National Day of the Federal Democratic Republic of Nepal

Nepal, country of Asia, lying along the southern slopes of the Himalayan mountain ranges. It is a landlocked country located between India to the east, south, and west and the Tibet Autonomous Region of China to the north. Its territory extends roughly 500 miles (800 kilometres) from east to west and 90 to 150 miles from north to south. The capital is Kathmandu. Nepal, long under the rule of hereditary prime ministers favouring a policy of isolation, remained closed to the outside world until a palace revolt in 1950 restored the crown’s authority in 1951; the country gained admission to the United Nations in 1955. In 1991 the kingdom established a multiparty parliamentary system. In 2008, however, after a decadelong period of violence and turbulent negotiation with a strong Maoist insurgency, the monarchy was dissolved, and Nepal was declared a democratic republic. Wedged between two giants, India and China, Nepal seeks to keep a balance between the two countries in its foreign policy—and thus to remain independent. A factor that contributes immensely to the geopolitical importance of the country is the fact that a strong Nepal can deny China access to the rich Gangetic Plain; Nepal thus marks the southern boundary of the Chinese sphere north of the Himalayas in Asia. As a result of its years of geographic and self-imposed isolation, Nepal is one of the least developed nations of the world. In recent years many countries, including India, China, the United States, the United Kingdom, Japan, Denmark, Germany, Canada, and Switzerland, have provided economic assistance to Nepal. The extent of foreign aid to Nepal has been influenced to a considerable degree by the strategic position of the country between India and China. Land - Relief Nepal contains some of the most rugged and difficult mountain terrain in the world. Roughly 75 percent of the country is covered by mountains. From the south to the north, Nepal can be divided into four main physical belts, each of which extends east to west across the country. These are, first, the Tarai, a low, flat, fertile land adjacent to the border of India; second, the forested Churia foothills and the Inner Tarai zone, rising from the Tarai plain to the rugged Mahābhārat Range; third, the mid-mountain region between the Mahābhārat Range and the Great Himalayas; and, fourth, the Great Himalaya Range, rising to more than 29,000 feet (some 8,850 metres). The Tarai forms the northern extension of the Gangetic Plain and varies in width from less than 16 to more than 20 miles, narrowing considerably in several places. A 10-mile-wide belt of rich agricultural land stretches along the southern part of the Tarai; the northern section, adjoining the foothills, is a marshy region in which wild animals abound and malaria is endemic. The Churia Range, which is sparsely populated, rises in almost perpendicular escarpments to an altitude of more than 4,000 feet. Between the Churia Range to the south and the Mahābhārat Range to the north, there are broad basins from 2,000 to 3,000 feet high, about 10 miles wide, and 20 to 40 miles long; these basins are often referred to as the Inner Tarai. In many places they have been cleared of the forests and savanna grass to provide timber and areas for cultivation. A complex system of mountain ranges, some 50 miles in width and varying in elevation from 8,000 to 14,000 feet, lie between the Mahābhārat Range and the Great Himalayas. The ridges of the Mahābhārat Range present a steep escarpment toward the south and a relatively gentle slope toward the north. To the north of the Mahābhārat Range, which encloses the valley of Kathmandu, are the more lofty ranges of the Inner Himalaya (Lesser Himalaya), rising to perpetually snow-covered peaks. The Kathmandu and the Pokharā valleys lying within this mid-mountain region are flat basins, formerly covered with lakes, that were formed by the deposition of fluvial and fluvioglacial material brought down by rivers and glaciers from the enclosing ranges during the four glacial and intervening warm phases of the Pleistocene Epoch (from about 2,600,000 to 11,700 years ago). The Great Himalaya Range, ranging in elevation from 14,000 to more than 29,000 feet, contains