St. Kitts Tourism, Vacations, and Island Guide | St. Kitts Hotels

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2025/09/21

Independence Day of the Belize

Belize, country located on the northeast coast of Central America. Belize, which was known as British Honduras until 1973, was the last British colony on the American mainland. Its prolonged path to independence was marked by a unique international campaign (even while it was still a British colony) against the irredentist claims of its neighbour Guatemala. Belize achieved independence on September 21, 1981, but it has retained its historical link with the United Kingdom through membership in the Commonwealth. Belize is often thought of as a Caribbean country in Central America because it has a history similar to that of English-speaking Caribbean nations. Indeed, Belize’s institutions and official language reflect its history as a British colony. However, its culture is more typical of that of other Central American countries. Belize’s small population is ethnically diverse and includes a large proportion of immigrants. Since the 1970s, migration has shifted Belize’s ethnic composition from a predominantly Creole (mixed African and British descent) population to one in which mestizos (in Belize, people of mixed Mayan and Spanish ancestry) make up half of the total inhabitants. Belize has one of the most stable and democratic political systems in Central America. After its original capital, Belize City, was ravaged by a hurricane in 1961, a new capital, Belmopan, was built inland, about 50 miles (80 km) west of Belize City, which remains the country’s commercial and cultural centre as well as its most populous city. The name Belize is traditionally believed to have been derived from the Spanish pronunciation of the last name of Peter Wallace, a Scottish buccaneer who may have begun a settlement at the mouth of the Belize River about 1638. It is also possible that the name evolved from the Mayan word belix (“muddy water”) or belikin (“land facing the sea”). Land Situated south of the Yucatán Peninsula, Belize is a land of mountains, swamps, and tropical jungle. It is bounded by Mexico to the north, Guatemala to the west and south, and the Caribbean Sea to the east. The country has a 174-mile (280-km) coastline. Relief The southern half of the country is dominated by the rugged Maya Mountains, a plateau of igneous rock cut by erosion into hills and valleys that stretch in a southwesterly to northeasterly direction. The Cockscomb Range, a spur of the Maya Mountains, runs toward the sea and rises to Doyle’s Delight. The northern half of the country consists of limestone lowlands and swamps less than 200 feet (60 metres) above sea level. Drainage and soils The lowlands are drained by the navigable Belize River (on which stands Belize City), the New River, and the Hondo River (which forms the northern frontier with Mexico). Both the New and the Hondo rivers drain into Chetumal Bay to the north. South of Belize City the coastal plain is crossed by short river valleys. Along the coast is the Belize Barrier Reef, the second largest barrier reef in the world, which is fringed by dozens of small islands called cays. The reef reserve system was designated a UNESCO World Heritage site in 1996. Belize’s most fertile soils are the limestone soils found in the northern half of the country and in the coastal plain and river valleys in the south. Climate of Belize Belize has a subtropical climate, with a well-marked dry season from late February to May and a wet season from June to November that is interrupted from August to September by another dry season. The mean temperature in Belize City is about 74 °F (23 °C) in December and 84 °F (29 °C) in July. The mean annual rainfall increases sharply from about 50 inches (1,270 mm) at Corozal on the northern frontier to 175 inches (4,445 mm) at Punta Gorda in the south, while at Belize City rainfall amounts to about 75 inches (1,900 mm). There are, however, considerable yearly variations throughout the country. Trade winds blow onshore most of the year, and from September to December northerly winds bring cooler, drier air. Hurricanes (tropical cyclones) are a threat from July through November. A hurricane in 2000 devastated the country’s infrastructure and displaced tens of thousands of Belizeans. Plant and animal life About three-fifths of Belize is forested. There are at least 50 different forest tree species, including mahogany, Santa Maria (Calophyllum brasiliense), cedar, and ironwood. In the north, limestone soils support deciduous forests, and sapodilla and mahogany predominate. In the south, the forest is taller and is evergreen. Santa Maria, rather than mahogany, flourishes on the plateau, and oak and pine grow on some of the plateau ridges. The rivers are largely bordered by swamp forests. On the southern coastal plain and inland from Belize City, open savanna (grassland) is marked by scattered oaks, pines, and palmetto palms. The coast is fringed with mangrove trees. The highlands are mostly forested and are largely uninhabited. The abundant wildlife of Belize includes such animals as tapir, deer, jaguar, puma (known locally as “red tiger”), American crocodile, and manatee, as well as many species of turtles, tortoises, birds, reptiles, insects, and fish. The herbivorous Baird’s tapir (Tapirus bairdii), which is colloquially named the “mountain cow” and can weigh as much as 600 pounds (270 kg), has protected status as the national animal of Belize. In the shadow of Victoria Peak lies the Cockscomb Basin Wildlife Sanctuary, which covers about 150 square miles (390 square km). The sanctuary, founded in 1986, has the most concentrated jaguar population in the world. People - Ethnic groups Many Belizeans are of mixed ancestry, most of them descendants of immigrants. Those of mixed Mayan and Spanish heritage (mestizos) constitute the largest ethnic group (about one-half of the population) and predominate in the more sparsely inhabited interior, along with the Maya (Yucatec Maya in the north and Mopán and Kekchí Maya in the south), who account for nearly one-tenth of the population. English-speaking people of largely African and British ancestry, who are called Creole, account for more than one-fourth of the population and predominate in the central coastal regions. A significant number of Garifuna (Garinagu), who are descendants of the Carib Indians and Africans deported from Saint Vincent by the British to the Gulf of Honduras in 1798, live in communities on the south coast. People of European and South Asian ancestry are also present, as are smaller numbers of immigrants from China, the Middle East, and elsewhere. Mennonite farmers began to migrate to Belize in the 1950s from Canada and Mexico to escape religious persecution, and Mennonite communities have been allowed to settle in rural areas throughout the country. Although this group makes up a tiny percentage of the population, its contribution to the Belizean economy, largely through farming, has been significant. Refugees from Guatemala, Honduras, and El Salvador began migrating to Belize in the 1980s to escape civil war and political unrest in their countries. Throughout the 1990s, these refugees made up the largest immigrant group in Belize. At the beginning of the 21st century, the number of these refugees significantly decreased, but their descendants account for about four-fifths of the total foreign-born population in Belize. More … Score: https://www.britannica.com/place/Belize

