Anniversary of the Proclamation of Independence Socialist Republic of Vietnam

Vietnam, country occupying the eastern portion of mainland Southeast Asia. Tribal Viets inhabiting the Red River delta entered written history when China’s southward expansion reached them in the 3rd century bce. From that time onward, a dominant theme of Vietnam’s history has been interaction with China, the source of most of Vietnam’s high culture. As a tribute-paying state after throwing off Chinese rule in 938 ce, Vietnam sent lacquerware, animal skins, ivory, and tropical products to the Chinese emperor and received scrolls on philosophy, administration, and literature in return. Sinic culture seeped deeply into society, but it shaped the aristocracy and mandarinal families more than it did the peasantry, which preserved distinctive customs, beliefs, vocabulary, lifeways, and gender relations. Modeling themselves on Chinese emperors, Vietnam’s kings exacted tribute from ethnic minorities on the periphery of the Vietnamese state and called themselves emperors when not addressing the Chinese court. Although cultural and spatial gaps between the Vietnamese court and the farthest reaches of society were not as great as they were in China (Vietnam is about the size of a Chinese province, with a comparable population), the Vietnamese state’s capacity to rule diminished with distance from the capital. The refractory character of bamboo-hedged peasant communes was captured in the cliché, "The emperor’s writ stops at the village gate." Vietnam has a long history of affiliating with a dominant civilization and adapting that civilization’s ideas, institutions, and technology to Vietnamese purposes. This pattern of affiliating and adapting was already evident in Vietnam’s historical relations with China, and it reappeared as descendants of mandarins responded to the challenge of the West by rejecting tradition and becoming communists to combat colonialism. The pattern was evident again as it animated 20th-century artistic movements that employed Western forms to promote social renovation; and since the 1980s it has been the driving force behind the Vietnam Communist Party’s embrace of economic liberalization and integration into the world economy. Such strategic absorption and adaptation have helped propel Vietnam to become one of the world’s most populous countries, with one of the most rapidly expanding market economies. The capital, Hanoi, is located in the north, while the country’s largest city, Ho Chi Minh City (formerly Saigon), is in the south. Vietnam experienced a period of prolonged warfare in the mid-20th century, and a partitioning (1954–75), first militarily and later politically, into the Democratic Republic of Vietnam, better known as North Vietnam, and the Republic of Vietnam, usually called South Vietnam. Following reunification in April 1975, the Socialist Republic of Vietnam was established in July 1976. Land With an area and configuration similar to those of Norway, Vietnam extends about 1,025 miles (1,650 km) from north to south and is about 30 miles (50 km) wide east to west at its narrowest part. It is bordered by China to the north, the South China Sea to the east and south, the Gulf of Thailand (Gulf of Siam) to the southwest, and Cambodia and Laos to the west. Relief Vietnam’s principal physiographic features are the Annamese Cordillera (French: Chaîne Annamitique; Vietnamese: Nui Truong Son), extending generally from northwest to southeast in central Vietnam and dominating the interior, and two extensive alluvial deltas formed by the Red (Hong) River in the north and the Mekong (Cuu Long) River in the south. Between these two deltas is a long, relatively narrow coastal plain. From north to south the uplands of northern Vietnam can be divided into two distinct regions—the area north of the Red River and the massif that extends south of the Red River into neighbouring Laos. The Red River forms a deep, relatively wide valley that runs in a straight northwest-southeast direction for much of its course from the Chinese border to the edge of its delta. North of the Red River the relief is moderate, with the highest elevations occurring between the Red and Lo (Clear) rivers; there is a marked depression from Cao Bang to the sea. In the Red River delta and in the valleys of the region’s