many of the world’s highest peaks—Everest, Kānchenjunga I, Lhotse I, Makālu I, Cho Oyu, Dhaulāgiri I, Manāslu I, and Annapūrna I—all of them above 26,400 feet. Except for scattered settlements in high mountain valleys, this entire area is uninhabited. Drainage The Kathmandu Valley, the political and cultural hub of the nation, is drained by the Bāghmati River, flowing southward, which washes the steps of the sacred temple of Paśupatinātha (Pashupatinath) and rushes out of the valley through the deeply cut Chhobar gorge. Some sandy layers of the lacustrine beds act as aquifers (water-bearing strata of permeable rock, sand, or gravel), and springs occur in the Kathmandu Valley where the sands outcrop. The springwater often gushes out of dragon-shaped mouths of stone made by the Nepalese; it is then collected in tanks for drinking and washing and also for raising paddy nurseries in May, before the monsoon. Drained by the Seti River, the Pokharā Valley, 96 miles west of Kathmandu, is also a flat lacustrine basin. There are a few remnant lakes in the Pokharā basin, the largest being Phewa Lake, which is about two miles long and nearly a mile wide. North of the basin lies the Annapūrna massif of the Great Himalaya Range. The major rivers of Nepal—the Kosi, Nārāyani (Gandak), and Karnāli, running southward across the strike of the Himalayan ranges—form transverse valleys with deep gorges, which are generally several thousand feet in depth from the crest of the bordering ranges. The watershed of these rivers lies not along the line of highest peaks in the Himalayas but to the north of it, usually in Tibet. The rivers have considerable potential for development of hydroelectric power. Two irrigation-hydroelectric projects have been undertaken jointly with India on the Kosi and Nārāyani rivers. Discussions have been held to develop the enormous potential of the Karnāli River. A 60,000-kilowatt hydroelectric project at Kulekhani, funded by the World Bank, Kuwait, and Japan, began operation in 1982. In the upper courses of all Nepalese rivers, which run through mountain regions, there are little or no flood problems. In low-lying areas of the Tarai plain, however, serious floods occur. The rivers and small streams of the Tarai, especially those in which the dry season discharge is small, are polluted by large quantities of domestic waste thrown into them. Towns and villages have expanded without proper provision for sewage disposal facilities, and more industries have been established at selected centres in the Tarai. The polluted surface water in the Kathmandu and Pokharā valleys, as well as in the Tarai, are unacceptable for drinking. Climate of Nepal Nepal’s climate, influenced by elevation as well as by its location in a subtropical latitude, ranges from subtropical monsoon conditions in the Tarai, through a warm temperate climate between 4,000 and 7,000 feet in the mid-mountain region, to cool temperate conditions in the higher parts of mountains between 7,000 and 11,000 feet, to an Alpine climate at altitudes between 14,000 and 16,000 feet along the lower slopes of the Himalaya mountains. At altitudes above 16,000 feet the temperature is always below freezing and the surface covered by snow and ice. Rainfall is ample in the eastern portion of the Tarai (which receives from 70 to 75 inches [1,800 to 1,900 millimetres] a year at Bīratnagar) and in the mountains, but the western portion of Nepal (where from 30 to 35 inches a year fall at Mahendranagar) is drier. In Kathmandu Valley, average temperatures range from 50° F (10° C) in January to 78° F (26° C) in July, and the lowest and highest temperatures recorded have been 27° and 99° F (-3° and 37° C). The average annual rainfall is about 55 inches, most of which falls in the period from June to September. At Pokharā the temperature ranges from 40° F (4° C) in January to approximately 100° F (38° C) in June, just before the monsoon. In winter, temperatures during the day rise to 70° F (21° C), creating pleasant conditions, with cool nights and warm days. Because warm rain-bearing monsoon winds discharge most of their moisture as they encounter the Annapūrna range, rainfall is quite heavy (about 100 inches) in the Pokharā Valley. More … Score: https://www.britannica.com/place/Nepal

