Quel est le point commun entre Jean-Pierre Norblin de la Gourdaine, Nicolas Chopin et Baudouin de Courtenay ? Ce sont tous les trois des Français de Varsovie !

Depuis début décembre, l’ambassade vous invite à venir voir sur ses grilles l’exposition « Les Français à Varsovie ». Ce projet du Centre de recherches sur la culture de Varsovie (Centrum Badań nad Kulturą Warszawy Uniwersytetu Warszawskiego), porté par Prof. Elżbieta Wichrowksa permet de replonger dans l’histoire de la capitale ?? et de celle des Français qui y ont élu résidence au fil des siècles.

2022/12/23

Emperor Akihito's birthday

Japan, island country lying off the east coast of Asia. It consists of a great string of islands in a northeast-southwest arc that stretches for approximately 1,500 miles (2,400 km) through the western North Pacific Ocean. Nearly the entire land area is taken up by the country’s four main islands; from north to south these are Hokkaido (Hokkaidō), Honshu (Honshū), Shikoku, and Kyushu (Kyūshū). Honshu is the largest of the four, followed in size by Hokkaido, Kyushu, and Shikoku. In addition, there are numerous smaller islands, the major groups of which are the Ryukyu (Nansei) Islands (including the island of Okinawa) to the south and west of Kyushu and the Izu, Bonin (Ogasawara), and Volcano (Kazan) islands to the south and east of central Honshu. The national capital, Tokyo (Tōkyō), in east-central Honshu, is one of the world’s most populous cities. The Japanese landscape is rugged, with more than four-fifths of the land surface consisting of mountains. There are many active and dormant volcanoes, including Mount Fuji (Fuji-san), which, at an elevation of 12,388 feet (3,776 metres), is Japan’s highest mountain. Abundant precipitation and the generally mild temperatures throughout most of the country have produced a lush vegetation cover and, despite the mountainous terrain and generally poor soils, have made it possible to raise a variety of crops. Japan has a large and, to a great extent, ethnically homogeneous population, which is heavily concentrated in the low-lying areas along the Pacific coast of Honshu. Complexity and contrast are the keynotes of life in Japan—a country possessing an intricate and ancient cultural tradition yet one that, since 1950, has emerged as one of the world’s most economically and technologically advanced societies. Heavy emphasis is placed on education, and Japan is one of the world’s most literate countries. Tension between old and new is apparent in all phases of Japanese life. A characteristic sensitivity to natural beauty and a concern with form and balance are evident in such cities as Kyōto and Nara, as well as in Japan’s ubiquitous gardens. Even in the countryside, however, the impact of rapid Westernization is evident in many aspects of Japanese life. The agricultural regions are characterized by low population densities and well-ordered rice fields and fruit orchards, whereas the industrial and urbanized belt along the Pacific coast of Honshu is noted for its highly concentrated population, heavy industrialization, and environmental pollution. Humans have occupied Japan for tens of thousands of years, but Japan’s recorded history begins only in the 1st century bce, with mention in Chinese sources. Contact with China and Korea in the early centuries ce brought profound changes to Japan, including the Chinese writing system, Buddhism, and many artistic forms from the continent. The first steps at political unification of the country occurred in the late 4th and early 5th centuries ce under the Yamato court. A great civilization then developed first at Nara in the 8th century and then at Heian-kyō (now Kyōto) from the late 8th to the late 12th century. The seven centuries thereafter were a period of domination by military rulers culminating in near isolation from the outside world from the early 17th to the mid-19th century. The reopening of the country ushered in contact with the West and a time of unprecedented change. Japan sought to become a modern industrialized nation and pursued the acquisition of a large overseas empire, initially in Korea and China. By late 1941 this latter policy caused direct confrontation with the United States and its allies and to defeat in World War II (1939–45). Since the war, however, Japan’s spectacular economic growth—one of the greatest of any nation in that period—brought the country to the forefront of the world economy. It now is one of the world’s foremost manufacturing countries and traders of goods and is a global financial leader. Land Japan is bounded to the west by the Sea of Japan (East Sea), which separates it from the eastern shores of South and North Korea and southeastern Siberia (Russia); to the north by La Perouse (Sōya) Strait, separating it from Russian-held Sakhalin Island, and by the Sea of Okhotsk; to the northeast by the southern Kuril Islands (since World War II under Soviet and then Russian administration); to the east and south by the Pacific; and to the southwest by the East China Sea, which separates it from China. The island of Tsushima lies between northwestern Kyushu and southeastern South Korea and defines the Korea Strait on the Korean side and the Tsushima Strait on the Japanese side. Relief The mountainous character of the country is the outcome of orogenic (mountain-building) forces largely during Quaternary time (roughly, the past 2.6 million years), as evidenced by the frequent occurrence of violent earthquakes, volcanic activity, and signs of change in sea levels along the coast. There are no sizable structural plains and peneplains (large land areas leveled by erosion), features that usually occur in more stable regions of the Earth. The mountains are for the most part in a youthful stage of dissection in which steep slopes are incised by dense river-valley networks. Rivers are mostly torrential, and their valleys are accompanied by series of river terraces that are the result of movements in the Earth’s crust, as well as climatic and sea-level changes in Holocene times (i.e., the past 11,700 years). Recent volcanoes are juxtaposed with old and highly dissected ones. The shores are characterized by elevated and depressed features such as headlands and bays, which display an incipient stage of development. The mountains are divided into many small land blocks that are separated by lowlands or deep saddles; there is no long or continuous mountain range. These land blocks are the result of intense faulting (movement of adjacent rock masses along a fracture) and warping (bending of the Earth’s crust); the former process is regarded as dominant. One consequence is that mountain blocks are often bounded by fault scarps and flexure slopes that descend in step formation to the adjacent lowlands. Coalescing alluvial fans—cone-shaped deposits of alluvium that run together—are formed where rivers emerge from the mountains. When the rivers are large enough to extend their courses to the sea, low deltaic plains develop in front of the fans; this occurs most frequently where the rivers empty into shallow and sheltered bays, as in the deltas of Kantō (Kwanto), Nōbi, and Ōsaka. In most places, however, fan surfaces plunge directly into the sea and are separated by low, sandy beach ridges. Dissected plains are common. Intense disturbances have caused many former alluvial fans, deltas, and sea bottoms to be substantially uplifted to form flat-topped uplands such as those found in the Kantō Plain. Frequently the uplands have been overlain with volcanic ash, as in the Kantō and Tokachi plains. Geologic framework Japan is one of the world’s most geologically unstable areas. The country experiences some 1,000 tremors annually, most of them minor, though major quakes—as in Tokyo-Yokohama in 1923 and Kōbe in 1995—cause considerable loss of life and widespread destruction. Violent volcanic eruptions occur frequently, and at least 60 volcanoes have been active within historical time. Volcanoes born since 1900 include Shōwa Volcano on Hokkaido and Myōjin Rock off the Beyoneisu (or Bayonnaise) Rocks in the Pacific. Among the major eruptions since 1980 are those of Mounts O (1983) and Mihara (1986) in the Izu Islands and Mount Unzen (1991) in Kyushu. The country’s abundant hot springs are mostly of volcanic origin. Many of the gigantic volcanoes are conical in shape (e.g., Mount Fuji), while others form steep lava domes (e.g., Mounts Dai and Unzen). Conspicuous shield volcanoes (broad, gently sloping volcanic cones) are rare, and extensive lava plateaus are lacking. One of the characteristics of the volcanic areas is the prevalence of calderas (large, circular, basin-shaped volcanic depressions), especially in the northeast and southwest, many of which are filled with water, such as Lakes Kutcharo, Towada, and Ashi. The cause of this instability—indeed, the reason for Japan’s existence—is the tectonic movement of several of the Earth’s major crustal plates in the vicinity of the archipelago. Most important is the subduction (sinking) of the Pacific Plate (in the north) and the Philippine Plate (in the south) beneath the Eurasian Plate, upon which Japan lies. The movements of these plates have formed six mountain arcs off the northeastern coast of Asia: from northeast to southwest, the Chishima Range of the Kuril Islands; the Karafuto (Sakhalin) Mountain system of Hokkaido; the Northeast, Southwest, and Shichito-Mariana ranges of Honshu; and the Ryukyu Island formations. More … Source: https://www.britannica.com/place/Japan  

