Independence Day of the Kyrgyz Republic

Kyrgyzstan, country of Central Asia. It is bounded by Kazakhstan on the northwest and north, by China on the east and south, and by Tajikistan and Uzbekistan on the south and west. Most of Kyrgyzstan’s borders run along mountain crests. The capital is Bishkek (known from 1862 to 1926 as Pishpek and from 1926 to 1991 as Frunze). The Kyrgyz, a Muslim Turkic people, constitute nearly three-fourths of the population. The history of the Kyrgyz in what is now Kyrgyzstan dates at least to the 17th century. Kyrgyzstan, known under Russian and Soviet rule as Kirgiziya, was conquered by tsarist Russian forces in the 19th century. Formerly a constituent (union) republic of the U.S.S.R., Kyrgyzstan declared its independence on August 31, 1991. Land - Relief Kyrgyzstan is above all a mountainous country. At its eastern extremity, next to the Uighur Autonomous Region of Sinkiang, China, rises Victory (Pobedy) Peak, at 24,406 feet (7,439 metres) Kyrgyzstan’s highest peak. Mount Khan-Tengri (22,949 feet) is on the border with Kazakhstan. These mountains stand in the core of the Tien Shan system, which continues eastward into China. On the southern border lie the Kok Shaal-Tau, Alay, Trans-Alay (Zaalay), and Atbashi ranges. To the southwest are two great hollows, the Fergana Valley and another valley close to Mount Khan-Tengri. The latter valley is bounded by the westward-thrusting arms of the Kungey-Alatau and Terskey-Alatau ranges and contains Lake Ysyk (Issyk-Kul), whose clear deep waters are fed by the snow-covered peaks. The rugged mountain-and-basin structure of much of the country, and the high alpine plateau of the central and eastern regions, are separated from the Fergana Valley on the west by the Fergana Range, running southeast to northwest, which merges into the Chatkal Range. The Chatkal Range is linked to the Ysyk-Köl region by a final enclosing range, the Kyrgyz. The only other important lowlands in the country are the Chu and Talas river valleys in the north, with the capital, Bishkek, located in the Chu. The country’s lowland areas, though occupying only one-seventh of the total area, are home to most of its people. Drainage Snow and ice perpetually cover the crests of Kyrgyzstan’s high mountain ranges. The Naryn River, draining into the Fergana Valley, continues northwestward as a tributary of the Syr Darya. The Chu River runs parallel to and forms part of the northern boundary with Kazakhstan. Both the Chu and the Naryn are of major importance to the country. Climate Kyrgyzstan’s great distance from the oceans and the sharp change of elevation from adjacent plains strongly influence the country’s climate. Deserts and plains surround Kyrgyzstan on the north, west, and southeast, making the contrast with the climate and landscape of its mountainous interior all the more striking. The lower parts of its fringing ranges lie in belts of high temperature and receive hot, drying winds from the deserts beyond. The amount of precipitation the country’s westward- and northward-facing slopes receive increases with their height. The valleys have hot dry summers, with a mean July temperature of 82 °F (28 °C). In January the average temperature is −0.5 °F (−18 °C). Annual precipitation varies from 7 inches (180 mm) in the eastern Tien Shan to 30 to 40 inches (760 to 1,000 mm) in the Kyrgyz and Fergana ranges. In the most populous valleys, rainfall ranges from 4 to 20 inches (100 to 500 mm) a year. Plant and animal life Woodlands run along the lower valleys and on slopes of the north-facing ranges. These are coniferous forests, containing the striking Tien Shan white spruce and occupying 3 to 4 percent of the country’s area. The brown bear, wild pig, lynx, gray wolf, and ermine live in the woodlands. Wooded ravines and the valleys of the mountainous steppe regions provide the abode of the argali, a mountain sheep, along with mountain goats, deer, and snow leopards. In the desert, yellow gophers, jerboas, hares, and a large-eared hedgehog are typical. People of Kyrgyzstan - Ethnic groups The Kyrgyz, formerly a transhumant (nomadic) people, were settled into collectivized agriculture by the Soviet regime. Besides Kyrgyz, the country’s population includes minorities of Russians, Uzbeks, Ukrainians, and Germans (exiled to the region from European parts of the Soviet Union in 1941), as well as Tatars, Kazakhs, Dungans (Hui; Chinese Muslims), Uighurs, and Tajiks. Since independence in 1991, many Russians and Germans have emigrated. Nearly three-fourths of the population is Kyrgyz, while about one-seventh is Uzbek. The other ethnic groups make up the remaining one-eighth of the population. Languages Most Kyrgyz speak a language belonging to the northwestern group of the Turkic languages, especially Kyrgyz. A sizeable minority speak Uzbek, a Turkic language of the southeastern branch. Russian is also spoken, and official language status has been accorded to both Kyrgyz and Russian. Settlement patterns Between 1926 and 1989 the urban portion of the Kyrgyz population grew from almost nothing to more than one-fifth, though the Kyrgyz remained a minority in most cities and towns. During this period fewer than one-fourth of the inhabitants of the capital, Frunze (now Bishkek), were Kyrgyz; Slavs made up more than half of the city’s population. Southern Kyrgyzstan tends to be rural and Islamic, but the more-urbanized Western-oriented north has traditionally dominated the country. Only about one-third of the total population is urban, however, while nearly two-thirds is rural. Demographic trends The population of Kyrgyzstan is young. Over half the population is under age 30, while nearly one-third is under age 15. The death rate is slightly lower than the global average, and the birth rate is slightly above average. Life expectancy is about 75 years for women and 67 years for men. Economy The people of Kyrgyzstan have traditionally raised livestock and engaged in farming. By the late 20th century the republic had become a source for nonferrous metals, notably of antimony and mercury ores, and a producer of machinery, light industrial products, hydroelectric power, and food products. Gold mining has increased in importance, and Kyrgyzstan possesses substantial coal reserves and some petroleum and natural gas deposits. Hydroelectric power provides more than three-fourths of the country’s electric energy. More … Score: https://www.britannica.com/place/Kyrgyzstan

