Naadam National Day of Mongolia

Mongolia, historically Outer Mongolia, country located in north-central Asia. It is roughly oval in shape, measuring 1,486 miles (2,392 km) from west to east and, at its maximum, 782 miles (1,259 km) from north to south. Mongolia’s land area is roughly equivalent to that of the countries of western and central Europe, and it lies in a similar latitude range. The national capital, Ulaanbaatar (Mongolian: Ulan Bator) is in the north-central part of the country. Landlocked Mongolia is located between Russia to the north and China to the south, deep within the interior of eastern Asia far from any ocean. The country has a marked continental climate, with long cold winters and short cool-to-hot summers. Its remarkable variety of scenery consists largely of upland steppes, semideserts, and deserts, although in the west and north forested high mountain ranges alternate with lake-dotted basins. Mongolia is largely a plateau, with an average elevation of about 5,180 feet (1,580 metres) above sea level. The highest peaks are in the Mongolian Altai Mountains (Mongol Altain Nuruu) in the southwest, a branch of the Altai Mountains system.Some three-fourths of Mongolia’s area consists of pasturelands, which support the immense herds of grazing livestock for which the country is known. The remaining area is about equally divided between forests and barren deserts, with only a tiny fraction of the land under crops. With a total population of fewer than three million, Mongolia has one of the lowest average population densities of any country in the world.The Mongols have a long prehistory and a most remarkable history. The Huns, a people who lived in Central Asia from the 3rd to the 1st century bce, may have been their ancestors. A united Mongolian state of nomadic tribes was formed in the early 13th century ce by Genghis Khan, and his successors controlled a vast empire that included much of China, Russia, Central Asia, and the Middle East. The Mongol empire eventually collapsed and split up, and from 1691 northern Mongolia was colonized by Qing (Manchu) China. With the collapse of Qing rule in Mongolia in 1911/12, the Bogd Gegeen (or Javzandamba), Mongolia’s religious leader, was proclaimed Bogd Khan, or head of state. He declared Mongolia’s independence, but only autonomy under China’s suzerainty was achieved. From 1919, nationalist revolutionaries, with Soviet assistance, drove out Chinese troops attempting to reoccupy Mongolia, and in 1921 they expelled the invading White Russian cavalry. July 11, 1921, then became celebrated as the anniversary of the revolution. The Mongolian People’s Republic was proclaimed in November 1924, and the Mongolian capital, centred on the main monastery of the Bogd Gegeen, was renamed Ulaanbaatar (“Red Hero”). From 1921 until the end of the 1980s, Mongolia was a one-party state closely tied to the Soviet Union. It received technical, economic, and military assistance from the Soviet Union and generally followed Soviet guidance in political and economic matters and in the building of a socialist society. However, beginning in 1990, forces for change in Mongolia ended the monopoly of political power by the communists in favour of free multiparty elections, coalition government, a new constitution, greater cultural and religious freedom with more emphasis on Mongol national traditions, a neutral position in international relations, and a transition to a market economy. Land - Relief Mongolia can be divided into three major topographic zones: the mountain chains that dominate the northern and western areas, the basin areas situated between and around them, and the enormous upland plateau belt that lies across the southern and eastern sectors. The entire country is prone to seismic movements, and some earthquakes are extremely severe. Their effects, however, are limited by the low population density. The mountains There are three major mountain chains in Mongolia: the Mongolian Altai Mountains, the Khangai Mountains (Khangain [or Hangayn] Nuruu), and the Khentii Mountains (Khentiin [or Hentiyn] Nuruu). The Mongolian Altai in the west and southwest constitute the highest and the longest of these chains. Branching southeastward from the main Altai range at the northwestern border with Russia, the Mongolian Altai stretch southeastward for some 250 miles (400 km) along the Chinese border before turning slightly more eastward for another 450 miles (725 km) in southwestern Mongolia. The range—the only one in the country where contemporary glaciation has developed—reaches an elevation of 14,350 feet (4,374 metres) at Khüiten Peak (Nayramadlyn Orgil) at the western tip of the country, Mongolia’s highest point. Extending eastward from the Mongolian Altai are the Gobi Altai Mountains (Govi Altain Nuruu), a lesser range of denuded hills that lose themselves in the expanses of the Gobi. The Khangai Mountains, also lying from northwest to southeast, form a solid mountain mass near the centre of the country. The range’s peaks reach some 12,000 feet (3,700 metres), with Otgontenger, the highest, rising to some 13,200 feet (4,025 metres) in the northwest. Characteristic of the Khangai are gentle slopes covered with fine pastureland. To the north the Eastern Sayan Mountains of Siberia lie along the border with Russia. The alignment of the third mountain chain, the Khentii range of northeastern Mongolia, is southwest to northeast, extending into Siberia. The highest peak is Asraltkhairkhan, which reaches about 9,200 feet (2,800 metres), but, in general, maximum elevations are about 7,000 feet (2,130 metres). Ulaanbaatar lies at the southwestern edge of the range. The Da Hinggan (Greater Khingan) Range rises along and beyond the eastern frontier with China. The northern intermontane basins Around and between the main ranges lie an important series of basins. The Great Lakes region, with more than 300 lakes, is tucked between the Mongolian Altai, the Khangai, and the mountains along the border with Siberia. Another basin lies between the eastern slopes of the Khangai Mountains and the western foothills of the Khentii range. The southern part of it—the basins of the Tuul and Orkhon (Orhon) rivers—is a fertile region important in Mongolian history as the cradle of settled ways of life. The remarkable Khorgo region, on the northern flanks of the Khangai Mountains, has a dozen extinct volcanoes and numerous volcanic lakes. Swift and turbulent rivers have cut jagged gorges. The source stream of the Orkhon River is in another volcanic region, with deep volcanic vents and hot springs. Near the northern border, Lake Khövsgöl (Hövsgöl) is the focus of another rugged region that is noted for its marshlands.More … Score: https://www.britannica.com/place/Mongolia