2022/09/20

Independence Day Federation St. Kitts and Nevis

Saint Kitts and Nevis, officially Federation of Saint Kitts and Nevis, also called Saint Christopher and Nevis, state composed of two islands of the Lesser Antilles in the eastern Caribbean Sea. Their combined area is 104 square miles (269 square km). The capital is Basseterre on the island of Saint Kitts. Land Saint Kitts is 23 miles (37 km) long and 5 miles (8 km) wide, is oval in shape, and has an area of 68 square miles (176 square km). A volcanic mountainous ridge down the centre forms a semicircle around a plain in the southeast. Mount Liamuiga (formerly Mount Misery), with a lake in its forested crater, is the highest point (3,792 feet [1,156 metres]). The soil—except in the mountains—is light and porous. Most of the beaches are of black volcanic sands. The island is well watered and fertile, with warm summers and somewhat cooler winters. The average summer temperature is about 86 °F (30 °C) and the average winter temperature about 81 °F (27 °C). The annual precipitation averages 55 inches (1,397 mm), and the rainy season is from May to November. Nevis, surrounded by coral reefs, lies 2 miles (3 km) southeast of Saint Kitts across a channel known as The Narrows. The island is circular, and it consists almost entirely of a mountain, Nevis Peak (3,232 feet [985 metres]), which is flanked by the lower Round Hill (1,014 feet [309 metres]) on the north and by Saddle Hill (1,850 feet [564 metres]) on the south. Its area is 36 square miles (93 square km). The soil of Nevis is clay studded with volcanic boulders. The climate is similar to that of Saint Kitts. Both Nevis and Saint Kitts lie in a tropical hurricane (tropical cyclone) belt; hurricane season is between August and October. People The population is largely black, with a small mulatto (of mixed African and white heritage) minority. There are also very small South Asian and white groups. More than two-thirds of the population lives in rural areas. The official language is English. The main religious denominations are Anglican and Methodist, with a smaller number of Roman Catholics. Both Saint Kitts and Nevis have traditionally had high levels of emigration, offsetting natural increases and enabling the islands to maintain a fairly stable population. About two-thirds of the population is between the ages of 15 and 59. Economy The cultivation of sugarcane—once a nationalized industry and the mainstay of the Saint Kitts and Nevis economy—ceased in 2005 following a decline in overseas markets. It was replaced by tourism as the most-important economic sector. Crops now cultivated include vegetables and fruits, chiefly coconuts. The Eastern Caribbean Central Bank serves as the country’s monetary authority, and the Eastern Caribbean dollar is the official currency. Light industries in Saint Kitts and Nevis produce items mainly for export from imported materials. Products include electronic equipment, batik-dyed fabrics, and other clothing and furniture. Remittances from emigrants form an important source of foreign exchange. The United States, the United Kingdom, and Trinidad and Tobago are the principal trading partners. There is a deepwater port at Basseterre, and each island has an international airport; Robert L. Bradshaw International Airport, is on Saint Kitts, and Vance Amory International Airport, is on Nevis. Government and society Since independence in 1983, the Federation of Saint Kitts and Nevis has been an independent member of the Commonwealth, with the British monarch as its head of state. An appointed governor-general represents the crown. The prime minister, who together with other ministers is a member of the cabinet, is the head of government. The monarch and the National Assembly constitute the parliament, some of whose members are appointed. The island of Nevis enjoys a certain amount of autonomy within the federal structure; it has its own premier and legislature, and the constitution provides for it to secede from the federation if certain procedures are followed. There is universal adult suffrage. Education is compulsory for all children from the age of 5 to 16, provided by a countrywide system of free public schools as well as private church-affiliated schools. There are several hospitals and many health centres throughout the islands. Tropical diseases have been virtually eliminated. Most of the state’s cultural activity is concentrated in the capital, Basseterre. History of Saint Kitts and Nevis - Early settlement Christopher Columbus visited Saint Kitts on his second voyage in 1493 and found it inhabited by Carib people. He named it Saint Christopher for his patron saint. The name was shortened to Saint Kitts by settlers under Sir Thomas Warner, who, arriving from England in 1623, established the first successful English colony in the West Indies at Old Road on the west coast. The French first arrived on the island in 1625 and established a colony of their own in 1627 under Pierre Bélain, sieur d’Esnambuc. Divided during the 17th century between warring French and English colonists, Saint Kitts was given to Britain by the Treaty of Utrecht of April 1713 and remained in British possession despite the capture in 1782 of Brimstone Hill by the French. The island was restored to Great Britain by the Peace of Paris treaty signed by Britain and France at Versailles in 1783. Nevis was also sighted by Columbus in 1493. The island’s name derives from Columbus’s description of the clouds atop Nevis Peak as las nieves, or “the snows,” when he sighted the island. It was settled by the English in 1628 and soon became one of the most prosperous of the Antilles. Although it suffered from French and Spanish attacks in the 17th and 18th centuries, it maintained a sound economic position until the mid-19th century. Federation and independence movements The islands of Saint Kitts, Nevis, and Anguilla were united by federal act in 1882 and became an independent state in association with the United Kingdom on February 27, 1967. The islands were granted full internal self-government, with the United Kingdom retaining responsibility for defense and foreign affairs. After the islands had assumed the status of associated states, Anguilla complained of domination by the Saint Kitts administration. In May 1967 the Anguillans ejected the Saint Kitts police and established their own council. In July of the same year, they proclaimed their independence. After unsuccessful negotiations, the Anguilla Act of July 1971 placed Anguilla directly under British control. On February 10, 1976, Anguilla was granted a constitution, and its union with Saint Kitts and Nevis was formally severed in 1980. A constitutional conference was held in London in 1982, and, in spite of disagreement over special provisions for Nevis, Saint Kitts and Nevis became independent on September 19, 1983. A drop in world sugar prices hurt the nation’s economy through the mid-1980s, and the government sought to reduce the islands’ dependence on sugar production and to diversify the economy. Kennedy Simmonds, the first prime minister of the independent Saint Kitts and Nevis, remained in office until 1995, when his People’s Action Movement was defeated decisively by the Saint Kitts–Nevis Labour Party (SKNLP). One of the early issues in the administration of the new prime minister, SKNLP leader Denzil Douglas, was a secession movement on Nevis. A referendum was held there in 1998 on the question of independence for the island, but it fell short of the two-thirds majority needed to secede. The nationalized sugar industry continued to slump and, after years of operating it at a loss, the government closed it down after the 2005 harvest. Tourism and the hosting of offshore financial and service companies became the leading income producers in the country’s economy. Douglas won reelection in 2000, 2004, and 2010 but was defeated in 2015 by Team Unity, a coalition of opposition parties led by former foreign minister Timothy Harris, who became the new prime minister. More … Score: https://www.britannica.com/place/Saint-Kitts-and-Nevis

