Anniversary of the Proclamation of the Azerbaijani Republic

Azerbaijan, also spelled Azerbaidzhan, officially Azerbaijani Republic, Azerbaijani Azärbayjan Respublikasi, country of eastern Transcaucasia. Occupying an area that fringes the southern flanks of the Caucasus Mountains, it is bounded on the north by Russia, on the east by the Caspian Sea, on the south by Iran, on the west by Armenia, and on the northwest by Georgia. The exclave of Naxçıvan (Nakhichevan) is located southwest of Azerbaijan proper, bounded by Armenia, Iran, and Turkey. Azerbaijan includes within its borders the predominantly Armenian enclave of Nagorno-Karabakh, which from 1988 was the focus of intense conflict between Azerbaijan and Armenia. The capital of Azerbaijan is the ancient city of Baku (Bakı), whose harbour is the best on the Caspian Sea. In addition to its variegated and often beautiful terrain, Azerbaijan offers a blend of traditions and modern development. The people of its remoter areas retain many distinctive folk traditions, but the lives of its inhabitants have been much influenced by accelerating modernization, characterized by industrialization, the development of power resources, and the growth of the cities, in which more than half the people now live. Industry dominates the economy, and more-diversified pursuits have supplemented the exploitation of oil, of which Azerbaijan was the world’s leading producer at the beginning of the 20th century. Fine horses and caviar continue as some of the more distinctive traditional exports of the republic. Azerbaijan was an independent nation from 1918 to 1920 but was then incorporated into the Soviet Union. It became a constituent (union) republic in 1936. Azerbaijan declared sovereignty on September 23, 1989, and independence on August 30, 1991. Land - Relief, drainage, and soils As a result of its broken relief, drainage patterns, climatic differences, and sharply defined altitudinal zoning of vegetation, Azerbaijan is characterized by a wide variety of landscapes. More than two-fifths of its territory is taken up by lowlands, about half lies at 1,300 to 4,900 feet (400 to 1,500 metres), and areas above 4,900 feet occupy a little more than one-tenth of the total area. The highest peaks are Bazardyuzyu (Bazardüzü; 14,652 feet [4,466 metres]), Shakhdag, and Tufan, all part of the Greater Caucasus range, the crest of which forms part of Azerbaijan’s northern boundary. Magnificent spurs and ridges, cut into by the deep gorges of mountain streams, make this part of Azerbaijan a region of great natural beauty. At the same time, it lies within a region characterized by a high degree of seismic activity. The spurs of the Lesser Caucasus, in southwestern Azerbaijan, form the second important mountain system, which includes the Shakhdag, Murovdag, and Zangezur ranges, their summits rising to nearly 13,000 feet, and also the Karabakh Upland. The large and scenic Lake Geygyol lies at an altitude of 5,138 feet. The southeastern part of Azerbaijan is bordered by the Talish (Talysh) Mountains, consisting of three longitudinal ranges, with Mount Kyumyurkyoy as the highest peak (8,176 feet), and the Länkäran Lowland, along the Caspian coast. This lowland, an extension of the Kura-Aras Lowland, reaches the Iranian border near Astara. The Kura-Aras Lowland is named for the main river, the Kura (Kür), and its tributary the Aras (Araz). The Shirvan, Milskaya, and Mugan plains are part of this lowland and have similar soils and climate. Gray soils and saline solonchaks (aridisols) and, in higher regions, gray alkaline solonetz and chestnut soils (mollisols) prevail. A well-developed network of canals between the Kura and Aras rivers makes it possible to irrigate a major part of the lowland. The Upper Karabakh Canal, 107 miles (172 kilometres) long, provides a vital link between the Aras River and the Mingäçevir Reservoir on the Kura River. The reservoir has a surface area of 234 square miles and a maximum depth of 246 feet. The Upper Karabakh Canal alone irrigates more than 250,000 acres (100,000 hectares) of fertile land and in addition supplies the Aras River with water during dry summer periods. The Upper Shirvan Canal, the second most important canal, is 76 miles in length and also irrigates about 250,000 acres. Climate The dry subtropical climate of central and eastern Azerbaijan is characterized by a mild winter and a long (four to five months) and very hot summer, with temperatures averaging about 81 °F (27 °C) and maximum temperatures reaching 109 °F (43 °C). Southeastern Azerbaijan is characterized by a humid subtropical climate with the highest precipitation in the country, some 47 to 55 inches (1,200 to 1,400 millimetres) a year, most of it falling in the cold months. A dry continental climate, with a cold winter and a dry, hot summer, prevails in Naxçıvan at altitudes of 2,300 to 3,300 feet. Moderately warm, dry, or humid types of climate are to be found in other parts of Azerbaijan. The mountain forest zone has a moderately cold climate, while an upland tundra climate characterizes elevations of 10,000 feet and above. Frosts and heavy snowfalls make the passes at such altitudes inaccessible for three or four months of the year. Plant and animal life Natural vegetation zones vary according to altitude. Steppe and semidesert conditions prevail in the lowlands and the foothills of the mountain regions. The slopes of the mountains are covered with beech, oak, and pine forests. Higher up there is a zone of alpine meadows. The Länkäran region of southern Azerbaijan has evergreen vegetation and thick beech and oak forests. In the lowlands the animal life includes gazelles, jackals, and hyenas as well as reptile and rodent species. The mountain regions are inhabited by Caucasian deer, roe deer, wild boar, brown bear, lynx, European bison (wisent), chamois, and leopard, though the latter is rare. Mild winters draw many birds to the Caspian coast, and nature reserves provide a resting home for flamingos, swans, pelicans, herons, egrets, sandpipers, and partridges. More … Score: https://www.britannica.com/place/Azerbaijan

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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

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