other major rivers are found wide limestone terraces, extensive alluvial plains, and low hills. The northeast coast is dotted with hundreds of islands composed mostly of limestone. Compared with the area north of the Red River, the vast massif extending southwest across Laos to the Mekong River is of considerably higher elevation. Among its outstanding topographic features is Fan Si Peak, which at 10,312 feet (3,143 metres) is the highest point in Vietnam. South of the Black (Da) River are the Ta P’ing, Son La, and Moc Chau plateaus, which are separated by deep valleys. In central Vietnam the Annamese Cordillera runs parallel to the coast, with several peaks rising to elevations above 6,000 feet (1,800 metres). Several spurs jut into the South China Sea, forming sections of the coast isolated from one another. Communication across the central ranges is difficult. The southern portion of the Annamese Cordillera has two identifiable regions. One consists of plateaus of approximately 1,700 feet (520 metres) in elevation that have experienced little erosion, as in the Dac Lac Plateau near Buon Me Thuot. The second region is characterized by heavily eroded plateaus: in the vicinity of Pleiku, the Kontum Plateau is about 2,500 feet (760 metres) above sea level; and in the Da Lat area, the Di Linh Plateau is about 4,900 feet (1,500 metres). Drainage Roughly triangular in shape, with its northeast and southwest sides bounded by the northern uplands, the Red River delta extends inland some 150 miles (240 km) and runs some 75 miles (120 km) along the Gulf of Tonkin. The delta can be divided into four subregions. The northwestern section has the highest and most broken terrain, and its extensive natural levees invite settlement despite frequent flooding. The low-lying eastern portion is less than seven feet (two metres) above sea level in the vicinity of Bac Ninh. Rivers there form small valleys only slightly lower than the general surface level, and they are subject to flooding by the area’s unusually high tides. The third and fourth subregions consist, respectively, of the poorly drained lowlands in the west and the coastal area, which is marked by the remains of former beach ridges left as the delta expanded. The Annamese Cordillera forms a drainage divide, with rivers to the east flowing to the South China Sea and those to the west to the Mekong River. South of the mountain range there is an identifiable terrace region that gives way to the Mekong delta. The terrace region includes the alluvial plains along the Saigon and Dong Nai rivers. The lowlands of southern Vietnam are dominated by alluvial plains, the most extensive of which is the Mekong delta, covering an area of 15,400 square miles (39,900 square km) in Vietnam. Smaller deltaic plains also occur along the south-central coast facing the South China Sea. Soils In northern Vietnam the heavy monsoonal rains wash away rich humus from the highlands, leaving slow-dissolving alumina and iron oxides that give the soil its characteristic reddish colour. The soils of the Red River delta vary: some are fertile and suitable for intense cultivation, while others lack soluble bases. Nonetheless, the delta soils are easily worked. The diking of the Red River to prevent flooding has deprived the delta’s rice fields of enriching silts they once received, and it has been necessary to apply chemical fertilizers. There are some two dozen soil associations, but certain soil types predominate. Among these are red and yellow podzolic soils (i.e., soils that are heavily leached in their upper layers, with a resulting accumulation of materials in the lower layers), which occupy nearly half of the land area, and lateritic soils (reddish brown, leached tropical soils), which constitute another one-tenth more. These soil types dominate the central highlands. Alluvial soils account for about one-fourth of the land in the south and are concentrated in the Mekong delta, as are peat and muck soils. Gray podzolic soils are found in parts of the central highlands and in old terraces along the Mekong, while regurs (rich black loams) and lateritic soils occur in both the central highlands and the terrace zone. Along the coast of central Vietnam are regosols (soft, undeveloped soils) and noncalcic brown soils. More … Score: https://www.britannica.com/place/Vietnam  