2022/09/19

Independence Day of the Republic of Chile

Chile, country situated along the western seaboard of South America. It extends approximately 2,700 miles (4,300 km) from its boundary with Peru, at latitude 17°30′ S, to the tip of South America at Cape Horn, latitude 56° S, a point only about 400 miles north of Antarctica. A long, narrow country, it has an average width of only about 110 miles, with a maximum of 217 miles at the latitude of Antofagasta and a minimum of 9.6 miles near Puerto Natales. It is bounded on the north by Peru and Bolivia, on its long eastern border by Argentina, and on the west by the Pacific Ocean. Chile exercises sovereignty over Easter Island, the Juan Fernández Archipelago, and the volcanic islets of Sala y Gómez, San Félix, and San Ambrosio, all of which are located in the South Pacific. Chile also claims a 200-mile offshore limit. The capital is Santiago. Chile’s relief is for the most part mountainous, with the Andes range dominating the landscape. Because of the country’s extreme length it has a wide variety of climates, from the coastal desert beginning in the tropical north to the cold subantarctic southern tip. Chile is also a land of extreme natural events: volcanic eruptions, violent earthquakes, and tsunamis originating along major faults of the ocean floor periodically beset the country. Fierce winter storms and flash floods alternate with severe summer droughts. Much of northern Chile is desert; the central part of the country is a temperate region where the bulk of the population lives and where the larger cities, including Santiago, are located. South-central Chile, with a lake and forest region, is temperate, humid, and suitable for grain cultivation; and the southernmost third of the country, cut by deep fjords, is an inhospitable region—cold, wet, windy, and limited in resources. The economy of Chile is based on primary economic activities: agricultural production; copper, iron, and nitrate mining; and the exploitation of sea resources. Chile exhibits many of the traits that typically characterize Latin American countries. It was colonized by Spain, and the culture that evolved was largely Spanish. However, appreciation for the influence of indigenous culture has been growing. The people became largely mestizo, a blend of Spanish and Indian bloodlines. The society developed with a small elite controlling most of the land, the wealth, and the political life. Chile did not, however, depend as heavily on agriculture and mining as did many Latin American countries, but rather developed an economy based on manufacturing as well. Thus, Chile has become one of the more urbanized Latin American societies, with a burgeoning middle class. Chile has also had a history of retaining representative democratic government. Except for a military junta that held power from September 1973 to March 1990, the country has been relatively free of the coups and constitutional suspensions common to many of its neighbours. Land – Relief The major landforms of Chile are arranged as three parallel north–south units: the Andes mountains to the east; the intermediate depression, or longitudinal valley, in the centre; and the coastal ranges to the west. These landforms extend lengthwise through the five latitudinal geographic regions into which the country is customarily subdivided. From north to south, with approximate boundaries, these are Norte Grande (extending to 27° S); the north-central region, Norte Chico (27° to 33° S); the central region, Zona Central (33° to 38° S); the south-central region, La Frontera and the Lake District (38° to 42° S); and the extreme southern region, Sur (42° S to Cape Horn). The Chilean Andes Extending almost the length of the country, the Chilean Andes, which form most of the border with Argentina, include the highest segment of the Andes mountain chain, which acts as both a physical and a human divide. The Chilean Andean system consists of lofty, often snow-capped mountains, deeply incised valleys, and steep slopes. The formation of the western Andes ranges began during the Jurassic Period, some 200 million years ago. Marine and terrestrial sediments that had accumulated in the Andean geosyncline were folded and lifted as the Pacific Plate was overridden by the South American Plate. In the Cenozoic Era (beginning about 65 million years ago) active volcanism and the injection of effusive rocks laid down the paleovolcanic materials (rhyolites and dacites) that contain the rich copper, iron, silver, molybdenum, and manganese ores of Chile. Also of Cenozoic origin are the coal deposits of central Chile. Later in the Cenozoic Era the uplift of the Andes continued, accompanied by further outbursts of volcanism. This active tectonism led to the