Ireland's official holiday and travel guide

Tourism Ireland's website is packed with holiday ideas, information and advice to help you find accommodation, plan activities and see what's on.

2025/03/19

St. Patrick's Day Republic of Ireland

Ireland, Irish Éire, country of western Europe occupying five-sixths of the westernmost major island of the British Isles. The magnificent scenery of Ireland’s Atlantic coastline faces a 2,000-mile- (3,200-km-) wide expanse of ocean, and its geographic isolation has helped it to develop a rich heritage of culture and tradition that was linked initially to the Gaelic language. Washed by abundant rain, the country’s pervasive grasslands create a green-hued landscape that is responsible for the popular sobriquet Emerald Isle. Ireland is also renowned for its wealth of folklore, from tales of tiny leprechauns with hidden pots of gold to that of the patron saint, Patrick, with his legendary ridding the island of snakes and his reputed use of the three-leaved shamrock as a symbol for the Christian Trinity. But while many may think of Ireland as an enchanted land, the republic has been beset with perennial concerns—emigration, cultural and political identity, and relations with Northern Ireland (comprising the 6 of Ireland’s 32 counties within the province of Ulster that remain part of the United Kingdom). At the beginning of the 21st century, Ireland’s long-standing economic problems were abating, owing to its diverse export-driven economy, but calamity struck again in 2008 when a new financial and economic crisis befell the country, culminating in a very costly bailout of the Irish economy by the European Union (EU) and the International Monetary Fund. The emergence of Ireland as an independent country is a fairly recent phenomenon. Until the 17th century, political power was widely shared among a rather loosely constructed network of small earldoms in often-shifting alliances. Following the so-called “Flight of the Earls” after an unsuccessful uprising in the early 17th century, Ireland effectively became an English colony. It was formally incorporated into the United Kingdom in 1801. A 1914 Home Rule Act was passed but never implemented due to pro-union militancy in the north, the onset of World War I, and the subsequent Irish War of Independence. In 1920 the island was effectively partitioned with the creation of Northern Ireland, a six-county area with devolved powers within the United Kingdom, whereas under the Anglo-Irish Treaty of December 6, 1921, the other 26 counties became the Irish Free State, a self-governing dominion within the British Commonwealth and Empire. In 1937 the southern state passed a new constitution that offered a more robust expression of sovereignty, and in 1949 it formally left the Commonwealth as the Republic of Ireland. Since then Ireland has become integrated with the rest of western Europe. It joined the European Economic Community (forerunner of the EU) in 1973. Though the country generally retained a neutral role in international affairs, in 2008 Ireland became an impediment to the enactment of the Lisbon Treaty—an agreement aimed at streamlining the EU’s processes and giving it a higher international profile—when the Irish voted against the passage of the treaty in a national referendum. The treaty, however, was approved by Irish voters in a second referendum, held the following year. Explore the history of the Irish people and the impact of the mass emigration in America during the 19th-century famine Overview of the people of Ireland, with a focus on the impact of the mass emigration to the United States during the 19th century. Dependent on agriculture, Ireland was long among Europe’s poorest regions, a principal cause of mass migration from Ireland, especially during the cycle of famine in the 19th century. Some 40 million Americans trace their ancestry to Ireland as a result of that traumatic exodus, as do millions of others throughout the world. Every year members of this diaspora visit their ancestral homeland and forge connections with long-lost family. Ireland’s capital is Dublin, a populous and affluent city whose metropolitan area is home to more than one-fourth of the