Independence day of the Republic of Tajikistan

Tajikistan, officially Republic of Tajikistan, Tajik Tojikiston or Jumhurii Tojikiston, Tajikistan also spelled Tadzhikistan, country lying in the heart of Central Asia. It is bordered by Kyrgyzstan on the north, China on the east, Afghanistan on the south, and Uzbekistan on the west and northwest. Tajikistan includes the Gorno-Badakhshan (“Mountain Badakhshan”) autonomous region, with its capital at Khorugh (Khorog). Tajikistan encompasses the smallest amount of land among the five Central Asian states, but in terms of elevation it surpasses them all, enclosing more and higher mountains than any other country in the region. Tajikistan was a constituent (union) republic of the Soviet Union from 1929 until its independence in 1991. The capital is Dushanbe. Several ethnic ties and outside influences complicate Tajikistan’s national identity to a greater extent than in other Central Asian republics. The Tajik people share close kinship and their language with a much larger population of the same nationality living in northeastern Afghanistan, whose population also includes a large proportion speaking Dari, a dialect of Persian intelligible to Tajiks. Despite sectarian differences (most Tajiks are Sunni Muslims, while Iranians are predominantly Shiʿis), Tajiks also have strong ties to the culture and people of Iran; the Tajik and Persian languages are closely related and mutually intelligible. The Tajiks’ centuries-old economic symbiosis with oasis-dwelling Uzbeks also somewhat confuses the expression of a distinctive Tajik national identity. Since the early years of independence, Tajikistan has been wracked by conflict between the government and the Islamic opposition and its allies. Land – Relief More than nine-tenths of Tajikistan’s territory is mountainous; about half lies 10,000 feet (3,000 metres) or more above sea level. The Trans-Alay range, part of the Tien Shan system, reaches into the north. The massive ranges of the southern Tien Shan—the Turkestan Mountains and the slightly lower Zeravshan and Gissar ranges—define the east-central portion of the country. The ice-clad peaks of the Pamir mountain system occupy the southeast. Some of Central Asia’s highest mountains, notably Ibn Sīnā (23,406 feet [7,134 metres]) and Imeni Ismail Samani (24,590 feet [7,495 metres]) peaks, are found in the northern portion of the Pamirs. The valleys, though important for Tajikistan’s human geography, make up less than one-tenth of the country’s area. The largest are the western portion of the Fergana Valley in the north and the Gissar, Vakhsh, Yavansu, Obikiik, Lower Kofarnihon (Kafirnigan), and Panj (Pyandzh) valleys to the south. The entire southern Central Asian region, including Tajikistan, lies in an active seismic belt where severe earthquakes are common. Seismologists have long studied the region, especially in connection with the massive hydroelectric dams and other public works in the area. Drainage and soils The dense river network that drains the republic includes two large swift rivers, the upper courses of the Syr Darya and the Amu Darya, together with their tributaries, notably the Vakhsh and Kofarnihon. The Amu Darya is formed by the confluence of the Panj and Vakhsh rivers; the Panj forms much of the republic’s southern boundary. Most of the rivers flow east to west and eventually drain into the Aral Sea basin. The rivers have two high-water periods each year: in the spring, when rains fall and mountain snows melt, and in the summer, when the glaciers begin to melt. The summer flow is particularly helpful for irrigation purposes. The few lakes in Tajikistan lie mostly in the Pamir region; the largest is Lake Karakul, lying at an elevation of about 13,000 feet. Lake Sarez was formed in 1911 during an earthquake, when a colossal landslide dammed the Murgab River. The Zeravshan Range contains Iskanderkul, which, like most of the country’s lakes, is of glacial origin. Tajikistan’s soil is poor in humus but rich in mineral nutrients. Sand, shingle, scree, bare rock, and permanent snow and ice cover about two-thirds of the surface. Climate The climate of Tajikistan is sharply continental and changes with altitude. In the