2021/07/11

Independence Day of the Commonwealth of the Bahamas

The Bahamas, archipelago and country on the northwestern edge of the West Indies. Formerly a British colony, The Bahamas became an independent country within the Commonwealth in 1973. The name Bahamas is of Lucayan Taino (Arawakan) derivation, although some historians believe it is from the Spanish bajamar, meaning “shallow water.” The islands occupy a position commanding the gateway to the Gulf of Mexico, the Caribbean Sea, and the entire Central American region. Their strategic location has given the history of The Bahamas a unique and often striking character. It was there that Christopher Columbus made his original landfall in the Americas. The subsequent fate of the peaceful original inhabitants remains one of the more tragic episodes in the development of the entire region, while the early attempts at European-dominated settlement were marked by intense national rivalries, interspersed with long periods of lawlessness and piracy. As a result, the society and culture that has evolved in The Bahamas is a distinctive blend of European and African heritages, the latter a legacy of the slave trade and the introduction of the plantation system using African slaves. The islands, lacking natural resources other than their agreeable climate and picturesque beaches, have become heavily dependent on the income generated by the extensive tourist facilities and the financial sector that have been developed, often as a result of the injection of foreign capital. The continued popularity of the islands with tourists, largely from North America, has helped to maintain a relatively high standard of living among the population, most of whom are of African descent. The capital, Nassau, is located on small but important New Providence Island. Land Lying to the north of Cuba and Hispaniola, the archipelago comprises nearly 700 islands and cays, only about 30 of which are inhabited, and more than 2,000 low, barren rock formations. It stretches more than 500 miles (800 km) southeast-northwest between Grand Bahama Island, which has an area of 530 square miles (1,373 square km) and lies about 60 miles (100 km) off the southeastern coast of the U.S. state of Florida, and Great Inagua Island, some 50 miles (80 km) from the eastern tip of Cuba. The islands other than New Providence are known collectively as the Out (Family) Islands. They include Grand Bahama, which contains the major settlements of Freeport and West End; Andros (2,300 square miles [6,000 square km]), the largest island of The Bahamas; Abaco, or Great Abaco, (372 square miles [963 square km]); and Eleuthera (187 square miles [484 square km]), the site of one of the early attempts at colonization. Relief and soils The Bahamas occupies an irregular submarine tableland that rises out of the depths of the Atlantic Ocean and is separated from nearby lands to the south and west by deepwater channels. Extensive areas of flatland, generally a few feet in elevation, are the dominant topographic features of the major islands; the Bimini group (9 square miles [23 square km]), for example, has a maximum elevation of only 20 feet (6 metres). A number of islands fronting the Atlantic have a range or series of ranges of hills on the northeastern side that parallel the longer axes of the islands. These ranges are formed of sand washed ashore and blown inland by the trade winds. The newer hills adjacent to the seashore