2023/08/31

LOST IN UZBEKISTAN 4K

From Tashkent, the capital of Uzbekistan, to the dreamy landscapes of Fergana Valley, from the jewels of Samarkand and Bukhara, a kaleidoscope of teeming squares and bazaars housed in the ancient caravanserais, to the fortress-city of Khiva, first among the historic sites of Uzbekistan to be recognized as a World Heritage Site by UNESCO, in 1990.

2023/08/31

Kyrgyz Republic video presentation in English

2023/08/30

Tourism | Republic Of Moldova

Although it has a small area, the Republic of Moldova as a tourist destination has a great potential represented first of all by the geomorphologic aspect of its territory – an unusual diversity of landscape reservations or scenery and unique geological monuments of European and world value.

2023/08/29

Independence Day of the Republic of Moldova

Moldova, country lying in the northeastern corner of the Balkan region of Europe. Its capital city is Chișinău, located in the south-central part of the country. Formerly known as Bessarabia, this region was an integral part of the Romanian principality of Moldavia until 1812, when it was ceded to Russia by its suzerain, the sultan of the Ottoman Empire. Bessarabia remained a province of the Russian Empire until after World War I, when it became a part of Greater Romania, and it reverted to Russian control in 1940–41 and again after World War II, when it was joined to a strip of formerly Ukrainian territory, the Moldavian Autonomous Soviet Socialist Republic, on the left bank of the Dniester River (Moldovan: Nistru) to form the Moldavian Soviet Socialist Republic. Upon the collapse of the Soviet Union in August 1991, this republic declared its independence and took the name Moldova. It became a member of the United Nations in 1992.Since its independence in 1991, Moldova has been beset with an array of challenges stemming from four problematic situations. First, the country has sought to establish a viable state where no tradition of self-government and sovereignty had existed before. Second, without a local political tradition, it was difficult for Moldova to agree on a constitution and to find political leaders untainted by association with the highly centralized, authoritarian Soviet Union. Third, the transition from a controlled economy to a free market economy has been rocky. A largely agricultural economy based on state and collective farms had been developed under Soviet rule. When many of these farms were broken up and turned over to individuals after independence, considerable dislocation, loss of productivity, and allegations of corruption resulted. Finally, the economic transition was further impeded by the fact that much of Moldovan industry was located in the separatist region of Transdniestria, which had proclaimed independence from Moldova in 1990, resulting in a brief civil war. Although a cease-fire was declared in 1992, relations remained tense between Moldova and Transdniestria, and Russian troops are still present in the security zone. Transdniestria is also the source of much of Moldova’s electricity, which has been cut off at various times. Thus, Moldova’s road to nationhood has remained bumpy—from the first efforts at nation-building to the country’s pursuit of peace and prosperity in the 21st century. Land Moldova is bounded by Ukraine to the north, east, and south and by Romania to the west. The bulk of the republic lies between the great meandering Prut and Dniester rivers. Relief Moldova lies to the east of the great arc of the Carpathian Mountains. It is underlain mostly by deep sedimentary rocks covering the southwestern portion of the ancient structural block known as the Russian, or East European, Plain. Harder crystalline rocks outcrop only in the north. Its surface is a hilly plain, with an average elevation of 482 feet (147 metres), cut by a deep network of river valleys, ravines, and gullies. The uplands of the centre of the republic, the Codri Hills, lie at an average elevation of about 1,150 to 1,300 feet (350 to 400 metres), and the highest point, Mount Bălănești, in the west, reaches 1,407 feet (429 metres). These uplands are interlaced by deep, flat valleys, ravines, and landslide-scoured depressions separated by sharp ridges. Steep forested slopes account for much of the