warm-temperate valley areas, summers are hot and dry; the mean temperature in July is 81 °F (27 °C) in Khujand (Khojand) and 86 °F (30 °C) in Kŭlob (Kulyab), farther south. The corresponding January figures are 30 °F (−1 °C) and 36 °F (2 °C), respectively. In very cold winters, temperatures of −4 °F (−20 °C) and lower have been recorded. Annual precipitation is slight and ranges between 6 and 10 inches (150 and 250 millimetres) but is higher in the Gissar Valley. In the highlands conditions are different: the mean January temperature for Murghob in the Pamirs is −3 °F (−20 °C), and temperatures can drop to −51 °F (−46 °C). In this area precipitation barely reaches 2 to 3 inches a year, most of it falling in summer. Moist air masses move from the west up the valleys, suddenly reaching low-temperature areas and producing locally heavy precipitation, mainly heavy snow of as much as 30 to 60 inches of annual accumulation. Plant and animal life The topographic and climatic variety gives Tajikistan an extremely varied plant life, with more than 5,000 kinds of flowers alone. Generally grasses, bushes, and shrubs predominate. The country’s animal life is abundant and diverse and includes species such as the great gray lizard, jerboa, and gopher in the deserts and deer, tiger, jackal, and wildcat in wooded areas or reedy thickets. Brown bears live at lower mountain levels, and goats and golden eagles higher up. People of Tajikistan - Ethnic groups The area’s population is ethnically mixed, as it has been for centuries, but more than four-fifths of the population is ethnically Tajik, a proportion that rose with the emigration of non-Tajiks during the protracted civil war. The Tajiks are a traditionally sedentary people who speak a form of Persian (called Tajik) and whose culture has been significantly influenced by Central Asian sedentary culture. The name Tajik came to denote a distinct nationality only in the modern period; not until the 1920s did an official Tajik territorial-administrative unit exist under that name. Citizens of Tajikistan, regardless of ethnicity, are referred to as Tajikistanis. On the basis of language, customs, and other traits, the Tajiks can be subdivided into a number of distinct groups. The Pamir Tajiks within the Gorno-Badakhshan autonomous region include minority peoples speaking Wakhī, Shughnī, Rōshānī, Khufī, Yāzgulāmī, Ishkashimī, and Bartang, all Iranian languages. Another distinct group is formed by the Yaghnābīs, direct descendants of the ancient Sogdians, who live in the Zeravshan River basin. So closely are the Tajiks mixed with neighbouring Uzbeks that the Soviet partition of the area in 1924 failed to segregate the two nationalities with any degree of thoroughness. With nearly one million Tajiks in Uzbekistan and more than one million Uzbeks in Tajikistan, these nationalities remain in intimate, though not always friendly, interrelation. The country’s other ethnic groups include Russians, Tatars, Kyrgyz, Ukrainians, Germans, Jews, and Armenians. Languages Tajik is the official language and is spoken by most people in Tajikistan. A member of the southwest group of Iranian languages, it is closely related to the mutually intelligible dialects of Farsi and Dari in Iran and Afghanistan, respectively, though it differs from these dialects in that it is written in the Cyrillic alphabet. The dialects of the Pamirs and the Yaghnob River valley, which were classified as Tajik during the Soviet era, actually belong to the eastern group of Iranian languages; speakers of these dialects must use Tajik as a lingua franca to communicate with outsiders. Russian is widely used for administration and business, but few speak it natively. Uzbek is the second most widely spoken language and is written in the Cyrillic script, unlike in Uzbekistan where Uzbek is written in a modified Latin alphabet. Religion The vast majority of Tajikistanis are Muslim, mostly of the Sunni Ḥanafī school. A small percentage of Muslims are Ismaʿīlī Shiʿi, located primarily in the Pamirs. The Christian population has been predominantly Russian, but most ethnic Russians have left since the disintegration of the Soviet Union. More … Score: https://www.britannica.com/place/Tajikistan