2025/09/21

Discover MALI: 10 INTERESTING FACTS ABOUT THIS WEST AFRICAN COUNTRY

Mali is a West African landlocked country subdivided into 10 regions... Officially, it is referred to as the Republic of Mali. Bamako is its capital city. According to the World Bank in 2020, the population of Mali stood at 20.25 million people. Its currency is the West African CFA Franc and the country’s official languages are Bambara and French. It is the eighth-largest country in Africa with an area of over 1,240,000 square kilometres.

2025/09/21

Independence day of the Republic of Malta

Malta, island country located in the central Mediterranean Sea. A small but strategically important group of islands, the archipelago has through its long and turbulent history played a vital role in the struggles of a succession of powers for domination of the Mediterranean and in the interplay between emerging Europe and the older cultures of Africa and the Middle East. As a result, Maltese society has been molded by centuries of foreign rule by various powers, including the Phoenicians, Romans, Greeks, Arabs, Normans, Sicilians, Swabians, Aragonese, Hospitallers, French, and British. The island of Malta specifically played a vital strategic role in World War II as a base for the Allied Powers. It was heavily bombarded by German and Italian aircraft, and by the end of the war Malta was devastated. In 1942 the island of Malta was presented with the George Cross, a British award for great gallantry, in recognition of the wartime bravery of the Maltese people. After the war, the movement for self-governance became stronger. The country of Malta became independent from Britain and joined the Commonwealth in 1964 and was declared a republic on December 13, 1974. It was admitted to the European Union (EU) in 2004. A European atmosphere predominates in Malta as a result of close association with the Continent, particularly with southern Europe. The Maltese are renowned for their warmth, hospitality, and generosity to strangers, a trait that was noted in the Acts of the Apostles, with respect to the experience of St. Paul, the Apostle, who was said to have been shipwrecked off Malta in 60 ce. Roman Catholicism is a major influence on Maltese culture. Various traditions have evolved around religious celebrations, notably those honouring the patron saints of towns and villages. The eight-pointed, or Maltese, cross, adopted by the Hospitallers of St. John of Jerusalem in 1126, is commonly linked with Malta’s identity and is printed on the country’s euro coin. Valletta is the capital city. Land The country comprises five islands—Malta (the largest), Gozo, Comino, and the uninhabited islets of Kemmunett (Comminotto) and Filfla—lying some 58 miles (93 km) south of Sicily, 180 miles (290 km) north of Libya, and about 180 miles (290 km) east of Tunisia, at the eastern end of the constricted portion of the Mediterranean Sea separating Italy from the African coast. Relief The islands of Malta are dominated by limestone formations, and much of their coastlines consist of steep or vertical limestone cliffs indented by bays, inlets, and coves. They lie on the submerged Malta-Hyblean Platform, a wide undersea shelf bridge that connects the Ragusa Platform of southern Sicily with the Tripolitana Platform of southern Libya. The main physical characteristic of the island of Malta is a well-defined escarpment that bisects it along the Victoria Lines Fault running along the whole breadth of the island from Point ir-Raħeb near Fomm ir-Riħ Bay to the coast northeast of Għargħur at Madliena Fort. The highest areas are coralline limestone uplands that constitute a triangular plateau; Ta’ Żuta, which rises to 830 feet (253 metres) in the southwest, is the highest