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!

2024/03/08

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

2024/03/06

Visit Ghana 2020

The whole world is heading to Ghana in 2020 to experience our culture, warmth, adventure, heritage, ecotourism, beautiful coast and above all our uniquely welcoming people. Come and discover yourself in 2020, 2021, 2022...

2024/03/05

Information Bulgaria - Comprehense Guide About Everything

Information Bulgaria the most comprehensive covering everything you could want to know from hotels in Sofia, the weather and it's history plus much more.

2024/03/05

Bulgaria's Liberation Day

Bulgaria, officially Republic of Bulgaria, Bulgarian Republika Bŭlgariya, country occupying the eastern portion of the Balkan Peninsula in southeastern Europe. Founded in the 7th century, Bulgaria is one of the oldest states on the European continent. It is intersected by historically important routes from northern and eastern Europe to the Mediterranean basin and from western and central Europe to the Middle East. Before the creation of the Bulgarian state, the empires of ancient Rome, Greece, and Byzantium were strong presences, and people and goods traveled the land with frequency. Emerging from centuries of Ottoman rule, Bulgaria gained its independence in the late 19th century, joined the losing side of several conflagrations in the first half of the 20th century, and, despite gravitating toward the Axis powers in World War II, found itself within close orbit of the Soviet Union by mid-century. This alliance had profound effects on the Bulgarian state and psyche, altering everything from land use and labour practices to religion and the arts. As communist governments fell in eastern Europe in the late 1980s and early 1990s, Bulgaria was suddenly released from the magnetic field of the Soviet giant and drifted into the uneasy terrain of postcommunism. Today its gaze is firmly fixed on the West; Bulgaria became a member of the North Atlantic Treaty Organization (NATO) in 2004 and of the European Union (EU) in 2007. The members of the EU engage in the bulk of Bulgarian trade. The country is remarkable for its variety of scenery; its rugged mountains and relaxing Black Sea resorts attract many visitors. Like other nations of the Balkan Peninsula, Bulgaria claims a mix of Eastern and Western cultures, and the mingling is evident in its cuisine, its architecture, and its religious heritage. Though located in western Bulgaria, the capital, Sofia, is neatly positioned near the geographic centre of the Balkan region, and in nearly every other respect it occupies the central position within Bulgaria. With more than one million inhabitants, Sofia has three times as many people as the next largest cities, Plovdiv and Varna. The Bulgarian writer Yordan Radichkov has placed the capital along the axis of two major transnational routes: (1) the historic Silk Road that connects China and the West and (2) a major natural path of migrating birds known as the “grand route of Aristotle.” According to Radichkov, “The universal core of Bulgaria is to be found at the crossroads of these two routes.” Land Nearly rectangular in outline, Bulgaria is bounded by Romania to the north, with most of the border marked by the lower Danube River. The Black Sea lies to the east, Turkey and Greece to the south, North Macedonia to the southwest, and Serbia to the west. The capital city, Sofia, lies in a mountainous basin in the west. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe Now Relief Within a relatively small compass, the Bulgarian landscape exhibits striking topographic variety. Open expanses of lowland alternate with broken mountain country, cut by deep river gorges and harbouring upland basins such as that in which Sofia lies. Three basic structural and physiographic divisions run east-west, splitting the country into the traditional regions of North Bulgaria, including the Danubian Plain and the Balkan Mountains; South Bulgaria, including the Rila-Rhodope Massif; and a transitional area between them. North Bulgaria All but a short section of the northern frontier of Bulgaria is marked by the lower Danube River. The abrupt and often steep banks on the Bulgarian side contrast with the swamps and lagoons of the Romanian side. Extending southward from the Danube to the foothills of the Balkan Mountains is the fertile, hilly Danubian Plain. The average elevation of the region is 584 feet (178 metres), and it covers some 12,200 square miles (31,600 square km). Several rivers cross the plain, flowing northward from the Balkans to join the Danube. The Balkan Mountains border the Danubian Plain on the south. Their rounded summits have an average height of 2,368 feet (722 metres) and rise to 7,795 feet (2,376 metres) at Mount Botev, the highest peak. Transitional region The mountain chain is larger than the adjacent ranges that run parallel in a transitional region of complex relief. Block faulting—the raising or lowering of great structural segments along regular lines of crustal weakness—has produced there the Sredna Mountains, the Vitosha Massif near Sofia, a number of sheltered structural basins, and the Upper Thracian and Tundzha lowlands. South Bulgaria Another mountain mass covers southern Bulgaria. This includes the Rhodope Mountains (Bulgarian: Rodopi; Greek: Rhodopis), which rise to 7,188 feet (2,190 metres) at Golyam Perelik Peak; the Rila Mountains, rising to 9,596 feet (2,925 metres) at Musala Peak, which is the highest point in the country and indeed in the whole Balkan Peninsula; the Pirin Mountains, with Vikhren Peak reaching 9,560 feet; and a frontier range known as the Belasitsa Mountains. These majestic ranges discharge meltwater from montane snowfields throughout the summer, and their sharp outlines, pine-clad slopes, and, in the Rila and Pirin ranges, several hundred lakes of glacial origin combine to form some of the most beautiful Bulgarian landscapes. Coastal region Trending north-south at the eastern fringe of three principal regions is the narrow Black Sea coastal region. With the exception of the fine harbours of Varna and Burgas, the coast has few bays, but it does have extensive stretches of sandy beach that are features of a number of picturesque seaside resorts. More … Score: https://www.britannica.com/place/Bulgaria  