2022/09/09

Anniversary of the DPRK Proclamation Democratic People's Republic of Korea

North Korea, country in East Asia. It occupies the northern portion of the Korean peninsula, which juts out from the Asian mainland between the East Sea (Sea of Japan) and the Yellow Sea; North Korea covers about 55 percent of the peninsula’s land area. The country is bordered by China and Russia to the north and by the Republic of Korea (South Korea) to the south. The national capital, P’yŏngyang, is a major industrial and transport centre near the west coast. North Korea faces South Korea across a demilitarized zone (DMZ) 2.5 miles (4 km) wide that was established by the terms of the 1953 armistice that ended fighting in the Korean War (1950–53). The DMZ, which runs for about 150 miles (240 km), constitutes the 1953 military cease-fire line and roughly follows latitude 38° N (the 38th parallel) from the mouth of the Han River on the west coast of the Korean peninsula to a little south of the North Korean town of Kosŏng on the east coast. Land - Relief Mountains and valleys characterize most of North Korea. The Kaema Highlands in the northeast have an average elevation of 3,300 feet (1,000 metres) above sea level and form the topographic roof of the entire Korean peninsula. Mount Paektu (9,022 feet [2,750 metres]), the highest mountain in North Korea and on the peninsula, rises at the northern edge of this plateau in the Changbaek (Changbai) Mountains along the Sino-Korean border; it is an extinct volcano topped by a large crater lake. The Nangnim Mountains run from north to south through the middle of the country, forming a divide between the eastern and western slopes of the peninsula. The Kangnam and Myohyang ranges and Mounts Ŏnjin and Myŏrak, all structural extensions of the Nangnim Mountains, extend parallel to each other toward the southwest. Large river-valley plains have developed between the western mountains; they merge along the narrow, irregular coastal plain on the west coast. The Hamgyŏng Mountains, extending from the Nangnim Mountains to the northeast, form a steep slope between the Kaema Highlands and the East Sea. The T’aebaek Mountains extend from southeastern North Korea into South Korea along the eastern coast; one peak, Mount Kŭmgang (5,374 feet [1,638 metres]), is renowned for its scenic beauty. Drainage and soils The longest river of North Korea is the Yalu, in Korean called the Amnok. It rises on the southern slope of Mount Paektu and flows southwestward for some 500 miles (800 km) to its mouth on Korea Bay. The Tumen (Tuman) River also begins at Mount Paektu but runs northeastward for about 325 miles (520 km) to the East Sea. There are no large streams along the east coast except for the Tumen River, and all the significant rivers, such as the Yalu, Ch’ŏngch’ŏn, Taedong, Chaeryŏng, and Yesŏng, drain to the Yellow Sea. The relatively large valley plains of the western rivers are major agricultural regions. More than three-fifths of the soils are locally derived from the weathering of granitic rocks or various kinds of schists (crystalline rocks). The soils are generally brownish, abundant in sandy materials, and low in fertility. Well-developed reddish brown soils derived from limestone are found in North Hwanghae province and the southern part of South P’yŏngan province. Podzols (ash-gray forest soil) have developed in the Kaema Highlands as a result of the cold climate and coniferous forest cover there. Although most of the soils are infertile and lack organic content, the valleys and coastal plains have relatively rich alluvial soils. Climate North Korea has a generally cool continental climate. The winter season, from December to March, is long and cold; mean temperatures in January range between about 20 °F (−7 °C) in the south and −10 °F (−23 °C) in the northern interior. The summer, from June to September, is warm, with mean July temperatures above the upper 60s F (about 20 °C) in most places. Accordingly, the