point. The uplands are separated from the surrounding areas by blue clay slopes, while an undercliff area is found where the coralline plateau has fallen and forms a subordinate surface between the sea and the original shore. The total shoreline of Malta is about 136 miles (219 km). In northern Malta the escarpment is occasionally abrupt and broken by deep embayments. To the south, however, the plateau gradually descends from about 600 to 830 feet (180 to 250 metres) into undulating areas of globigerina (derived from marine protozoa) limestone less than 300 feet (90 metres) in elevation. The western area is characterized by deeply incised valleys and undercliff areas, while to the east there are several valley systems that descend to the central plains. The west coast of Malta presents a high, bold, and generally harbourless face. On the east, however, a tongue of high ground known as Mount Sceberras, on which the capital city, Valletta, is built, separates Marsamxett Harbour and Grand Harbour. Because of tectonic activity, Malta has been tilted in a northerly direction, producing cliffs of up to about 800 feet (250 metres) high on the south and southwestern coasts, while slopes descend to low cliffs and rocky shores on the northern and eastern coasts. The landscape of the island of Gozo is characterized by broken upper coralline mesas, with the highest point being Ta’ Dbiegi Hill (636 feet [194 metres]). Gozo has a gentle easterly dip, so the lower coralline limestone, which forms high cliffs on the west coast, declines to below sea level but reappears on the east coast at Qala Point. Semicircular bays have formed on coastal cliffs where sinkholes have been invaded by the sea. The rounded bays at Xlendi and Dwejra on the west coast of Gozo originated as underground caverns with roofs that have collapsed. Drainage The island of Malta possesses favourable conditions for the percolation and underground storage of water. The impermeable blue clays provide two distinct water tables between the limestone formations—the perched and the mean sea-level aquifer. The principal source for the public supply of water has for several centuries been the main sea-level water table. The absence of permanent streams or lakes and a considerable runoff into the sea, however, have made water supply a problem, which has been addressed with an intensive reverse-osmosis desalination program. About half of Malta’s daily water needs are supplied by desalination plants throughout the islands. Soils Mainly young or immature and thin, Maltese soils generally lack humus, and a high carbonate content gives them alkaline properties. Human settlement and construction developments have altered the distribution and composition of soils. The Fertile Soil (Preservation) Act of 1973 requires that, when soils are removed from construction sites, they be taken to agricultural areas, and level stretches in quarries are often covered with carted soil. Climate of Malta The climate of Malta is typically Mediterranean, with hot, dry summers, warm and sporadically wet autumns, and short, cool winters with adequate rainfall. More than three-fourths of the total annual rainfall of about 22 inches (550 mm) falls between October and March; June, July, and August are normally quite dry. The temperature is very stable, with the annual mean in the mid-60s F (about 19 °C) and monthly averages ranging from the mid-50s F (about 12 °C) to the mid-80s F (about 29 °C). Winds can be strong and frequent; the most prevalent are the cool northwesterly (the majjistral), the dry northeasterly (the grigal), and the hot and humid southeasterly (the xlokk, or sirocco). The relative humidity rarely falls below 40 percent. More … Score: https://www.britannica.com/place/Malta