2022/12/23

NIAMEY CITY ,THE CAPITAL OF NIGER

2022/12/19

Alter do Chão

No estado do Pará, no coração da Amazônia brasileira, encontra-se Alter do Chão, um belíssimo trecho da margem direita do rio Tapajós. Alter do Chão, que fica a 37 quilômetros da cidade de Santarém, conta com a mais bonita praia de água doce do mundo, segundo avaliação do jornal britânico The Guardian. A melhor época do ano para visitar Alter do Chão é o chamado verão amazônico, de agosto a dezembro, quando não chove na região e as praias de areia branca surgem nas margens dos rios.

2022/12/19

QATAR PROMO VIDEO

Building Quality and Safety into the Healthcare System - ISQua's 32nd International Conference will be held in Doha's National Convention centre.

2022/12/19

Cérémonie de décoration de Mme Agata Tuszyńska dans l’Ordre des Arts et des Lettres

Le 5 décembre 2022, l’Ambassadeur de France a remis l’insigne de chevalier de l’Ordre des Arts et des Lettres à Agata Tuszyńska, théâtrologue, historienne de la littérature, écrivaine et poète. S’intéressant tout particulièrement aux questions de mémoire, Mme Tuszyńska commence sa carrière d’écrivaine par un travail de mémoire personnel sur ses origines juives puis étend ses recherches à l’histoire des Juifs de Pologne en général.