annual range of temperatures is large—about 54 °F (30 °C) at P’yŏngyang and about 77 °F (43 °C) at Chunggang (Chunggangjin), where the lowest temperature in the Korean peninsula, −46.5 °F (−43.6 °C), has been recorded. Because of ocean currents and the mountain ranges bordering the narrow coastal lowlands, winter temperatures on the east coast are some 5 to 7 °F (3 to 4 °C) higher than those of the west coast. Most of the country receives about 40 inches (1,000 mm) of precipitation annually. The northern inland plateau, however, receives only about 24 inches (610 mm) and the lower reaches of the Taedong River valley 32 inches (810 mm), while the upper Ch’ŏngch’ŏn River area averages between about 48 and 52 inches (1,220 and 1,320 mm) yearly. Some three-fifths of the annual precipitation falls in the four months from June to September; this heavy concentration of rainfall is related to the humid summer monsoon from the Pacific Ocean, which also produces occasional typhoons (tropical cyclones). Only a small portion of the total precipitation occurs in winter, generally as snow; snowfall can be locally heavy, as in the T’aebaek Mountains. There are about 200 frost-free days along the coast but fewer than 120 in the northern Kaema Highlands. Plant and animal life Vegetation on the highlands, especially around Mount Paektu, consists of coniferous trees such as the Siberian fir, spruce, pine, and Korean pine (Pinus koraiensis). The western lowlands were originally covered by temperate mixed forests with many types of plants, but continuous deforestation has left only remote patches of the original forests. Most of the lowlands are now cultivated, except for some of the hills that are covered with small pine groves mixed with oaks, lindens, maples, and birches. Along streams that are subject to flooding or where the ground is too stony for cultivation, reeds, sedges, wild mulberry trees, and Italian poplars are found. Common river fish include carp and eels. Because of deforestation, the populations of deer, mountain antelope, goats, tigers, and leopards have greatly decreased and are restricted to the remote forests. In the plains, however, it is still possible to see wild pigeons, herons, cranes (which nest near areas of human habitation), and many migratory waterfowl, which alight in the rice fields. The DMZ between North and South Korea has become a de facto nature preserve. Once farmland and subsequently a devastated battleground, the DMZ has lain almost untouched since the end of hostilities in 1953 and has reverted to nature to a large extent, making it one of the most pristine undeveloped areas in Asia. The zone contains many ecosystems including forests, estuaries, and wetlands frequented by migratory birds. It serves as a sanctuary for hundreds of bird species, among them the endangered white-naped and red-crowned cranes, and is home to dozens of fish species and Asiatic black bears, lynxes, and other mammals. People of North Korea - Ethnic groups and languages The Korean peninsula is one of the most ethnically homogeneous regions in the world. The North Korean population, which has been largely isolated since 1945, is almost entirely Korean; a tiny number of Chinese constitute the only other significant ethnic group. All Koreans speak the Korean language, whose relationship to other languages is disputed; it may be related to Japanese or languages of the Altaic group, and it contains many Chinese loanwords. The Korean script, known in North Korea as Chosŏn muntcha and in South Korea as han’gŭl (Hangul), is composed of phonetic symbols for the 10 vowels and 14 consonants. In North Korea a systematic effort has been made to eliminate Chinese and Western loanwords, as well as any vestiges of the Japanese imposed during the colonial period, and Chosŏn muntcha has been used exclusively without Chinese characters in newspapers and other publications since 1945. More … Score: https://www.britannica.com/place/North-Korea

