the north of Eritrea the highlands narrow and then end in a system of hills, where erosion has cut down to the basement rock. To the east the plateau drops abruptly into a coastal plain. North of the Gulf of Zula, the plain is only 10 to 50 miles (15 to 80 km) wide, but to the south it widens to include the Danakil Plain. This barren region contains a depression known as the Kobar Sink (more than 300 feet [90 metres] below sea level), the northern end of which extends into Eritrea. The coastal plain and the Danakil Plain are part of the East African Rift System and are sharply delimited on the west by the eastern escarpment of the plateau, which, although deeply eroded, presents a formidable obstacle to travelers from the coast. The western flank of the central highlands is a broken and undulating plain that slopes gradually toward the border with Sudan. It lies at an average elevation of 1,500 feet (460 metres). The vegetation is mostly savanna, consisting of scattered trees, shrubs, and seasonal grasses. Off the coast in the Red Sea is the Dahlak Archipelago, a group of more than 100 small coral and reef-fringed islands. Only a few of these islands have a permanent population. Drainage The Eritrean highlands are drained by four major rivers and numerous streams. Two of the rivers, the Gash and the Tekezē, flow westward into Sudan. The Tekezē River (also known as the Satit) is a major tributary of the Atbara River, which eventually joins the Nile. The Gash River reaches the Atbara only during flood season. As it crosses the western lowlands, the Tekezē forms part of Eritrea’s border with Ethiopia, while the upper course of the Gash, known as the Mereb River, forms the border on the plateau. The other two major rivers that drain the highlands of Eritrea are the Baraka and the Anseba. Both of these rivers flow northward into a marshy area on the eastern coast of Sudan and do not reach the Red Sea. Several seasonal streams that flow eastward from the plateau reach the sea on the Eritrean coast. Climate Eritrea has a wide variety of climatic conditions, produced mainly by differences in elevation. The effects of elevation are seen most clearly in the wide range of temperatures experienced throughout the country. On the coast, Massawa (Mitsiwa) has one of the highest averages in the world (the mid-80s F [about 30 °C]), while Asmara, only 40 miles (65 km) away yet roughly 7,500 feet (2,300 metres) higher on the plateau, averages in the low 60s F (about 17 °C). Mean annual rainfall on the plateau is about 16 to 20 inches (400 to 500 mm), while on the western plain it is less than 16 inches. In both the highlands and the western lowlands, rainfall comes in summer, carried on a southwesterly airstream. Toward the northeastern extremes of the plateau, the amount of precipitation decreases, and the length of the rainy season becomes shorter. The eastern edges of the plateau and, to a lesser extent, the coastal fringes receive much smaller quantities of rain from a northeasterly airstream that arrives in winter and spring. The interior regions of the Danakil Plain are practically rainless. People - Ethnic groups and languages Eritrea’s population consists of several ethnic groups, each with its own language and cultural tradition. In addition to the languages spoken by the various ethnic groups, Arabic and English are widely understood. Italian is occasionally used as well. The bulk of the people in the Eritrean highlands are Tigray. In Eritrea that group is sometimes called Tigrinya, though linguists of Semitic languages note that -nya is an Amharic suffix meaning “language of.” In any case, proper nomenclature for the people is fluid, given contemporary political sensitivities. The Tigray make up about half the country’s total population. They also occupy the adjacent Ethiopian region of Tigray. The Tigrinya language is one of two major indigenous languages in Eritrea. Inhabiting the northernmost part of the Eritrean plateau, as well as lowlands to the east and west, are the Tigre people. The Tigre, who constitute nearly one-third of Eritrea’s population, speak the other major Eritrean language—Tigré. Tigré and Tigrinya are written in the same script and are both related to the ancient Semitic Geʿez language, but they are mutually unintelligible. Also occupying the northern plateau are Bilin speakers, whose language belongs to the Cushitic family. The Rashaida are a group of Arabic-speaking nomads who traverse the northern hills. On the southern part of the coastal region live Afar nomads. The Afars—who also live across the borders in Djibouti and Ethiopia—are known to surrounding peoples as the Danakil, after the region that they inhabit. The coastal strip south of Massawa, as well as the eastern flanks of the plateau, are occupied by Saho pastoralists. In the western plain the dominant people are Beja pastoralists; Beja also live across the border in Sudan. Two small groups speaking Nilotic languages, the Kunama and the Nara, also live in the west. More … Score: https://www.britannica.com/place/Eritrea

2025/05/24

Yemen Tourism Promotion Board - Home

Sana'a - Tourism Media : The Ministry of Tourism and the Tourism Promotion Council... Read more ... Executive Director of the Tourism Promotion Council: The ...

2025/05/24

Argentina "Official Video"

2025/05/24