country’s total population. The city’s old dockside neighbourhoods have given way to new residential and commercial development. Cork, Ireland’s second largest city, is a handsome cathedral city and port in the southwest. Other principal centres include Waterford, Wexford, and Drogheda on the east coast, Sligo in the northwest, and Limerick and Galway in the west. Although Ireland is now both urbanized and Europeanized, its culture retains many unique characteristics, and its people prize folkloric and social traditions that largely derive from and celebrate the country’s rural past. In “Meditations in Time of Civil War” William Butler Yeats, perhaps Ireland’s best-known poet, evokes the idyllic and idealized countryside, a place central to the memories of the country’s millions of expatriates and their descendants: An acre of stony ground, Where the symbolic rose can break in flower, Old ragged elms, old thorns innumerable, The sound of the rain or sound Of every wind that blows; The stilted water-hen Crossing stream again Scared by the splashing of a dozen cows. Land The republic of Ireland occupies the greater part of an island lying to the west of Great Britain, from which it is separated—at distances ranging from 11 to 120 miles (18 to 193 km)—by the North Channel, the Irish Sea, and St. George’s Channel. Located in the temperate zone between latitudes 51°30′ and 55°30′ N and longitudes 6°00′ and 10°30′ W—as far north as Labrador or British Columbia in Canada and as far west as the West African state of Liberia—it constitutes the westernmost outpost of the Atlantic fringe of the Eurasian landmass (the absolute extreme of which is Tearaght Island, the westernmost member of the Blasket Islands, which lie off the Dingle Peninsula and are part of County Kerry). Ireland, which, like Great Britain, once formed part of this landmass, lies on the European continental shelf, surrounded by seas that are generally less than 650 feet (200 metres) deep. The greatest distance from north to south in the island is 302 miles (486 km), and from east to west it is 171 miles (275 km). Relief The territory of the republic consists of a broad and undulating central plain underlain by limestone. This plain is ringed almost completely by coastal highlands, which vary considerably in geologic structure. The flatness of the central lowland—which lies for the most part between 200 and 400 feet (60 and 120 metres) above sea level—is relieved in many places by low hills between 600 and 1,000 feet (180 to 300 metres) in elevation. With many lakes, large bog areas, and low ridges, the lowland is very scenic. The principal mountain ranges are the Blue Stack Mountains in the north, the Wicklow Mountains in the east (topped by Lugnaquillia, at 3,039 feet [926 metres]), the Knockmealdown and Comeragh mountains in the south, the Macgillycuddy’s Reeks in the southwest, and the Twelve Pins in the west. Carrantuohill, at 3,414 feet (1,041 metres) in the Macgillycuddy’s Reeks, is the highest point in the republic. In the west and southwest the wild and beautiful coast is heavily indented where the mountains of Donegal, Mayo, Galway, and Kerry thrust out into the Atlantic, separated by deep wide-mouthed bays, some of which—Bantry Bay and Dingle Bay, for example—are, in fact, drowned river valleys. By contrast, the east coast is little indented, but most of the country’s trade passes through its ports because of their proximity to British and Continental markets. The coastal mountain fringe illustrates the country’s complex geologic history. In the west and northwest as well as in the east, the mountains are composed mainly of granite. Old Red Sandstone predominates in the south, where the parallel folded mountain ridges trend east-west, separated by limestone river valleys. Ireland experienced at least two general glaciations—one covering most of the country and the other extending as far south as a line linking Limerick, Cashel, and Dublin—and the characteristic diversity of Irish scenery owes much to this glacial influence. The large areas of peat bog to be found throughout the country are a notable feature of the landscape. More …   Score: https://www.britannica.com/place/Ireland