2024/09/02

Reverie of Vietnam

When in Vietnam - Set off on a 1650Km north to south journey: capturing the best wonders of Vietnam: Hanoi ancient quarter, the breathtaking Halong Bay, the claustrophobic caves in Trang An, the glamorous fabric merchants in Hoi An, the secret temples inside the marble mountain in Da Nang, the historical old capital Hue, the wet and tropical mekong delta and the white sandy beaches at Phu Quoc.

2024/09/01

Independence day of the Republic of Uzbekistan

Uzbekistan, officially Republic of Uzbekistan, Uzbek Ŭzbekiston or Ŭzbekistan Respublikasi, country in Central Asia. It lies mainly between two major rivers, the Syr Darya (ancient Jaxartes River) to the northeast and the Amu Darya (ancient Oxus River) to the southwest, though they only partly form its boundaries. Uzbekistan is bordered by Kazakhstan to the northwest and north, Kyrgyzstan and Tajikistan to the east and southeast, Afghanistan to the south, and Turkmenistan to the southwest. The autonomous republic of Qoraqalpoghiston (Karakalpakstan) is located in the western third of the country. The Soviet government established the Uzbek Soviet Socialist Republic as a constituent (union) republic of the U.S.S.R. in 1924. Uzbekistan declared its independence from the Soviet Union on August 31, 1991. The capital is Tashkent (Toshkent). Relief Nearly four-fifths of Uzbekistan’s territory, the sun-dried western area, has the appearance of a wasteland. In the northwest the Turan Plain rises 200 to 300 feet (60 to 90 metres) above sea level around the Aral Sea in Karakalpakstan (Qoraqalpog’iston). This terrain merges on the south with the Kyzylkum (Uzbek: Qizilqum) Desert and farther west becomes the Ustyurt Plateau, a region of low ridges, salt marshes, sinkholes, and caverns. Southeast of the Aral Sea, small hills break the flatness of the low-lying Kyzylkum Desert, and, much farther east, a series of mountain ridges partition Uzbekistan’s territory. The western Tien Shan includes the Karzhantau, Ugam, and Pskem ranges, the latter featuring the 14,104-foot (4,299-metre) Beshtor Peak, the country’s highest point. Also part of the western Tien Shan are the Chatkal and Kurama ranges. The Gissar (Hissar) and Alay ranges stand across the Fergana (Farghona) Valley, which lies south of the western Tien Shan. The Mirzachol desert, southwest of Tashkent, lies between the Tien Shan spurs to the north and the Turkestan, Malguzar, and Nuratau ranges to the south. In south-central Uzbekistan the Zeravshan valley opens westward; the cities of Samarkand (Samarqand) and Bukhara (Bukhoro) grace this ancient cultural centre. Drainage Disastrous depletion of the flow of the two historic rivers—the Syr Darya and Amu Darya—has brought rapid change in the Aral Sea and greatly altered the delta of the Amu Darya. Most streams of the delta have dried up, and the Aral Sea, once the fourth largest inland body of water in the world, has lost as much as nine-tenths of both its water (volume) and its surface area since 1961. On the north as well as on the east, huge shallow and dead ponds have become separated from the main remnant Aral Sea, cut off by sandbars that emerged as the water level dropped some 45 feet between 1961 and 1992. After 2010 the eastern lobe began alternating between wet periods and dry periods during which it would dry up completely. Overuse of water from the Syr Darya and Amu Darya in both agriculture and industry brought about this dangerous decline. The Syr Darya ceased to deliver any appreciable amount of water to the Aral Sea by about 1978, and flows from the Amu Darya became negligible in the first decade of the 21st century. The southern rivers tributary to the Amu Darya—the Surkhan and Sherabad, followed by the Zeravshan and Kashka—contribute little flow, for the last two trickle into nothing in the desert. The Syr Darya, the second largest river in Uzbekistan, forms there by the confluence of the Naryn and Qoradaryo rivers. The diversion of the Amu Darya and the Syr Darya has resulted in intense salinization of the sea, which also has suffered tremendous pollution from insecticides and chemical fertilizers during the past several decades. This chemical pollution and the decline in water level have killed the once-flourishing fishing industry, grounded most ships that formerly worked within the Aral’s shores, and contaminated wide areas around the sea with salty lethal dust. This in turn has poisoned vegetables and drinking water, most harmfully affecting the health and livelihood of the human population around the Aral Sea littoral. Climate Marked aridity and much sunshine characterize the region, with rainfall averaging only 8 inches (200 mm) annually. Most