2022/12/19

Day of the Republic of Niger

Niger, officially Republic of Niger, French République du Niger, landlocked western African country. It is bounded on the northwest by Algeria, on the northeast by Libya, on the east by Chad, on the south by Nigeria and Benin, and on the west by Burkina Faso and Mali. The capital is Niamey. The country takes its name from the Niger River, which flows through the southwestern part of its territory. The name Niger derives in turn from the phrase gher n-gheren, meaning “river among rivers,” in the Tamashek language. Land - Relief Niger extends for about 750 miles (1,200 km) from north to south and about 930 miles (1,460 km) from east to west. It tends to monotony in its features, is intersected by numerous depressions, and is dominated by arid highlands in the north. Rainfall increases as one proceeds southward so that the country divides naturally into three distinct zones—a desert zone in the north; an intermediate zone, where nomadic pastoralists raise cattle, in the centre; and a cultivated zone in the south. It is in this southern zone that the greater part of the population, both nomadic and settled, is concentrated. The highlands of the north are cut by valleys (kori) of the Aïr Massif, which is an extension of the Ahaggar (Hoggar) Mountains of Algeria and consists of a range running north to south in the centre of Niger, with individual mountain masses forming separate “islands”: from north to south these are Tazerzaït, where Mount Gréboun reaches an elevation of 6,379 feet (1,944 metres); Tamgak; Takolokouzet; Angornakouer; Bagzane; and Tarouadji. To the northeast is a series of high plateaus, which form a bridge between the Ahaggar Mountains of Algeria and the Tibesti Mountains of Chad. From west to east these are the plateaus of Djado, Mangueni, and Tchigaï. The sandy regions of the Nigerien Sahara extend to either side of the Aïr. To the west the Talak region includes the Tamesna area in the north (where fossil valleys are filled with moving sand dunes) and the Azaoua area in the south. East of the Aïr is the Ténéré region, covered partly by an expanse of sand called an erg, partly by a stony plain called a reg. The plateaus of the south, which form a belt about 900 miles long, may be divided into three regions. To the west is the Djerma Ganda region. Its large valleys are filled with sand, while dallol (fossilized valleys of rivers that formed tributaries of the Niger in ancient times) descend from the Aïr and the Iforas Massif of neighbouring Mali. The central region consists of the rocky Adar Doutchi and Majia areas; it is the region of the gulbi (dried-up valleys of former tributaries of the Sokoto River) and the Tegama—a tableland of sandstone, ending, toward the Aïr, at the Tiguidit scarp. To the east the underlying rock reappears in the Damagarim, Mounio, and Koutous regions, to the north of which is the region of Damergou, consisting of clays. In the Manga region, in the east, traces of ancient watercourses appear on the sandy plain. Drainage and soils It is convenient to make a distinction between the ancient hydrographic system, which allowed agriculturalists, fishermen, and pastoralists to live in the Aïr region about 5,000 or 6,000 years ago, and the present simple system, which forms the basis of the marked difference between the northern and southern parts of the country. The present system includes to the west the Niger River basin and to the east the basin of Lake Chad; between the two occur vestiges of the older system, such as the dallol and the gulbi. To the west the Niger River crosses about 350 miles of Niger’s territory. Because of the change in river flow, which occurs because of the dispersal of its waters in its interior delta region in Mali, it is only in January and February that it flows past Niamey in flood. At other times the river is fed by certain temporary watercourses that flow in from the right bank. These are the Gorouol, the Dargol, the Sirba, the Goroubi, the Djamangou, the Tapoa, and the Mékrou; the last two flow through W National Park (so called because the Niger flows through the area in the form of a W). On the left bank, proceeding eastward, appear the dallol, the vestiges of the older watercourses. Generally running from north to south, they constitute zones of dampness, although a few still contain waters that flow toward the Niger. The best known are the Bosso, the Foga, and the Maouri wadis. Other vestiges consist