are normally sand dunes. Solidity increases toward the interior, where the particles become cemented to form Bahama limestone. Eleuthera and Long Island (230 square miles [596 square km]) have the greatest number of hills exceeding 100 feet (30 metres). The highest point in The Bahamas, Mount Alvernia, at 206 feet (63 metres), is on Cat Island (150 square miles [388 square km]). Beneath the soil, the islands are composed of limestone rock and skeletal remains of coral fossils and other marine organisms. There are no rivers, but several islands—particularly New Providence, San Salvador (63 square miles [163 square km]), and Great Inagua—have large lakes. There is abundant fresh water on Andros Island. Climate of the The Bahamas The Bahamian climate, mild throughout the year, is one of the great attractions of the area. The average temperature varies from the low 70s F (about 21 °C) during the winter to the low 80s F (about 27 °C) during the summer, and extremes seldom fall below the low 60s F (about 16 °C) or rise above the low 90s F (about 32 °C). The average annual rainfall is about 44 inches (1,120 mm), occurring mostly during the summer months. Prevailing winds, coming from the northeast in winter and from the southeast in summer, lend a cooling influence to a generally humid atmosphere. Tropical cyclones (hurricanes) pose a threat during the period from June to November and have occasionally caused great destruction. Plant and animal life Extensive and beautiful forests of Caribbean pine are found on Grand Bahama, Abaco, Andros, and New Providence islands. Hardwood forests also occur on some of the islands. Elsewhere the woody vegetation consists mostly of shrubs and low trees. Animal life is dominated by frogs, lizards, and snakes, all of them nonpoisonous, and several species of bats are found in caves along the more rocky coasts. Larger animals include the agouti, a rodent; the raccoon; the iguana; and the elegant flamingo, the national bird. All of these have been much reduced in numbers and in distribution. In addition, several animals—notably sheep, horses, and other livestock—have been introduced from Europe. The surrounding waters abound with fish and other edible marine animals, such as conch and spiny lobster (crayfish). More … Score: https://www.britannica.com/place/The-Bahamas  

2021/07/10

With a visit to the exhibition “The world or Rembrandt’

Ambassador Daphne Bergsma had the honor to be guided through the most interesting exhibition ‘Different Perspectives’ by the curator Ms. Alexandra Janiszewska. The exhibition of 17th century Dutch and Flemish art is on view until July 25th at the National Museum. We recommend to combine a visit to the National Museum with a visit to the exhibition “The world or Rembrandt’ which opened last Monday at the Royal Castle in Warsaw.

2021/07/09

Wizyta Ambasadora Królestwa Belgii w Domu Pomocy Społecznej w Trzebiechowie

W dniu 28 czerwca 2021 r., w Domu Pomocy Społecznej w Trzebiechowie, odbyło się spotkanie Starosty Zielonogórskiego Krzysztofa Romankiewicza oraz Wójt Gminy Trzebiechów Izabelli Staszak z Ambasadorem Królestwa Belgii Lucem Jacobsem. W spotkaniu uczestniczyli również Wicedyrektor Domu Przemysław Żurawiecki, Główna Księgowa Iwona Tyrcz oraz tłumacz Pani Dorota Krzyżyńska. Pan Ambasador zwiedził nasze zabytki w tym Dom Pomocy Społecznej i dzieło Henrego van de Velde, Pałac oraz halę gimnastyczną. Była to pierwsza i nie ostatnia wizyta Ambasadora.