terrain. The Dniester uplands, their eastern slopes forming the high right bank of the Dniester River, border the central uplands on the east and northeast. The northern landscape of Moldova is characterized by the level plain of the Bălți steppe (500 to 650 feet [150 to 200 metres] in elevation) and also by uplands averaging twice this elevation, culminating in Vysokaya Hill (1,053 feet [321 metres]). The northern uplands include the strikingly eroded Medobory-Toltry limestone ridges, which border the Prut River. In the south, the extensive Bugeac Plain is broken by numerous ravines and gullies, while, in the east, left-bank Moldova includes spurs of the Volyn-Podolsk Upland cut into by tributaries of the Dniester. Drainage Moldova has a well-developed network of rivers and streams, all draining south to the Black Sea, but only about one-tenth of these exceed 6 miles (10 km) in length, and even fewer exceed 60 miles (100 km). In fact, many of these are small, shallow streams that dry up during the summer. The Dniester, the rapidly flowing main artery, is navigable almost throughout the republic; the river becomes swollen by spring snowmelt from the Carpathians and by heavy summer rains. It does not freeze over during warmer winters. The other, smaller, main artery, the Prut, is a tributary of the Danube River, which it joins at the extreme southern tip of the country. The Ialpug, Cogâlnic, and other small southern rivers drain largely into the Danubian estuary in nearby Ukraine. Underground water, extensively used for the republic’s water supply, includes more than 2,000 natural springs. The terrain favours construction of reservoirs. Soils The soils of Moldova are varied and highly fertile, with chernozem—rich black soils—covering three-fourths of the republic. The best-developed chernozem, fostering the growth of grain, tobacco, and sugar beets, is found in the north and in the low-lying parts of the central and Dniester uplands, as well as in the left-bank regions. Soil quality diminishes southward, but grapes and sunflowers still can be grown. Brown and gray forest soils characterize the uplands: two-fifths are covered by forests, the rest by orchards, vineyards, and fields of grain. Alluvial soils characterize the floodplains, while the lower reaches of the Prut and southern river valleys have saline and marshland soils. In general, the excessive use of chemical fertilizers, pesticides, and herbicides during the Soviet period has resulted in significant contamination of the soil and groundwater. Climate Moldova’s climate—warm and moderately continental—is characterized by a lengthy frost-free period, a comparatively mild winter, considerable temperature fluctuations, and, in the south, extended droughts. The average annual temperature is in the mid-40s F (about 8 °C) in the north and the low 50s F (about 10 °C) in the south, but the July averages rise to the upper 60s and low 70s F (about 19 and 23 °C), respectively, and the mercury seldom drops below the low 20s F (about −3 °C) in January. Extreme lows near −30 °F (about −36 °C) in the north and excessive highs near 100 °F (about 41 °C) in the south have been recorded. Moldova receives highly variable amounts of precipitation—usually averaging about 20 inches (500 mm) annually, with totals a little lower in the south—but these figures conceal variations that may double the quantity in some years and result in prolonged dry spells in others. Most precipitation occurs as rain in the warmer months, and heavy summer showers, coupled with the irregular terrain, cause erosion problems and river silting. Winter snow cover is thin. Winds tend to come from either the northwest or the southeast. More … Score: https://www.britannica.com/place/Moldova  

2023/08/27

GUB.UY: Sitio oficial de la República Oriental del Uruguay

La información y los servicios del Estado, en un solo lugar.

2023/08/27

Country of MOLDOVA Tourism Promo

Country of MOLDOVA, one of the most beautiful countries to visit. This promo piece produced by DreamQuest Productions takes the viewer on a short journey to what you could expect to find on your next vacation.

2023/08/26

Ukraine

Explore Ukraine, an open and modern European country and your next travel destination. Invest. Study. Fall in love with Ukraine right NOW.