of the kori, which run down from the Aïr and from former tributaries that had their sources in the Iforas Massif, and which flowed to a confluence at what is now the Ti-m-merhsoï Wadi. No waters flow through the kori now, but water is still to be found beneath their sands. Other remnants of the old system are formed by the gulbi, through which water still flows annually, occasionally causing damage. To the east is situated the basin of Lake Chad, a large, shallow lake, which at its highest contemporary level has an area of approximately 9,650 square miles; of this, Niger possesses about 1,100 square miles. Its extent is considerably reduced during the dry season. The Komadougou Yobé River, which flows into Lake Chad from the west, forms part of the frontier between Niger and Nigeria. Its water level, which begins to rise in August, from January to May consists only of some stagnant pools. In addition to the drainage system described, it may be noted that rainwater collects in several basins, so that some permanent lakes or pools also exist; these are found at Keïta and Adouna in the Adar Doutchi region, at Madaroumfa in the Maradi gulbi, and at Guidimouni to the east of Zinder. The water table in some areas can also be tapped to produce artesian wells. The soils fall into three natural regions. In the Saharan region in the north the soil is infertile, except in a few oases where water is found. In the region known as the Sahel, which forms a transitional zone between the Sahara and the region to the south, the soils are thin and white, being covered with salty deposits resulting from intense evaporation that forms an infertile surface crust. The third region (in the south) is cultivated. In this area the soils are associated with extensive dunes or uplands or with basins or depressions. Some of the soils in the latter, such as those in the Niger basin and in the gulbi, are rich. Black soils occur in the Kolo basin. Throughout the region, however, and above all on the plateaus, less fertile lateritic (leached iron-bearing) soils occur. Climate of Niger Niger extends southward from the tropic of Cancer, and the northern two-thirds of its territory lies in dry tropical desert. In the southern part of the country the climate is of the type known as Sahelian, which is characterized by a single, short rainy season. In January and February the continental equivalent of the northeast trade winds, the harmattan, blows southwestward from the Sahara toward the equator. Typically dust-laden, dry, and desiccating, the harmattan hinders normal living conditions on the southern fringe of the desert. From April to May the southern trade winds blowing from the Atlantic reach the equator and are diverted toward the Sahara where they meet with the harmattan—an encounter that results in violent line squalls and that signals the beginning of the rainy season. The rains last from one to four months, according to the latitude; August is the rainy month everywhere except in the far north, where the rainfall is unpredictable. Niger lies in one of the hottest regions of the world. Temperatures rise from February to May and drop during the “winter” rainy season, rising again somewhat before falling to their annual minimum averages in December or January. During May (the hottest month), afternoon temperatures are high everywhere, ranging from a low of about 108 °F (42 °C) at Nguigmi on Lake Chad to 113 °F (45 °C) at Bilma and Agadez, both in the northern desert. In January, afternoon temperatures average more than 90 °F (mid-30s C) at most stations but at night may drop to freezing level in the desert. The daily range is greater in the desert north than in the south and is also more extreme during the dry season. Rainfall varies according to location as well as season. The 10-inch isohyet (line on a map connecting points having equal rainfall) follows a line from near Tahoua to Gouré, in effect marking the northern limit of nomadic pastoral life, for the rainfall permits a sparse vegetation to grow. To the extreme south the 30-inch isohyet marks the southern limit of this zone, after which the southern agricultural zone begins. In the course of the same rainy season a most irregular spatial pattern of rainfall may occur, while from one year to another the total amount of rainfall may also vary; in addition, the rainy season itself may arrive early or late, thus jeopardizing crops. More … Source: https://www.britannica.com/place/Niger