2022/09/09

Anniversary of the Proclamation of the Republic of San Marino

San Marino, small republic situated on the slopes of Mount Titano, on the Adriatic side of central Italy between the Emilia-Romagna and Marche regions and surrounded on all sides by the republic of Italy. It is the smallest independent state in Europe after Vatican City and Monaco and, until the independence of Nauru (1968), the smallest republic in the world. San Marino has an irregular rectangular form with a maximum length of 8 miles (13 km), northeast to southwest. It is crossed by the Marano and Ausa (Aussa) streams, which flow into the Adriatic Sea, and by the stream of San Marino, which falls into the Marecchia River. The landscape is dominated by the huge, central limestone mass of Mount Titano (2,424 feet [739 metres]); hills spread out from it on the southwest, whereas the northeastern part gently slopes down toward the Romagna plain and the Adriatic coast. The silhouette of Mount Titano, with its three summits crowned by ancient triple fortifications, may be seen from many miles away. In 2008 Mount Titano and the historic centre of San Marino were designated a UNESCO World Heritage site. The climate is mild and temperate, with maximum temperatures in the high 70s F (about 26 °C) in summer and the high teens F (about −7 °C) in winter. Annual rainfall ranges between about 22 inches (560 mm) and 32 inches (800 mm). Vegetation is typical of the Mediterranean zone, with variations due to elevation, and includes olive, pine, oak, ash, poplar, fir, and elm, as well as many kinds of grasses and flowers. Besides domestic and farmyard animals, moles, hedgehogs, foxes, badgers, martens, weasels, and hares are found. Indigenous birds and birds of passage are plentiful. Although traces of human presence from both prehistoric and Roman times exist in the territory, Mount Titano and its slopes are known to have been populated, with certainty, only after the arrival of St. Marinus and his followers. San Marino citizens, or Sammarinesi, make up more than four-fifths of the country’s population, with Italians composing most of the remainder. Thousands of Sammarinesi reside abroad, principally in Italy, the United States, France, and Argentina. Nearly nine-tenths of San Marino’s citizens are Roman Catholics, though there is no official religion. The official language is Italian. A widely spoken dialect has been defined as Celto-Gallic, akin to the Piedmont and Lombardy dialects as well as to that of Romagna. Because centuries-long quarrying has exhausted Mount Titano’s stone and ended the craft that depended upon it, the territory is now without mineral resources. All electrical power is transferred via electrical grid from Italy, San Marino’s main trading partner. The country’s principal resources are industry, tourism, commerce, agriculture, and crafts. Manufactures include electronics, paint, cosmetics, ceramics, jewelry, and clothing. Ceramic and wrought-iron articles, as well as modern and reproduction furniture, are among San Marino’s traditional craft products. Fine printing, particularly of postage stamps, is a consistent source of revenues. Banking is a vital industry. In 2002 San Marino replaced the Italian lira with the euro as its national currency. Tourism is the sector of greatest expansion, and it makes a major contribution to the inhabitants’ income. Alongside traditional excursion tourism, there is convention-type tourism, based on modern hotel facilities, as well as residential tourism. Agriculture, although no longer the principal economic resource in San Marino, remains vital. Wheat, grapes, and barley are the chief crops; dairying and livestock also are important. About three-fourths of the land is given to permanent cultivation. The capital, San Marino city, is set high on the western side of Mount Titano, beneath the fortress crowning one of its summits, and is encircled by triple walls. Borgo Maggiore, farther down the slope, was for centuries San Marino’s commercial centre, and Serravalle, beneath its castle of the Malatesta family, is agricultural and industrial. San Marino is overwhelmingly urban in character, and those three cities are home to nearly two-thirds of San Marino’s population. Most of San Marino’s landscape is agricultural in character, but industrial concerns have intruded on the centuries-old forms of agricultural life. The San Marino constitution, originating from the Statutes of 1600, provides for a parliamentary form of government. The Great and General Council (Parliament) has 60 members, elected every five years by all adult citizens. It has legislative and administrative powers and every six months nominates the two captains regent (capitani reggenti), who hold office for that period and may not be elected again until three years have elapsed. The Great and General Council is headed by the captains regent, who are heads of state and of the administration. The Congress of State, a council of ministers, is composed of 10 members, elected by the Great and General Council from among its members, and constitutes the central organ of executive power. Each member has charge of a ministerial department. Social programs for the citizens of San Marino are extensive. The state attempts to keep unemployment in check by seeking to provide employment for those who cannot find work with private concerns. All citizens (who make social security contributions) receive free, comprehensive, high-quality medical care and assistance in sickness, accident, and old age, as well as family allowances. The state aids home ownership through its buildings schemes. Education is free and compulsory up to age 16. The University of San Marino was founded in 1985. A public security force of about 50 persons provides national defense. A network of roads connects San Marino with the surrounding regions of Italy. Motorcoach services connect San Marino city with Rimini, Italy, and, in summer, directly with the Adriatic coast. The main airport serving San Marino is the Federico Fellini International Airport in Rimini. There are no railroads, but the capital is reached from Borgo Maggiore by means of a cable railway. History The Republic of San Marino traces its origin to the early 4th century ce when, according to tradition, St. Marinus and a group of Christians settled there to escape persecution. The Castellum Sancta Marini is mentioned in the Liber Pontificalis (“The Book of the Pontiffs”) in 755; the oldest document in the republican archives mentions the abbot of San Marino in 885. By the 12th century San Marino had developed into a commune ruled by its own statutes and consuls. The commune was able to remain independent despite encroachments by neighbouring bishops and lords, largely because of its isolation and its mountain fortresses. Against the attacks of the Malatesta family, who ruled the nearby seaport of Rimini, San Marino enjoyed the protection of the rival family of Montefeltro, who ruled Urbino. By the middle of the 15th century, it was a republic ruled by a Grand Council—60 men taken from the Arengo, or Assembly of Families. Warding off serious attacks in the 16th century (including an occupation by Cesare Borgia in 1503), San Marino survived the Renaissance as a relic of the self-governing Italian city-states. Rule by an oligarchy and attempts to annex it to the Papal States in the 18th century marked the decline of the republic. When Napoleon invaded Italy, he respected the independence of the republic and even offered to extend its territory (1797). The Congress of Vienna (1815), at the end of the Napoleonic Wars, also recognized its independent status. During the 19th-century movement for Italian unification, San Marino offered asylum to revolutionaries, among them Giuseppe Garibaldi. After Italy became a national state, a series of treaties (the first in 1862) confirmed San Marino’s independence. In World War II, San Marino remained neutral, but it was the target of a British bombing raid in 1944 and was briefly occupied by both the Germans and the Allies later that year. More … Score: https://www.britannica.com/place/San-Marino-republic-Europe  