2025/03/17

Ireland - Official IMAX Trailer

IRELAND will be released in IMAX® and giant screen theaters in February 11, 2022. Journey to a magical land of stunning natural wonders, ancient clifftop marvels, and a rich, cultural heritage in the new film IRELAND for IMAX® and giant screen theatres. Follow Irish writer Manchán

2025/03/16

Vatican News: News from the Vatican - News about the Church

Visit Vatican News for all the latest updates on Pope Francis, the Holy See and the Church in the World.

2025/03/15

Mauritius Welcomes You: The Official Site for Mauritius

Mauritius Welcomes You - The Official Site for Mauritius. ... Mauritius government, it is noted the aim of the events will be to promote the air corridor.

2025/03/14

Anniversary of the Election of Pope Francis

Holy See Roman Catholic government - The Holy See is the name given to the government of the Roman Catholic Church, which is led by the pope as the bishop of Rome. As such, the Holy See’s authority extends over Catholics throughout the world. Since 1929 it has resided in Vatican City,… Vatican City, in full State of the Vatican City, Italian Stato della Città del Vaticano, ecclesiastical state, seat of the Roman Catholic Church, and an enclave in Rome, situated on the west bank of the Tiber River. Vatican City is the world’s smallest fully independent nation-state. Its medieval and Renaissance walls form its boundaries except on the southeast at St. Peter’s Square (Piazza San Pietro). Of the six entrances, only three—the piazza, the Arco delle Campane (Arch of the Bells) in the facade of St. Peter’s Basilica, and the entrance to the Vatican Museums and Galleries in the north wall—are open to the public. The most imposing building is St. Peter’s Basilica, built during the 4th century and rebuilt during the 16th century. Erected over the tomb of St. Peter the Apostle, it is the second largest religious building (after Yamoussoukro Basilica) in Christendom. The Vatican palace is the residence of the pope within the city walls. The Holy See is the name given to the government of the Roman Catholic Church, which is led by the pope as the bishop of Rome. As such, the Holy See’s authority extends over Catholics throughout the world. Since 1929 it has resided in Vatican City, which was established as an independent state to enable the pope to exercise his universal authority. Vatican City has its own telephone system, post office, gardens, astronomical observatory, radio station, banking system, and pharmacy, as well as a contingent of Swiss Guards responsible for the personal safety of the pope since 1506. Almost all supplies—including food, water, electricity, and gas—must be imported. There is no income tax and no restriction on the import or export of funds. As the Holy See, it derives its income from the voluntary contributions of more than one billion Roman Catholics worldwide, as well as interest on investments and the sale of stamps, coins, and publications. Banking operations and expenditures have been reported publicly since the early 1980s. During the period from the 4th century to 1870, the Vatican gained control of territory around Rome and served as capital of the Papal States. In 1929 Vatican City’s independent sovereignty was recognized by the Fascist Italian government in the Lateran Treaty. Sovereignty is exercised by the pope upon his election as the head of the Roman Catholic Church. He has absolute executive, legislative, and judicial powers within the city. In 1984 a major reshuffle of offices in the Roman Curia resulted in the delegation of the routine administration of Vatican City to a pontifically appointed commission of five cardinals headed by the Secretariat of State. The inhabitants of Vatican City, the majority of whom are priests and nuns, also include several hundred laypersons engaged in secretarial, domestic, trade, and service occupations. Special extraterritorial privileges are extended to more than 10 other buildings in Rome and to Castel Gandolfo, the pope’s summer residence in the Alban Hills. In addition, Vatican City maintains embassies in numerous foreign nations. Vatican cultural life has much declined since the Renaissance, when the popes were among Italy’s foremost patrons of the arts. The Vatican Museums and Galleries, the frescoes by Michelangelo in the Sistine Chapel, the frescoes by Pinturicchio in the Borgia Apartment, and Raphael’s Stanze (“Rooms”) nevertheless attract critics, artists, and flocks of tourists from throughout the world. Years of restoration work on the Sistine Chapel frescoes were completed in 1994, making it possible to view Michelangelo’s work in full vibrant colours. In 2000 the millennial Jubilee focused world attention on Vatican City. The Vatican Apostolic Library contains a priceless collection of some 150,000 manuscripts and 1.6 million printed books, many from pre-Christian and early Christian times. The Vatican publishes its own influential daily newspaper, L’Osservatore Romano, and its press can print books and pamphlets in any of 30 languages, from old Ecclesiastical Georgian to Indian Tamil. Since 1983 the Vatican has produced its own television programming. Its radio broadcasts are heard in some 40 languages in many parts of the world. Vatican City was designated a UNESCO World Heritage site in 1984. More … Score: https://www.britannica.com/place/Vatican-City