2022/12/18

Anniversary of the assumption of power by the founder of the state, Sheikh Jassem Bin Mohamed Bin Al-Thani State of Qatar

Qatar, independent emirate on the west coast of the Persian Gulf. Occupying a small desert peninsula that extends northward from the larger Arabian Peninsula, it has been continuously but sparsely inhabited since prehistoric times. Following the rise of Islam, the region became subject to the Islamic caliphate; it later was ruled by a number of local and foreign dynasties before falling under the control of the Thani dynasty (Āl Thānī) in the 19th century. The Thani dynasty sought British patronage against competing tribal groups and against the Ottoman Empire—which occupied the country in the late 19th and early 20th centuries—and in exchange the United Kingdom controlled Qatar’s foreign policy until the latter’s independence in 1971. Thereafter the monarchy continued to nurture close ties with Western powers as a central pillar of its national security. Qatar has one of the world’s largest reserves of petroleum and natural gas and employs large numbers of foreign workers in its production process. Because of its oil wealth, the country’s residents enjoy a high standard of living and a well-established system of social services. he capital is the eastern coastal city of Doha (Al-Dawḥah), which was once a centre for pearling and is home to most of the country’s inhabitants. Radiating inland from its handsome Corniche, or seaside boulevard, Doha blends premodern architecture with new office buildings, shopping malls, and apartment complexes. Qatar’s traditions draw on a nomadic past and practices that are centuries old, from hand-woven products to falconry. However, the country’s population is urban and coastal, its daily life is thoroughly modern, and its rulers have sought to enhance civil liberties. The press is among the freest in the region, and though they are religious and traditional, Qataris pride themselves on their tolerance for the cultures and beliefs of others. On the status of the country’s large expatriate community, the ruling emir has noted that “in Qatar, they find security and a dignified livelihood.” Land Slightly smaller in area than the U.S. state of Connecticut, the Qatar peninsula is about 100 miles (160 km) from north to south, 50 miles (80 km) from east to west, and is generally rectangular in shape. It shares a border with eastern Saudi Arabia where the peninsula connects to the mainland and is north and west of the United Arab Emirates. The island country of Bahrain lies some 25 miles (40 km) northwest of Qatar. A territorial dispute with Bahrain was resolved in 2001, when the International Court of Justice awarded the Ḥawār Islands (just off the coast of Qatar) to Bahrain and gave Qatar sovereignty over Janān Island and the ruined fortress-town of Al-Zubārah (on the Qatari mainland). That year Qatar also signed a final border demarcation agreement with Saudi Arabia. Relief and drainage Most of Qatar’s area is flat, low-lying desert, which rises from the east to a central limestone plateau. Hills rise to about 130 feet (40 metres) along the western and northern coasts, and Abū al-Bawl Hill (335 feet [103 metres]) is the country’s highest point. Sand dunes and salt flats, or sabkhahs, are the chief topographical features of the southern and southeastern sectors. Qatar has more than 350 miles (560 km) of coastline; its border with Saudi Arabia is some 37 miles (60 km) long. There are no permanent bodies of fresh water. Soils Soils in Qatar are marked by a small degree of organic material and are generally calcareous and agriculturally unproductive. Windblown sand dunes are common, and soil distribution over bedrock is light and uneven. Soil salinity is high in coastal regions and in agricultural regions where poor regulation of irrigation has led to increased salinity. Climate The climate is hot and humid from June to September, with daytime temperatures as high as 122 °F (50 °C). The spring and fall months—April, May, October, and November—are temperate, averaging about 63 °F (17 °C), and the winters are slightly cooler. Precipitation is scarce, with less than 3 inches (75 mm) falling annually (generally in winter). Plant and animal life Vegetation is found only in the north, where the country’s irrigated farming areas are located and where desert plants blossom briefly during the spring rains. Fauna is limited, and the government has implemented a program to protect the Arabian oryx, Qatar’s national animal. People - Ethnic groups and languages Qatar was originally settled by Bedouin nomads from the central part of the Arabian Peninsula. Qatari citizens, however, constitute only a small portion—roughly one-ninth—of the total population today. Economic growth beginning in the 1970s created an economy dependent on foreign workers—mostly from Pakistan, India, and Iran—who now far outnumber nationals. Few Qataris retain a nomadic lifestyle. Arabic is the official language, and most Qataris speak a dialect of Gulf Arabic similar to that spoken in surrounding states. Modern Standard Arabic is taught in schools, and English is commonly used. Among the large expatriate population, Persian and Urdu are often spoken. Religion Islam is the official religion, and Qataris are largely Sunni Muslims. There is a small Shiʿi minority. The ruling Thani family (Āl Thānī) adheres to the same Wahhābī interpretation of Islam as the rulers of Saudi Arabia, though not as strictly. Women, for example, have greater freedom in Qatar than in Saudi Arabia. The non-Qatari population has a more diverse religious makeup, with Muslims, Christians, and Hindus constituting the largest religious groups. More … Source: https://www.britannica.com/place/Qatar  