2023/08/26

Independence Day of the Eastern Republic of Uruguay

Uruguay, country located on the southeastern coast of South America. The second smallest country on the continent, Uruguay has long been overshadowed politically and economically by the adjacent republics of Brazil and Argentina, with both of which it has many cultural and historical similarities. “On the map, surrounded by its large neighbors, Uruguay seems tiny,” writes contemporary Uruguayan historian and novelist Eduardo Galeano. “But not really. We have five times more land than Holland and five times fewer inhabitants. We have more cultivable land than Japan, and a population forty times smaller.” This combination of open space and low population density has afforded Uruguay many opportunities for economic development. An independent country since 1828, with strong ties to the United Kingdom, France, and Italy, Uruguay developed throughout much of the 20th century as one of Latin America’s more progressive societies, notable for its political stability, advanced social legislation, and a relatively large middle class. A period of repressive military rule (1973–85) has cast a long shadow over national life, and, like other countries in the region, Uruguay has been troubled by economic decline and factional struggles in the decades since civilian democratic rule was restored. Such adversities have caused many Uruguayans to emigrate to Europe and North America; as Galeano has remarked, “We export our young.”Almost half the people are concentrated in the metropolitan area of Montevideo, the capital; the second and third largest cities, Salto and Paysandú, are small by comparison. Facing a deep bay at the mouth of the Río de la Plata, Montevideo blends historic areas with tall office towers and well-appointed shopping centres. The old city, with its many museums, open-air markets, and restaurants, remains the heart of Montevideo and sees thousands of international visitors each year. Popular as tourist destinations, too, are beach resorts such as Piriápolis and Punta del Este, as well as the colonial masterpiece Colonia del Sacramento. Land The wedge-shaped country is bounded by Brazil to the north and east, by the Atlantic Ocean to the southeast, and by the Río de la Plata to the south, while the Uruguay River serves as its western boundary with Argentina. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe Now Relief and soils The Uruguayan landscape is largely characterized by gently rolling land, with an average elevation of about 383 feet (117 metres). Tidal lakes and sand dunes fringe the coastline. Elsewhere there are broad valleys, plains (pampas), low plateaus and hills, and ridges—notably Haedo Ridge (Cuchilla de Haedo) in the north and Grande Ridge (Cuchilla Grande) in the southeast—that are a southward extension of the Brazilian Highlands. Mount Catedral, which rises to 1,685 feet (514 metres) near the southeastern coast, is the highest point in the country. The valleys and coastal plains are covered with deposits of sand, clay, and fertile alluvium. Drainage Although it is a well-watered land, no large rivers flow entirely within Uruguay. The Uruguay River and the estuary of the Río de la Plata, along the western border of the nation, are navigable for oceangoing ships until Paysandú and for smaller vessels above that point to the falls at Salto. The smaller Negro River, which traverses the country from northeast to southwest, is navigable only in its lower part, below Rincón del Bonete Lake (the Río Negro Reservoir). Among other small rivers are the Santa Lucía, Cebollatí, and Queguay Grande. Merín (Mirim) Lagoon, which lies mainly within Brazil, is the largest natural lake. Climate Uruguay has a generally pleasant, temperate climate. The average temperature for the midwinter month of July varies from 54 °F (12 °C) at Salto in the northern interior to 50 °F (10 °C) at Montevideo in the south. The midsummer month of January varies from a warm average of 79 °F (26 °C) at Salto to 72 °F (22 °C) at Montevideo. Frost is almost unknown along the coast. Both summer and winter weather may vary from day to day with the passing of storm fronts; a hot northerly wind may occasionally be followed by a cold wind (pampero) from the Argentine Pampas. Uruguay has neither a decidedly dry nor a rainy season. The heaviest precipitation occurs during the autumn months (March and April), although more frequent rains occur in winter. The mean annual precipitation is generally greater than 40 inches (1,000 mm), decreasing with distance from the seacoast, and is relatively evenly distributed throughout the year. Thunderstorms occur frequently during the summer. Plant and animal life Tall-grass prairies once covered most of Uruguay’s land surface but now compete with enclosed, planted pastures. Only a small percentage of the land is forested, most of the trees growing in narrow stretches along watercourses. The principal species are ombu—a scrubby, treelike plant—and alder. Others include willow, eucalyptus, pine, poplar, acacia, and aloe. The algaroba (carob tree) and quebracho (whose wood and bark are utilized in tanning and dyeing) are prevalent, and indigenous palms grow in the valleys and along the southeastern coast. Common smaller plants include mimosa, myrtle, rosemary, and scarlet-flowered ceibo. Animals native to Uruguay have largely disappeared, although pumas and jaguars are still occasionally found in remote areas. Other native mammals include foxes, deer, wildcats, armadillos (mulitas), and several types of rodents, including huge capybaras. Scorpions are rare, but venomous spiders are common. Birdlife includes tiny burrowing owls, crows, lapwings, partridges, quails, hummingbirds, and cardinals. Parakeets are plentiful in the hills, and the lagoons swarm with waterfowl, including white herons, cranes, and flamingos. Rheas are now mainly limited to semidomesticated settings. Lizards, tortoises, and venomous snakes are found in many areas. Caimans inhabit the upper waters of the Uruguay River, and seals are found on small islands off the southeastern coast, particularly on Lobos Island. A network of national parks and a wildlife reserve are dedicated to the preservation of animal and bird populations. More … Score: https://www.britannica.com/place/Uruguay

2023/08/25