separation of the Andes from the older coastal ranges and the formation of the intermediate depression. At the beginning of the Quaternary Period (about 2.6 million years ago) the Andes had reached a higher elevation than at present. During the global cooling that occurred from the beginning of the Quaternary, the higher summits were covered by ice masses whose glacier tongues descended into the intermediate depression. Rich sediments were washed down the glacial valleys and deposited into the longitudinal depression. The numerous lakes in the Lake District of south-central Chile are remnants of the ice melting that began some 17,000 years ago. Since the advent of the Holocene Epoch (11,700 years ago) the Chilean Andes have not changed significantly, but they still experience uplift and episodic volcanic eruptions. The Andes of northern Chile to latitude 27° S are wide and arid, with heights generally between 16,500 and 19,500 feet (5,000 and 6,000 metres). Most of the higher summits are extinct volcanoes, such as the Llullaillaco, 22,109 feet; Licancábur, 19,409 feet; and Ojos del Salado, 22,614 feet. After the last glaciation the melting waters collected in shallow lakes in the intermediate elevated basins. Today these salt lake basins (salares), the most noted of which is the Atacama Salt Flat, are evaporating to the point of disappearing. Farther south the mountains decrease somewhat in height, but in central Chile, between latitudes 32° and 34°30′ S, they heighten again, with peaks reaching 21,555 feet at Mount Tupungato and 17,270 feet at Maipo Volcano. All of these summits are capped by eternal snow that feeds the numerous rivers of central Chile. Winter sports are pursued in the Andes near Santiago. Most of the highest mountains between 34°30′ and 42° S are volcanoes, ranging between 8,700 and 11,500 feet. Some of them are extinct while others are still active. Among them are Copahue, Llaima, Osorno, and the highest, Mount Tronador, at an elevation of 11,453 feet. Their perfect conical shapes reflecting on the quiet waters in the Lake District provide some of the most splendid scenery in temperate South America. In southern Chile, below latitude 42° S, the Andes lose elevation and their summits become more separated as a consequence of the Quaternary glacial erosion. Farther south is Chilean Patagonia, a loosely defined area that includes the subregion of Magallanes and sometimes Chilean Tierra del Fuego. There significant heights are still reached: Mount San Valentín is more than 12,000 feet high, and Mount Darwin in Tierra del Fuego reaches almost 8,000 feet. Reminders of the last ice age are the perfectly U-shaped glacial troughs, sharp-edged mountains, Andean lakes, and some 7,000 square miles of continental ice masses. The Southern Ice Cap, between 48°30′ and 51°30′ S, is the largest in the Southern Hemisphere, with the exception of Antarctica The intermediate depression The intermediate depression between the Andes and the coastal ranges is mostly flanked by fault lines. A natural receptacle for materials coming from the Andes, the depression has been filled by alluvial, fluvioglacial, or moraine sediments, depending on the region. In northern Chile it appears as a plateau with elevations between 2,000 and 4,000 feet. Saline sediments that washed down during the Cenozoic Era created the rich nitrate deposits found in the Tamarugal Plain and Carmen Salt Flat, where the once-bustling mining towns of María Elena, Pedro de Valdivia, and Baquedano are located. In north-central Chile, extending southward out of the desert region, the depression is interrupted by east–west mountain spurs that create fertile transverse valleys. The Aconcagua River valley, a transverse valley farther south, marks the beginning of central Chile. The alluvial deposits from the numerous Andean rivers in central Chile have provided mineral-rich soils that support the flourishing Mediterranean-type agriculture of the Central Valley of the intermediate depression. These soils and abundant water resources, along with a temperate climate, make the Central Valley the most populated and productive area in Chile. In south-central Chile the intermediate depression is formed by mixtures of fluvial and alluvial depositions, making this region suitable for growing grain and for pastures that support an important dairy industry. South of the Biobío River dense forests replace open scrub woodland moraines and lakes are common, and the intermediate depression descends to sea level at Puerto Montt. In the extreme south only the Andes and the summits of the coastal ranges are visible because the intermediate depression submerges or is replaced by intracoastal channels and fjords. More … Score: https://www.britannica.com/place/Chile