2022/12/18

National Day Anniversary of the election of the King of Bhutan

Bhutan, country of south-central Asia, located on the eastern ridges of the Himalayas. Historically a remote kingdom, Bhutan became less isolated in the second half of the 20th century, and consequently the pace of change began to accelerate. With improvements in transportation, by the early 21st century a trip from the Indian border to the Bhutanese capital, Thimphu, that once took six days by mule could be made in just a few hours by car along a winding mountain road from the border town of Phuntsholing. The governmental structure also changed radically. Reforms initiated by King Jigme Dorji Wangchuk (reigned 1952–72) in the 1950s and ’60s led to a shift away from absolute monarchy in the 1990s and toward the institution of multiparty parliamentary democracy in 2008. The economic core of Bhutan lies in the fertile valleys of the Lesser Himalayas, which are separated from one another by a series of high and complex interconnecting ridges extending across the country from north to south. The political nucleus of Bhutan is centred in the Paro and Thimphu valleys in the Lesser Himalayan region. Its location between the Assam-Bengal Plain of India to the south and the Plateau of Tibet of southwestern China to the north gives the country considerable geopolitical significance. Land Bhutan’s northern and western boundary with the Tibet Autonomous Region (part of China), although undefined, generally follows the crest of the Great Himalayas. In the Duars Plain to the south of the Himalayan range lies Bhutan’s boundary with the Indian states of West Bengal and Assam. Bhutan borders the Indian states of Arunachal Pradesh to the east and Sikkim to the southwest. Relief Physically, Bhutan may be divided into three regions from north to south: the Great Himalayas, the Lesser Himalayas, and the Duars Plain. The Great Himalayas The northern part of Bhutan lies within the Great Himalayas; the snowcapped peaks in this region reach an elevation of more than 24,000 feet (7,300 metres). High valleys occur at elevations of 12,000 to 18,000 feet (3,700 to 5,500 metres), running down from the great northern glaciers. Alpine pastures on the high ranges are used for grazing yaks in the summer months. To the north of the Great Himalayas are several “marginal” mountains of the Plateau of Tibet that form the principal watershed between the northward- and the southward-flowing rivers. A dry climate is characteristic of the Great Himalayan region. Until about 1960 the tempo of life in the Great Himalayas continued much as it had for centuries. Long relatively undisturbed in their ways, Bhutanese traders carried cloth, spices, and grains across the mountain passes into Tibet and brought back salt, wool, and sometimes herds of yaks. The absorption of Tibet by China, however, necessarily pushed Bhutan toward ending its isolation; the event brought major changes to the way of living in those high regions, as military precautions were taken to guard against the potential danger of a Chinese incursion from Tibet. The Lesser Himalayas Spurs from the Great Himalayas radiate southward, forming the ranges of the Lesser Himalayas (also called Inner Himalayas). The north-south ranges of the Lesser Himalayas constitute watersheds between the principal rivers of Bhutan. Differences in elevation and the degree of exposure to moist southwest monsoon winds determine the prevailing vegetation, which ranges from dense forest on the rain-swept windward slopes to alpine vegetation at higher elevations. Several fertile valleys of central Bhutan are in the Lesser Himalayas at elevations varying from 5,000 to 9,000 feet (1,500 to 2,700 metres). These valleys, notably the Paro, Punakha, Thimphu, and Ha, are relatively broad and flat, receive moderate rainfall (from 40 to 50 inches [about 1,000 to 1,270 mm] or less a year), and are fairly well populated and cultivated. The Duars Plain South of the Lesser Himalayas and the foothills lies the narrow Duars Plain, which forms a strip 8 to 10 miles (12 to 16 km) wide along the southern border of Bhutan. The Himalayan ranges rise sharply and abruptly from this plain, which constitutes a gateway to the strategic mountain passes (known as dwars or dooars) that lead into the fertile valleys of the Lesser Himalayas. Subject to abundant rainfall (200 to 300 inches [5,100 to 7,600 mm] a year), the entire Duars tract is hot and steamy and is covered with dense semitropical forest and undergrowth. The northern part of the Duars, immediately bordering the mountains, consists of a rugged, irregular, and sloping surface. At the foot of the mountains, small villages are found in forest clearings, but most of the area is thickly covered with vegetation inhabited by an array of large wild animals. The southern part of the Duars, bordering India, is mostly covered with savanna (grassy parkland) and bamboo jungle. In many areas the savannas have been cleared for rice cultivation. The principal trade routes between central Bhutan and India follow the valleys of the main rivers. Drainage Bhutan’s mountainous territory is dissected by numerous rivers. The main rivers from west to east are the Torsa (Amo), Wong (Raidak), Sankosh (Mo), and Manas. All the rivers flow southward from the Great Himalayas and join the Brahmaputra River in India. Climate of Bhutan Bhutan’s climate is perhaps more diverse than that of any other similarly sized area in the world. The climate changes with elevation, producing striking meteorologic contrasts, and differing exposures to sunlight and moisture-laden winds result in complex local variations. Three principal climatic regions can be distinguished: the hot, humid, subtropical tract of the Duars Plain and its adjacent foothills; the cooler region of the Lesser Himalayas; and the alpine tundra region of the Great Himalayas. A temperate climate occurs only in the central mountain valleys. For instance, in Thimphu, in the country’s west-central region, in January, high temperatures are usually in the low 50s F (about 12 °C) and low temperatures in the mid-30s F (about 2 °C); in July, Thimphu’s temperatures are somewhat warmer, typically rising to the mid-60s F (about 19 °C) and dropping to the mid-50s F (about 13 °C). The remainder of the country experiences either extreme heat, as in the Duars, or extreme cold, as in the north. More … Source: https://www.britannica.com/place/Bhutan

2022/12/17