2025/03/13

Independence Day the Republic of Mauritius

Mauritius, island country in the Indian Ocean, located off the eastern coast of Africa. Physiographically, it is part of the Mascarene Islands. The capital is Port Louis. Land Mauritius lies about 500 miles (800 km) east of Madagascar in the Indian Ocean. Its outlying territories are Rodrigues Island, situated about 340 miles (550 km) eastward, the Cargados Carajos Shoals, 250 miles (400 km) northeastward, and the Agalega Islands, 580 miles (930 km) northward from the main island. Mauritius also claims sovereignty over the Chagos Archipelago (including Diego Garcia), some 1,250 miles (2,000 km) to the northeast, although this claim is disputed by Britain. Relief and drainage The island of Mauritius is volcanic in origin and is almost entirely surrounded by coral reefs. The northern part is a plain that rises to a central plateau, varying in elevation from about 900 to 2,400 feet (270 to 730 metres) above sea level. The plateau is bordered by small mountains that may have formed the rim of an ancient volcano; the highest point (2,717 feet [828 metres]) is Piton de la Petite Rivière Noire in the southwest. The two major rivers, the Grand River South East and the Black River, are the primary sources of hydroelectric power. Lake Vacoas, one of the main reservoirs, is the chief source of water. Soils and climate More than half of the country’s area is arable, and it is almost entirely planted in sugarcane, the major export crop. Vegetables and tea for local consumption are also grown. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe Now The climate is maritime subtropical, with fairly uniform temperature throughout the year. Mean temperatures vary from the mid-70s F (low to mid-20s C) at sea level to the upper 60s F (upper 10s C) on the high plateau. Two seasons are recognized: hot (December to April) and cool (June to September). Annual rainfall varies from around 35 inches (900 mm) on the west coast to 60 inches (1,525 mm) on the southeast coast and about 200 inches (5,080 mm) on the central plateau. Plant and animal life The vegetation includes some 600 indigenous species, even though little original forest is left. The fauna includes the samber (a long-tailed, dark brown deer), tenrec (a spiny insectivore), and mongoose, as well as a variety of birds and insects. The island was once home to the dodo, a flightless bird that was extinct by 1681. Efforts began in the late 20th century to save several other species of endemic birds that were close to extinction. People Ethnic groups, languages, and religion Approximately two-thirds of the population is of Indo-Pakistani origin, most of whom are descendants of indentured labourers brought to work in the sugar industry during the 19th and early 20th centuries. About one-fourth of the population is Creole (of mixed French and African descent), and there are small numbers of people of Chinese and Franco-Mauritian descent. Although English is the official language, it is spoken by a very small percentage of the population. Creole, a French-based patois, is spoken by about four-fifths of the population and is the lingua franca of the country. Bhojpuri, an Indo-Aryan language, is spoken by one-tenth of the population, and French is spoken by a small percentage. Other languages spoken on the island include Hindi, Chinese, Marathi, Tamil, Telugu, and Urdu. Mauritians commonly speak two, three, or even more languages, and the educational system supports a wide range of language instruction. Religious affiliation varies: about half of the population is Hindu, about one-third is Christian (the majority of whom are Roman Catholic), and—with the exception of a small group of Buddhists—the majority of the remainder are Muslims. Settlement patterns The population density in Mauritius is the highest of African countries and is among the highest in the world. Overpopulation became a serious problem after the eradication of falciparum malaria by the early 1950s led to a sharp increase in population. Driven by government policy, supported by all the Mauritian religious communities, and assisted by the rapid pace of economic growth, the rate of natural increase dropped rapidly in the last decades of the 20th century, and it is now below the world average. Emigration, primarily to Britain and France, also helped slow the annual growth rate. The birth rate remains well below the world average, while the death rate is similar to the world average. Life expectancy—about 70 years for men and more than 75 years for women—is higher than the world average and is well above the average for African countries. About two-fifths of the country’s population is younger than age 30. Economy Mauritius has a mixed developing economy based on manufactured exports, agriculture, tourism, and financial services. Government efforts to