2021/07/09

Ósma rocznica członkostwa Republiki Chorwacji w Unii Europejskiej

Stając się członkiem europejskiej rodziny, Chorwacja osiągnęła jeden ze swoich głównych celów polityki zagranicznej, co pozwoliło nam żyć w jednej z najbardziej zaawansowanych społeczności na świecie. Unia Europejska opiera się na wartościach, które podziela sama Chorwacja, a członkostwo bazuje na solidarności między państwami Unii i daje nam jasne i konkretne korzyści.

2021/07/09

Wizyta Ambasadora Japonii w Polsce na UMCS

W środę, 30 czerwca 2021 roku gościliśmy w naszej Alma Mater JE Ambasadora Japonii w Polsce pana Akio Miyajima wraz z panią Tae Sato-Takita, Drugą Sekretarz w Dziale Ekonomii Ambasady Japonii. Gościom towarzyszyła pani Elżbieta Korona – tłumacz i urzędnik z Działu Ekonomii Ambasady Japonii.

2021/07/09

Independence Day of the Republic of South Sudan

South Sudan, also called Southern Sudan, country located in northeastern Africa. Its rich biodiversity includes lush savannas, swamplands, and rainforests that are home to many species of wildlife. Prior to 2011, South Sudan was part of Sudan, its neighbour to the north. South Sudan’s population, predominantly African cultures who tend to adhere to Christian or animist beliefs, was long at odds with Sudan’s largely Muslim and Arab northern government. South Sudan’s capital is Juba. South Sudan was settled by many of its current ethnic groups during the 15th–19th centuries. After the Sudan region was invaded in 1820 by Muḥammad ʿAlī, viceroy of Egypt under the Ottoman Empire, the southern Sudan was plundered for slaves. By the end of the 19th century the Sudan was under British-Egyptian rule. Although the north accepted British rule relatively quickly, there was greater resistance in the south. Because of this, British energies in the north were free to be directed toward modernization efforts, whereas in the south they were more focused on simply maintaining order, leading to a dichotomy of development between north and south that continued for several decades. After Sudan became independent in 1956, numerous governments over the years found it difficult to win general acceptance from the country’s diverse political constituencies, especially in the south. An early conflict arose between those northern leaders who hoped to impose the vigorous extension of Islamic law and culture to all parts of the country and those who opposed this policy. The latter group included the majority of southern Sudan’s population, many of whom were already up in arms over fears that the south would be further marginalized by the northern-based government; those fears led to a lengthy civil war (1955–72). The Addis Ababa Agreement of 1972 ended the conflict only temporarily, and in the next decade widespread fighting resumed with the second civil war (1983–2005). Numerous discussions, cease-fires, and agreements between southern leaders and their northern counterparts occurred but yielded very little success until the 2005 Comprehensive Peace Agreement (CPA), which ended warfare and generated an outline of new measures to share power, distribute wealth, and provide security in Sudan. Significantly, it also granted southern Sudan semiautonomous status and stipulated that a referendum on independence for the region would be held in six years. Despite some obstacles, the eagerly awaited referendum did take place: a weeklong vote on independence for southern Sudan was held January 9–15, 2011, with the results indicating the south’s overwhelming preference to secede. The country of South Sudan declared independence on July 9, 2011. Land South Sudan is bounded on the north by Sudan; on the east by Ethiopia; on the south by Kenya, Uganda, and the Democratic Republic of the Congo; and on the west by the Central African Republic. Relief South Sudan’s vast plains and plateaus are drained by the Nile River and its tributaries. This river system runs from south to north across the entire length of the east-central part of the country. At the heart of the country is a clay plain, the centre of which is occupied by an enormous swampy region known as Al-Sudd (the Sudd). There are two contrasting upland areas. The Ironstone Plateau lies between the Nile-Congo watershed and the clay plain; its level country is marked with inselbergs (isolated hills rising abruptly from the plains). On the Uganda border there are massive ranges with peaks rising to more than 10,000 feet (3,000 metres). The Imatong Mountains contain Mount Kinyeti (elevation 10,456 feet [3,187 metres]), the highest point in South Sudan. Drainage and soils The Nile River