2025/09/21

Restoration of Armenian Independence: Third Republic of 1991

Proceeding from the provisions of 1990 August 23 Armenian Declaration of Independence, the National Assembly decided to hold a referendum on September 21, 1991, to leave the USSR and declaring independence. Based on the results of the referendum, the Supreme Council declared Armenia an independent state. The centuries-long dream of the Armenian nation to reinstate independence came true. On October 16, nationwide presidential elections were held in Armenia, as a result of which, Levon Ter-Petrosyan was elected as the first president of the republic. On December 8, 1991, in Belovezhskaya Puscha (near Minsk) the leaders of the three Slavic states (Russia, Ukraine, and Belarus) signed an agreement on seizing the existence of the USSR. Simultaneously the sides declared the creation of a new entity of international cooperation, the Commonwealth of Independent States (CIS.) The Republic of Armenia was he first among the former Soviet republics to respond to the Minsk agreement welcoming the creation of CIS and expressed its willingness to join the organization. On December 21 of the same year 11 independent states (former soviet republics) signed an agreement in Alma-Ata about the creation of CIS. This marked the final collapse of the USSR and the independence of the Soviet Republics. Shortly after declaring independence the Republic of Armenia received universal international recognition. Thus began the process of state-building of the Armenian Republic. One of the most important events of the state-political and public life of the Republic was the adoption of the RA Constitution that took place on July 5, 1995. It contributed to and greatly strengthened the legal bases of transition from a totalitarian system to a democratic state. In the context of the war unleashed by Azerbaijan, the security of the population of Nagorno Karabakh became a priority alongside the issue of preserving the independence of the Armenian nation-state, whose guarantee could only be the creation of an efficient military. In the period of 1992-1993 with the unification of Yerkrapah Voluntary Detachments and army conscripts the Armenian National Army was created. On January 28, 1992, the Government adopted the historical decision on RA Ministry of Defense. The regular military units were formed generally based on the Soviet Army. Hundreds of Armenian officers, that have served in various branches of the Soviet Army, returned to Armenia. Special attention was paid given to the combat readiness and improvement. Another important event contributing to the raising of public and political activism were the presidential elections that took place on September 22, 1996. These elections were held amid active political struggle. For the second time, Levon Ter-Petrosyan was elected as the president of the republic. The alienation between the authorities and public following the 1996 elections as well as the internal political crisis led to the resignation of the president in 1998. In March of the same year the main struggle during the snap presidential elections was between Robert Kocharyan, the Prime Minister of Armenia and Karen Demirchyan, the former First Secretary of the Central Committee of the Communist Party of Armenia who had recently returned to the political arena. Robert Kocharyan was elected the President of the Republic. The Unity alliance became the victor in the March 30, 1999 parliamentary elections, that took place amid quite active political struggle. Karen Demirchyan was elected the president of the National Assembly, while Vazgen Sargsyan was appointed as the Prime Minister. The domestic political situation worsened unprecedentedly with October 27, 1999 terrorist act, as a result of which were murdered the Prime Minister, the President of the National Assembly, NA Deputy Presidents and deputies. It was a heavy and unexpected blow to the (Armenian) statehood and democracy. Nevertheless, the political leadership was able to gradually stabilize the situation. The fourth presidential elections of Armenia were held of February 19, 2003. Robert Kocharyan was reelected. The next parliamentary elections took place on May 25, 2003, as a result of which not one party received an absolute majority and form a government on its own and, thus, for the first time in the history of the Third Republic, three parties that had received the most votes, the Republican Party of Armenia (RPA,) the Orinats Yerkir (OEK,) and the Armenian Revolutionary Federation (AFD,) formed a political coalition and jointly formed a cabinet. Andranik Margaryan, the Chairman of the Board of the Republican Party