2022/09/18

Querida Polonia

An open invitation for travelers of Poland to visit Mexico. Make your dream trip come true!

2022/09/16

Pierwsze Delegacje Programu Open World w USA

10 sierpnia 2022 r. pierwsze delegacje z Polski wyleciały do Stanów Zjednoczonych w ramach Programu Open World finansowanego przez Kongres Stanów Zjednoczonych, prowadzonego przez Biuro Kongresu ds. Międzynarodowego Przywództwa (Open World Leadership Center) i realizowanego przez American Councils for International Education.

2022/09/16

LOS LUGARES MÀS BELLOS DE NICARAGUA

Nicaragua tierra de lagos y volcanes y en este video te mostrare los lugares mas turisticos de Nicaragua, entre ellos se destacan la ciudad de Leon, El Cañon de Somoto, Chinandega, Granda, Masaya, entre otros.

2022/09/16

Spotkanie Marszałek Sejmu z Ambasadorem Kolumbii

Nowy ambasador Kolumbii w Polsce Assad José Jater Peńa złożył w piątek, 5 sierpnia 2022 roku, wizytę u marszałek Sejmu Elżbiety Witek. Spotkanie poświęcone było omówieniu dotychczasowej współpracy miedzi krajami. Sporo miejsca zajął temat Ukrainy i polskiej pomocy skierowanej do uchodźców zza wschodniej granicy.

2022/09/16

Wystawa ukraińskich artystów pt.: "Unfolding Landscapes".

Wprawdzie znaczna część wakacji już za nami, ale dla wielu podróżników wrzesień to idealny moment na urlop. Jeśli planujecie wojaże po Europie, to Belgia ?? musi koniecznie znaleźć się na Waszej trasie! Poza swym niezwykłym urokiem, zabytkami i kulturą, do 18 września ma dla odwiedzajacych dodatkową atrakcję.

2022/09/16

HONDURAS - Honduras | The Republic of Honduras | imágenes inéditas tiroteo en chamelecón, honduras

Honduras officially the Republic of Honduras (Spanish: República de Honduras), is a country in Central America. The republic of Honduras is bordered to the west by Guatemala, to the southwest by El Salvador, to the southeast by Nicaragua, to the south by the Pacific Ocean at the Gulf of Fonseca, and to the north by the Gulf of Honduras, a large inlet of the Caribbean Sea. Honduras was home to several important Mesoamerican cultures, most notably the Maya, before the Spanish Colonization in the sixteenth century.

2022/09/16