system is the dominant physical feature, and all streams and rivers of South Sudan drain either into or toward the Nile. The White Nile (Baḥr Al-Abyaḍ) enters the country as the Mountain Nile (Baḥr Al-Jabal) from the south through rapids at Nimule on the Uganda border. After its confluence with the left- (west-) bank tributary known as the Baḥr Al-Ghazāl, the Mountain Nile becomes the White Nile. A little farther north along its course, the White Nile receives much of its water from the right-bank Sobat River, which flows from the Ethiopian Plateau to join the Nile near Malakal. Drainage in the country does not always reach the Nile rivers; the rivers of the southwest, for example, infrequently reach the Baḥr Al-Ghazāl system. In 1978 construction began on the Jonglei (Junqalī) Canal, which was planned to bypass Al-Sudd swamp and provide a straight well-defined channel for the Mountain Nile River to flow northward until its junction with the White Nile. It also would have drained the swamplands of the Sudd for agricultural use. The project was suspended in 1983 because of disruptions arising from the civil war between the north and the south. After the CPA was signed in 2005, there was discussion about resuming work on the canal, spearheaded by the Egyptian government and Sudan’s Khartoum government, although the government of southern Sudan (GoSS) was hesitant to embrace the project and deferred making a decision about it until they could give the matter further study; a decision had not been made at the time of independence. The southern plains consist of an alkaline soil that is a heavy cracking clay. The clays of Al-Sudd were deposited in the area of impeded drainage. Climate of South Sudan South Sudan has a tropical climate with wet and dry seasons. The seasons are characterized by the oscillation, north and south, of the boundary between moist southerly air and dry northerly air. This phenomenon, more specifically, involves the seasonal migration and pulsation of the northern tropical continental air mass and the southern maritime continental air mass, which are divided by the intertropical convergence zone. In winter the north winds of the tropical air mass blow across the country toward the front, which may be as far south as the Tropic of Capricorn. These winds are relatively cool and dry and usually bring no rain. By April the front begins to move northward, and the moist southerly air of the maritime air mass is drawn in from the South Atlantic Ocean. Because of this, South Sudan has a rainy season, the total length of which varies according to latitude and is generally no more than eight to nine months a year, beginning as early as April and continuing as late as December. South Sudan’s lowest annual temperatures are in the high 60s to high 70s F (low to mid-20s C) in the centre and north of the country, while the lowest annual temperatures in the outlying areas are slightly cooler, about high 50s to high 60s F (mid-10s to low 20s C). The highest annual temperatures for most of South Sudan generally range from the mid-80s to the mid-90s F (low to mid-30s C), although some areas toward the north of the country range from the mid-90s to mid-100s F (mid- to upper 30s C). The highest temperatures normally occur just before the rainy season. In South Sudan, most precipitation usually occurs during the summer months and varies across the country. The majority of the country receives about 30–40 inches (750–1,000 mm) annually. Areas in the western part of the country receive slightly more, about 40–60 inches (1,000–1,500 mm) annually, while some areas in the northeastern and southeastern parts of the country receive less, about 20–30 inches (500–750 mm). Some areas in the extreme southeast receive fewer than 20 inches (500 mm). More … Score: https://www.britannica.com/place/South-Sudan

2021/07/09

100. rocznica nawiązania polsko-łotewskich stosunków dyplomatycznych

Dnia 30 czerwca 2021 r. została wprowadzona do obiegu kartka pocztowa z nadrukowanym znakiem opłaty pocztowej, emisji: "100. rocznica nawiązania polsko-łotewskich stosunków dyplomatycznych". Dziękujemy Poczcie Polskiej za współpracę!

2021/07/08

Spotkanie Ambasador Wielkiej Brytanii z pracownikami UAM

W piątek 18 czerwca 2021 pracownicy i studenci Uniwersytetu im. Adama Mickiewicza w Poznaniu wzięli udział w śniadaniu z JE Anną Louise Clunes – Ambasador Zjednoczonego Królestwa Wielkiej Brytanii i Irlandii Północnej w Polsce. Spotkanie odbyło się w Hotelu Mercure na zaproszenie Ambasady Brytyjskiej w Polsce, w towarzystwie Konsula Honorowego Włodzimierza Walkowiaka.

2021/07/08