2024/03/03

Bulgaria 8K HDR 60P (FUHD)

We were invited to Bulgaria by "Our Home is Bulgaria" to explore the country for the first time this year and it was an amazing experience to travel through this space with so much history and diverse landscapes. Some of the places we feature here are the Seven Rila Lakes, Alexander Nevsky Cathedral, Thracian Tomb of Kazanlak, Belogradchik Fortress, Devetashka cave, and Mount Buzludzha.

2024/03/02

Dominican Republic Tourism Official Website ...

Known for our warm and hospitable people, Dominican Republic is a destination like no other, featuring astounding nature, intriguing history and rich culture.

2024/02/29

TOURISTIC ENTERPRISES COMPANY | KUWAIT TOURISM

Touristic Enterprises Company is a leading government-owned Kuwait tourism company in Kuwait. Explore Kuwait, Kuwait towers, Cable Park, Yacht club, ...

2024/02/27

Independence Day of the Dominican Republic

Dominican Republic, country of the West Indies that occupies the eastern two-thirds of Hispaniola, the second largest island of the Greater Antilles chain in the Caribbean Sea. Haiti, also an independent republic, occupies the western third of the island. The Dominican Republic’s shores are washed by the Caribbean to the south and the Atlantic Ocean to the north. Between the eastern tip of the island and Puerto Rico flows the Mona Passage, a channel about 80 miles (130 km) wide. The Turks and Caicos Islands are located some 90 miles (145 km) to the north, and Colombia lies about 300 miles (500 km) to the south. The republic’s area, which includes such adjacent islands as Saona, Beata, and Catalina, is about half the size of Portugal. The national capital is Santo Domingo, on the southern coast. The Dominican Republic has much in common with the countries of Latin America (with which it is often grouped), and some writers have referred to the country as a microcosm of that region. Dominicans have experienced political and civil disorder, ethnic tensions, export-oriented booms and busts, and long periods of military rule, including a Haitian occupation (1822–44), the oppressive dictatorship of Rafael Trujillo (1930–61), and military interventions by the United States (1916–24 and 1965–66). However, the nation’s troubles have paled in comparison with those of neighbouring Haiti. The two countries have long been strategic because of their proximity to the United States and their positions on major sea routes leading to the Caribbean and the Panama Canal. The land Relief, drainage, and soils The Dominican Republic includes the highest and lowest elevations in the West Indies. Its major mountain ranges and elongated, fertile valleys mainly extend from northwest to southeast. The Cordillera Septentrional, the northernmost range, looms above a narrow coastal plain drained by such short rivers as the Balabonico and the Yasica. The southern slopes of the mountains give way to the extensive Cibao Valley, which stretches from Manzanillo Bay in the northwest to the Samaná Peninsula and the Bay of Samaná in the east. The valley’s fertile soils are fed by two of the nation’s main river systems: the Yaque del Norte, which flows generally northwestward, and the Camu-Yuna system, which flows eastward. The Cordillera Central, the island’s most rugged and imposing feature, is known in Haiti as the Massif du Nord (“Northern Massif”). In Dominican territory its crest line averages some 6,000 feet (1,800 metres) in elevation and rises to 10,417 feet (3,175 metres) at Duarte Peak, the highest mountain in the Caribbean. Other prominent peaks are Yaque, La Rucilla, Bandera, and Mijo. Tributaries of the Yaque del Norte drain most of the range’s northern flanks, whereas its southern flanks are drained by the Yaque del Sur system and the Ocoa, Nizao, and other smaller rivers. The San Juan River, one of the Yaque del Sur’s main tributaries, is the centrepiece of the fertile San Juan Valley, which connects with Haiti’s Central Plateau via the upper Artibonite River valley. Bounding the San Juan Valley to the south is the Sierra de Neiba, which corresponds to the Matheux and Trou d’Eau mountains of Haiti; its high peaks reach approximately 7,200 feet (2,200 metres). Water flowing off the Neiba range drains partly to the Caribbean, via the Yaque del Sur system, and partly inland, to saline Lake Enriquillo. Enriquillo is the country’s largest natural lake, about 23 miles (37 km) long and up to 11 miles (18 km) wide; the lake’s surface is also the lowest point in the West Indies, at 144 feet (44 metres) below sea level. The Dominican Republic’s southernmost range, the Sierra de Baoruco (Bahoruco), is called the Massif de la Selle in Haiti; it overlooks Cape Beata and the arid southwestern plain, including the largely infertile Pedernales region. The Cordillera Oriental forms the country’s less-rugged eastern