diversify the economy after 1980 have been successful, and the island is no longer as completely dependent on sugar production as it was throughout most of its history. The gross domestic product, among the highest of African countries, grew more rapidly than the population in the 1990s and 2000s. Agriculture, forestry, and fishing Although the significance of the agricultural sector has diminished with efforts to diversify the economy, it is still important. Sugar production, generating about one-sixth of export earnings, occupies about four-fifths of the total arable land. Tea and tobacco are also cash crops. Subsistence crops include potatoes, tomatoes, and bananas. The livestock population primarily consists of poultry, sheep, goats, pigs, and cattle. Forests make up about one-fifth of the total land area of Mauritius. Rapid deforestation occurred during the colonial era, and non-native species were introduced to repopulate the forestland, including the slash pine (Pinus elliottii), which is predominant, Japanese cedar (Cryptomeria japonica), and Moreton Bay pine (Araucaria cunninghamii). Eucalyptus trees and trees that belong to the beefwood (Casuarina) family are also present. Roundwood is the primary forest product, of which some two-fifths is used for fuel; sawn wood is also produced. Mauritius is unique among countries in the region in that it consumes more wood products than it produces and must import the difference. Technical assistance from Japan and India is regenerating the fishing industry, which has grown in importance. Mauritius’s waters contain many species of fish with commercial value, including tuna, snapper, and grouper. Aquaculture is practiced with such species as channel bass and sea bream. Resources, power, and manufacturing Mauritius has few viable mineral resources. Basalt and lime are mined. Electricity is largely generated from imported petroleum, with a small percentage derived from hydropower. Sugar plantations often use bagasse—the fibre that remains from sugarcane after sugar-bearing juice is extracted—as fuel to produce electricity. There has been a steady increase in manufacturing since the 1970s. The Mauritius Export Processing Zone, which concentrates on labour-intensive processing of imported raw materials or semifinished goods for the export market, has successfully attracted foreign investment. Economically important manufactures include textiles, food processing, metal and metal products, and chemical products. Finance and trade Mauritius is home to many financial institutions, including a development bank, offshore banking facilities, and several commercial banks. The Bank of Mauritius is the central bank and issues the country’s currency, the Mauritian rupee. The country’s stock exchange is located in Port Louis. Imports, largely of machinery and transport equipment, petroleum, and foodstuffs, outweigh exports of clothing and textiles, sugar, and fish and fish products. Important trading partners include the United Kingdom, France, the United States, South Africa, and China. Services, labour, and taxation Significant growth in tourism since the 1970s has made it a major earner of foreign exchange. Information and communication technology is becoming increasing important. In 2001 the government created the Information and Communication Technologies Authority to promote and oversee the burgeoning sector. More than two-fifths of the labour force is employed in the areas of finance and services. Construction and manufacturing employ about one-third of the labour force, and about one-tenth is employed in the agricultural sector. Taxation is an important source of funding in Mauritius, accounting for about nine-tenths of the government’s revenue. About half of the total tax revenue is derived from taxes on goods and services. Trade taxes account for about one-fifth; corporate income tax, about one-eighth. Transportation and telecommunications Mauritius has a strong transportation infrastructure. The road system is well developed and in good repair, and almost all roadways are paved. Most of the country’s shipping activity is conducted through port facilities at Port Louis, which has been cultivated as a free port to encourage its development as an international shipping hub. An international airport is located at Plaisance, and there are other airports located throughout the country. Air Mauritius, the national carrier, flies many international routes. The island does not have any rail service. The country’s telecommunications sector is well developed and among the best in the region. There has been rapid progress in this area owing to the country’s growing information and communication technology industry. About three-fourths of the population has mobile phone service, and one-fourth has internet service. More … Score: https://www.britannica.com/place/Mauritius