2022/09/03

Difusión del aplicativo móvil "Bienvenido al Perú"

La Embajada del Perú en Polonia tiene el agrado de informar sobre la implementación y entrada en producción de la aplicación móvil “Bienvenidos al Perú” mediante la cual los pasajeros que ingresan al país que porten equipaje afecto al pago de tributos o dinero por declarar podrán registrar la “Declaración Jurada de Equipaje” y “Declaración Jurada de Dinero” (ingreso), la misma que se encuentra disponible para su descarga gratuita en las tiendas virtuales.

2022/09/02

W Rybniku na Śląsku stanęła 15-metrowa replika wieży Eiffla ....

Une réplique de la Tour Eiffel haute de 15 mètres vient d’être érigée à Rybnik en Silésie sur le nouveau rond-point appelé « Niedobczyce-Paryż » du nom attribué au quartier résidentiel qui se trouve à proximité. L'installation de la tour illuminée indiquera l'entrée de la route régionale Racibórz-Pszczyna.

2022/09/02

EXAKT4YOU EXCHANGE AFRIKA HEIDENHEIM

H.E. Dr. Abdallah Possi, the Ambassador of Tanzania to Germany, attending EXAKT4YOU EXCHANGE AFRIKA HEIDENHEIM 12.8.2022 theme is sustainability communication-climate change #Tanzania #nmaist #ClimateCrisis #sdg13

2022/09/02

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.

2022/09/02

La publicación de la centésima décima tercera edición del Boletín Cultural Quipu Internacional

La Embajada del Perú en Polonia informa sobre la publicación de la centésima décima tercera edición del Boletín Cultural Quipu Internacional. Este número está dedicado al quechua. El texto principal es un fragmento del recientemente publicado libro ¨Nación anti¨ del poeta, traductor y profesor cusqueño Odi González, quien reflexiona en esta publicación sobre su lengua materna: el quechua. Asimismo, incluye una nota sobre la nueva exhibición permanente del Museo Nacional de Arqueología, Antropología e Historia del Perú que lleva por título ¨Sala Independencia¨, que busca mostrar la complejidad de nuestro proceso independista.

2022/09/02

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  

2022/09/02