spine, separating a narrow coastal plain to the north from a wider belt of rolling lowlands to the south, where most of the country’s sugarcane is grown. The region’s main rivers all flow to the Caribbean, including the Ozama, which reaches the coast at Santo Domingo, and the Macorís, Soco, Chavón, and Yuma. The country’s most fertile alluvial soils are located in the valleys of the Yaque del Norte, Yuna, San Juan, and Yaque del Sur rivers, as well as the Ozama and various smaller rivers in the southeast. The mountain slopes have lower-quality soils and are generally covered in forests and grasslands. Salt deposited around Lake Enriquillo creates some of the nation’s only unproductive soils. Climate The Dominican Republic has a moderate, relatively mild tropical climate, although it lies well within the tropical zone. Conditions are ameliorated in many areas by elevation and by the northeast trade winds, which blow steadily from the Atlantic all year long. The annual mean temperature is 77 °F (25 °C); regional mean temperatures range from 69 °F (21 °C) in the heart of the Cordillera Central to as high as 82 °F (28 °C) on the coastal plains. Temperatures rarely rise above 90 °F (32 °C), and freezing temperatures are unknown. The heaviest precipitation is in the mountainous northeast (the windward side of the island), where the average annual rainfall is more than 100 inches (2,540 mm). As the trade winds pass over the country, they lose their moisture on various mountain slopes, so that the far western and southwestern valleys, along the Haitian border, remain relatively dry, with less than 30 inches (760 mm) of annual precipitation. The northwestern and southeastern extremes of the country are also arid. The Dominican Republic is occasionally damaged by tropical storms and hurricanes, which originate in the mid-Atlantic and southeastern Caribbean from August until October each year; hurricanes in 1930, 1954, 1979, and 1998 were particularly devastating. Plant and animal life Vegetation varies considerably, but there is generally more ground cover in the Dominican Republic than in neighbouring Haiti. The mountains are still largely forested with pines and tropical hardwoods, although the trees on the lower and more accessible slopes have been severely cut for use as charcoal and commercial lumber. In the drier regions low shrubs and scrub predominate, but grasslands and dense rainforests occur where there is heavier precipitation. Royal palms grow throughout much of the country. Cultivated crops have largely replaced the natural vegetation in many areas, particularly in the more fertile upland valleys and on the lower mountain slopes. Mangrove swamps line some coastal areas, whereas extensive sandy beaches are found elsewhere, notably along the northern shore. Wild animals are not abundant; for several centuries cattle and goats, introduced by the early Spanish colonists, ran wild on the grasslands and in the desert areas. Alligators are found near the mouths of the Yaque rivers and in the waters of Lake Enriquillo. A great variety of birds, including ducks, are hunted. Fish and shellfish inhabit the surrounding waters, particularly within the coral reefs. Settlement patterns The nation’s coasts and interior plains have been inhabited since Arawak Indians maintained villages there in pre-Columbian times. Settlement from the late 15th century was closely tied to sugarcane plantations and export-oriented commerce. Throughout the colonial period the population of European colonists and African slaves grew slowly, and their mulatto (mixed African and European) descendents now predominate in most regions of the country. People of mainly European descent inhabit the southeastern savannas, which include large sugar plantations, cattle ranches, and small and medium-size farms. However, the southeastern coastline itself is increasingly inhabited by Blacks from Haiti and other West Indian nations who have gone there to work on the plantations, in the mills, or on the docks; most are temporary or seasonal workers. Many of the inhabitants of the town of Azua and its environs are the descendants of immigrants from the Canary Islands.Santo Domingo, the nation’s largest city, is central to one of the nation’s most densely populated regions; founded by the Spanish in 1496, it was the first permanent town established by Europeans in the Americas. The Cibao Valley is also densely settled, particularly in its central and eastern sections at Santiago, San Francisco de Macorís, and La Vega. Santiago, the nation’s second largest city, vies with Santo Domingo in political, cultural, and economic matters. Secondary coastal centres include La Romana and San Pedro de Macorís in the southeast, Barahona in the southwest, and Puerto Plata in the north. South of the Cordillera Central lies an alluvial plain where