2025/03/12

Visit Ghana: The Official Tourism Website of Ghana

Explore Ghana, the land of rich culture, heritage, warmth and rhythm. Discover where nature is still pure and warmth flows easily. Akwaaba!

2025/03/08

Independence Day the Republic of Ghana

Ghana, country of western Africa, situated on the coast of the Gulf of Guinea. Although relatively small in area and population, Ghana is one of the leading countries of Africa, partly because of its considerable natural wealth and partly because it was the first black African country south of the Sahara to achieve independence from colonial rule. In addition to being known for its lush forests, diverse animal life, and miles of sandy beaches along a picturesque coast, Ghana is also celebrated for its rich history its habitation possibly dating from 10,000 bce and as a fascinating repository of cultural heritage. The country takes it name from the great medieval trading empire that was located northwest of the modern-day state until its demise in the 13th century. Direct sea trade with Europe, established in the 15th century, had much impact on the area’s inhabitants, many of whom actively traded with the Portuguese, Dutch, British, and other Europeans. Forts and castles, many of which still dot the Ghanaian coast today, were constructed by Europeans to protect their trade interests. Although trading was originally centred on the gold that was readily available in the area (and from which the future British colony the Gold Coast would take its name), the focus shifted to the lucrative slave trade in the 17th century. The area later became known for growing cacao, the source of cocoa beans. Introduced there in the late 19th century, cacao continues to provide an important export for Ghana. Modern-day Ghana, which gained its independence on March 6, 1957, consists primarily of the former Gold Coast. The colony’s drive for independence was led by nationalist and Pan-African leader Kwame Nkrumah, who viewed Ghana’s sovereignty as being important not only for the Ghanaian people but for all of Africa, saying “Our independence is meaningless unless it is linked up with the total liberation of the African continent.” Indeed, more than 30 other African countries, spurred by Ghana’s example, followed suit and declared their own independence within the next decade. Nkrumah quickly laid the groundwork for fiscal independence within the new country as well, embarking on many economic development projects. Unfortunately, decades of corruption, mismanagement, and military rule stymied growth and achievement. By the 1990s, though, the country’s state of affairs began showing signs of improvement, and Ghana is now held up as an example of successful economic recovery and political reform in Africa. Ghana’s administrative capital is the coastal city of Accra. Originally founded on the site of several Ga settlements, Accra developed into a prosperous trading hub; today it serves as the commercial and educational centre of the county. Kumasi, another prominent commercial centre, is located in the south-central part of the country. Known as the “Garden City of West Africa,” Kumasi is also the seat of the king of the Asante people, the vestige of an empire (see Asante empire) that existed in the 18th and 19th centuries. Land Situated on the coast of the Gulf of Guinea in western Africa, Ghana is bordered to the northwest and north by Burkina Faso, to the east by Togo, to the south by the Atlantic Ocean, and to the west by Côte d’Ivoire. Relief and drainage Relief throughout Ghana is generally low, with elevations not exceeding 3,000 feet (900 metres). The southwestern, northwestern, and extreme northern parts of the country consist of a dissected peneplain (a land surface worn down by erosion to a nearly flat plain, later uplifted and again cut by erosion into hills and valleys or into flat uplands separated by valleys); it is made of Precambrian rocks (about 540 million to 4 billion years old). Most of the remainder of the country consists of Paleozoic deposits (about 250 to 540 million years old), which are thought to rest on older rocks. The Paleozoic sediments are composed mostly of beds of shales (laminated sediments consisting mostly of particles of clay) and sandstones in which strata of limestone occur in places. They occupy a large area called the Voltaian Basin in the north-central part of the country where the elevation rarely exceeds 500 feet (150 metres). The basin is dominated by Lake Volta, an artificial lake that extends far into the central part of the country behind the Akosombo Dam and covers about 3,275 square miles (8,500 square km). Along the north and south, and to some extent along the west, the uplifted edges of the basin give rise to narrow plateaus between 1,000 and 2,000 feet (300 and 600 metres) high, bordered by impressive scarps. The most outstanding are the Kwahu (Mampong) Scarp (see Kwahu Plateau) in the south and the Gambaga Scarp in the north. Surrounding the basin on all of its sides, except in the east, is the dissected Precambrian peneplain, which rises to elevations of 500 to 1,000 feet above sea level and contains several distinct ranges as high as 2,000 feet. Along the eastern edge of the Voltaian Basin, and extending from the Togo border to the sea immediately west of Accra, is a narrow zone of folded Precambrian rocks running northeast to southwest, forming the Akwapim-Togo Ranges, which vary in elevation from 1,000 to 3,000 feet (300 to 900 metres). The highest points in Ghana are found there, including Mount Afadjato (2,903 feet [885 metres]), Mount Djebobo (2,874 feet [876 metres]), and Mount Torogbani (2,861 feet [872 metres]), all situated east of the Volta River near the Togo border. These ranges are part of the Togo-Atakora Mountains, which extend northward into Togo and Benin. The southeastern corner of the country, between the Akwapim-Togo Ranges and the sea, consists of the gently rolling Accra Plains, which are underlain by some of the oldest Precambrian rocks known—mostly gneisses (coarse-grained rocks in which bands containing granular minerals alternate with bands containing micaceous minerals); in places they rise above the surface to form inselbergs (prominent steep-sided hills left after erosion). The only extensive areas of young rocks less than about 136 million years old are in the wide, lagoon-fringed delta of the Volta, about 50 miles (80 km) east of Accra, and in the extreme southwest of the country, along the Axim coast. In the east the predominant rocks are less than 65 million years old, though there is a patch of Cretaceous sediments (about 65 to 145 million years old) near the Ghana-Togo border. To the west of Axim, near the Côte d’Ivoire frontier, the rocks date to the Cretaceous Period. The intervening coastal zone between eastern and western extremes contains patches of Devonian sediments (about 360 to 415 million years old). With the older and more resistant rocks of the Precambrian peneplain, these form a low, picturesque coastline of sandy bays and rocky promontories. The drainage system is dominated by the Volta River basin, which includes Lake Volta and the Black Volta, White Volta, and Oti rivers. Most of the other rivers, such as the Pra, the Ankobra, the Tano, and a number of smaller ones, flow directly south into the ocean from the watershed formed by the Kwahu Plateau, which separates them from the Volta drainage system. South of Kumasi, in the south-central part of the country, is Ghana’s only true natural lake—Bosumtwi—lying in a meteorite impact crater and without any outlet to the sea. Along the coast are numerous lagoons, most of them formed at the mouths of small streams. Over much of the surface of Ghana, the rocks are weathered, and great spreads of laterite (red, leached, iron-bearing soil) and lesser spreads of bauxite and manganese are found on the flat tops of hills and mountains. Although the movements of Earth’s crust that produced the basic geologic structure of the country have now virtually ceased, periodic earthquakes occur, especially near Accra along the eastern foot of the Akwapim-Togo Ranges, where there is a major fault line. More … Score: https://www.britannica.com/place/Ghana

2025/03/06