of who had already been holding that office since 2000, was elected a Prime Minister. On November 27, 2005, the new reformed version of the RA Constitution. On May 12, 2007 took place amid a climate of high political activity the parliamentary elections of the fourth convocation of the National Assembly, where, according to the system of proportional representation, the Republican Party of Armenia received the majority of votes, followed by the “Prosperous Armenia” and the Armenian Revolutionary Federation. As a result of the elections, with the assistance of the RA President, an agreement of creating a political coalition was signed between the parties. Those three parties formed the new government of the Republic of Armenia. Serzh Sargsyan was appointed a Prime Minister. The fifth presidential elections of the Republic of Armenia took place on February 19, 2008. Serzh Sargsyan was elected as the President of the Republic of Armenia. The results of the presidential elections were challenged by the leader of the fundamental faction of the opposition, Levon Ter-Petrosyan. On February 20, the opposition initiated rallies that developed into clashes between the opposition and the law enforcement on March 1-2. Initiated by the newly-elected president with the purpose of enstating reforms in the republic and ensuring an atmosphere of solidarity in the society the four parties with the most votes in the RA National Assembly signed a new agreement of political coalition, assuming responsibility for the future activities of the government. Tigran Sargsyan was appointed as the Prime Minister. Later, on April 22, 2009, the ARF quit the coalition. The parliamentary elections of the fifth convocation of the National Assembly took place on May 6, 2012, resulting in RPA receiving 44% of the votes according to the system of proportional representation. RPA and OEK form a new coalition assuming the the responsibility of the political, economic and social development of the Republic of Armenia. Tigran Sargsyan was appointed the Prime Minister. On February 18, 2013, Serzh Sargsyan is reelected as a result of presidential elections. Starting April 13, 2014, Hovik Abrahamyan leads the Government of the Republic of Armenia. In April of the Same year, OEK quits the coalition joining the opposition. On December 6, 2015, a new reformed version of the Constitution is adopted through a referendum, according to which the Republic of Armenia underwent a transition to a parliamentary form of government. Starting September 13, 2016, Karen Karapetryan assumed the office of the head of the RA government, holding that position until April 17, 2018. According to the new Constitution, on March 2, 2018, the National Assembly elected Armen Sarkissian, the former ambassador of the Republic of Armenia to Great Britain as the President of the Republic of Armenia. Armen Sarkissian assumed the presidency on April 9, 2018. According to the new Constitution, the next election of the RA Prime Minister were held by the National Assembly, as a result of which, on April 17, 2018, Serzh Sargsyan was elected the Prime Minister. However, as a result of an opposition movement that had started in April, that government survived only seven days, becoming the shortest government in the history of Armenia. On May 8, 2018, the National Assembly of the Republic of Armenia elected Nikol Pashinyan, the leader of “Yelq” (Exit) parliamentary bloc, as the Prime Minister. Score: https://www.mfa.am/en/history/

2025/09/21

Introduction to Belize

A revamp of Belize Tourism Board's(BTB) "Be One With Belize" video. Special Thanks to Minister of Tourism, Hon. Manuel Heredia Jr. for allowing us to borrow some clips in an effort to market Belize and all its natural, wonder to the world.

2025/09/20

Malta

This video takes us on a journey to discover an island of contrasts and surprises: Malta. From lounging on St.Peter’s pool beach to discovering the colourful village of Marsaxlokk, mingling with the fishermen and relaxing on the traditional Luzzu boats marked by “Eye of Osiris”, there is a whole island of stunning views to wake up to. Add to that the famed old capital of Mdina, the imposing Saint John’s Co-Cathedral in Valletta, and magnificent cliffs in Gozo and it’s easy to understand why most of the people start planning their return trip to Malta before they’ve even left the island the first time.

2025/09/20

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

2025/09/20

Oficinas de Información Turística (OIT) - Sernatur

Oficina de Información Turística de Antofagasta ... Lunes a viernes de 8:30 a 18:00 horas. 600 600 60 66. infoantofagasta@sernatur.cl. Ver mapa ...

2025/09/20