rice is grown; its population is centred on San Juan de la Maguana. Traditionally, the Dominican Republic had a large rural population, but growing numbers have moved to cities and towns since the mid-20th century, and today about fourth-fifths of the population is urban In rural areas some settlements exist as well-defined villages, but most take the form of scattered neighbourhoods, typically clustered around a small store or church or stretched along a roadside, with cultivated patches behind the houses. In addition, there are still many households so isolated from roadways that they can be reached only on foot or horseback. The people - Ethnicity The population of the Dominican Republic is predominantly of mixed African and European ethnicity, and there are small Black and white minorities. It has long been believed that few people are descended, even indirectly, from the indigenous Taino peoples, who were largely decimated by disease, warfare, and the effects of forced labour shortly after their first contact with Europeans. Some scholars, however, have argued that Taino legacy is more pronounced than this, both genetically in the current population and in terms of survival elements in Dominican language and material culture. The colonizing whites, mostly Spaniards, were joined in the 19th and 20th centuries by immigrants from East Asia and from such European countries as France, Italy, England, and Germany, as well as by small numbers of Sephardic Jews and Arabs from North Africa and the Middle East. This last group of immigrants at first competed with Chinese peddlers and shopkeepers in the rural areas, but most later moved to the cities, where they now occupy positions in commerce and industry. The Chinese particularly established themselves in the hotel and restaurant business. A small group of Japanese developed truck farming in the Constanza River valley before World War II, and their descendants are now found throughout the republic. Intermarriage among all these groups has blurred, but not erased, their ethnic origins. The exact African heritage of the large Black population is unknown, although many of their ancestors arrived as slaves from West Africa. Some were brought in within the first two decades of the Spanish conquest to work in mines and early sugar plantations. Others came indirectly, via the French colony of Saint-Domingue (later independent Haiti), particularly during the early 19th century when Haitian troops occupied the Dominican Republic. Haitian workers without immigration papers have long crossed over the mountainous frontier between the two countries; other Haitians have worked legally in the south as itinerant cane cutters, and some have found ways to remain after their contracts expired. Language and religion The Spanish language has always been predominant, although English is becoming more common because of continued emigration to the United States—which has been accompanied by continual visiting back and forth—plus some repatriation. A French Creole is spoken among Haitian immigrants. More than four-fifths of the people are adherents to the Roman Catholic church, which exerts a marked influence on all levels of cultural, political, and economic life. Many of the religious beliefs and practices of the rural populace are syncretic, rooted in the cultures of both the early Spanish and African communities. Evangelical groups account for a small but growing segment of the population. There are a few adherents of Judaism and other religions. Demographic trends The rate of population increase in the Dominican Republic is greater than in most other West Indian nations, and about three-tenths of the population is less than 15 years of age. Both birth and death rates in the republic have long been higher than the regional average, although they have been lower than in Haiti (see Health and welfare). The country experienced one of the world’s highest urbanization rates in the late 20th century: in 1950 roughly one-fourth of Dominicans lived in cities, but by the late 1990s nearly two-thirds of the population was urban. Santo Domingo expanded into formerly rural zones as it became more crowded, and its urban slums grew as well. Santiago, La Romana, and other cities also grew considerably. The Dominican Republic’s high rate of emigration has been primarily directed to New York City and other cities in the United States. Since the mid-1960s more than one-tenth of the total population has emigrated, principally to improve their economic situation; many have been illegal immigrants. The outward flow of people alleviated the strain on local resources (notably housing, water supplies, and food production) while boosting many families’ incomes with remittances of cash and consumer goods. More … Source: https://www.britannica.com/place/Dominican-Republic

2024/02/27