rain falls in winter and spring, with higher levels in the mountains and minimal amounts over deserts. The average July temperature is 90 °F (32 °C), but daytime air temperatures in Tashkent and elsewhere frequently surpass 104 °F (40 °C). Bukhara’s high summer heat contrasts with the cooler temperatures in the mountains. In order to accommodate to these patterns, Uzbeks favour houses with windows facing away from the sun but open to porches and tree-filled courtyards shut off from the streets. Although more than 600 streams crisscross Uzbekistan, the climate strongly affects drainage, because river water rapidly escapes through evaporation and filtration or runs off into irrigation systems. Plant and animal life Vegetation patterns in Uzbekistan vary largely according to altitude. The lowlands in the west have a thin natural cover of desert sedge and grass. The high foothills in the east support grass, and forests and brushwood appear on the hills. Forests cover less than 8 percent of Uzbekistan’s area. Animal life in the deserts and plains includes rodents, foxes, wolves, and occasional gazelles and antelopes. Boars, roe deer, bears, wolves, Siberian goats, and some lynx live in the high mountains. Ethnic groups Uzbeks make up more than four-fifths of the population, followed by Tajiks, Kazakhs, Tatars, Russians, and Karakalpaks. Uzbeks are the least Russified of the Turkic peoples formerly under Soviet rule, and virtually all of them still claim Uzbek as their primary language. Languages The Uzbeks speak a language belonging to the southeastern, or Chagatai (Turki), branch of the Turkic language group. Karakalpak, a distantly related Turkic language, enjoys official status alongside Uzbek in Karakalpakstan, where it is spoken by about half a million people. About one-seventh of the population of Uzbekistan speaks Russian. Religion The Uzbeks are Sunni Muslims, and they are considered to be among the most devout Muslims in all of Central Asia. Thus, about three-fourths of the population is Muslim. Slightly less than one-tenth of the population is Eastern Orthodox Christian, and the remainder of the people consider themselves nonreligious or follow other religions. Settlement patterns Most of the population lives in the eastern half of the country. Heavily populated oases and foothill basins are covered with an extensive network of canals intersecting fields, orchards, and vineyards. The fertile Fergana Valley in the extreme east, the most populous area in Central Asia, supports both old and new cities and towns and traditional rural settlements. Much of Karkalpakstan, in the west, is under threat of depopulation caused by the environmental poisoning of the Aral Sea area. Roughly half of the population of Uzbekistan lives in urban areas; the urban population has a disproportionately high number of non-Uzbeks. Slavic peoples Russians, Ukrainians, and Belarusians—held a large proportion of administrative positions. In the late 1980s and early ’90s, many Russians and smaller numbers of Jews emigrated from Uzbekistan and other Central Asian states, changing the ethnic balance and employment patterns in the region. The cities of Samarkand, Bukhara, and Tashkent have histories that extend back to ancient times. Andijon (Andizhan), Khiva, and Qŭqon (Kokand) also have served the region as cultural, political, and trade centres for centuries. Soviet-era architects purposely laid out some newer towns, including Chirchiq, Angren, Bekobod, and Nawoiy (Navoi), close to rich mineral and energy resources. Soviet planners also sited Yangiyul, Guliston, and Yangiyer in areas that produce and process cotton and fruit. Demographic trends Uzbekistan’s population remains youthful in comparison with those of the western parts of the former Soviet Union, though the population aged slightly and steadily over the decades following its independence. Nearly half the population is in the age range of 25–54. This age structure results from the high birth rate after independence: of all the former Soviet republics, Uzbekistan had the greatest number of mothers with 10 or more living children under the age of 20. The birth rate has since decreased. More … Score: https://www.britannica.com/place/Uzbekistan

2024/09/01

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

2024/08/31

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.

2024/08/31

Kyrgyz Republic video presentation in English

2024/08/30

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.

2024/08/29

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  

2024/08/27

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

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

2024/08/27