Independence Day of the Community of Dominica

Dominica, island country of the Lesser Antilles in the eastern Caribbean Sea. It lies between the French islands of Guadeloupe and Marie-Galante to the north and Martinique to the south. The country has been a member of the Commonwealth since independence in 1978. The island is 29 miles (47 km) long and has a maximum breadth of 16 miles (26 km). The capital and chief port is Roseau. Dominica’s great natural beauty, especially its spectacular mountainous topography, has impressed generations of nature lovers. Land - Relief, drainage, and soils The island is of volcanic formation. Dominica has a number of active volcanoes, although eruptions are rare. Other signs of geothermal activity include fumaroles (volcanic vents) and hot springs. In the south, Boiling Lake lies 2,300 feet (700 metres) above sea level; its waters are often forced 3 feet (1 metre) above normal by the pressure of escaping gases. The island has rich alluvial and volcanic soils. There are numerous rivers, all of them unnavigable. A range of high forest-clad mountains runs north to south, broken in the centre by a plain drained by the Layou River, which flows to the west; the highest points are Mount Diablotins (4,747 feet [1,447 metres]) and Mount Trois Pitons (4,670 feet [1,424 metres]). Climate Dominica has a pleasant climate, particularly during the cooler months from December to March. Summer temperatures reach an average high of 90 °F (32 °C). Winter temperatures are not much lower, the average high being anywhere from 84 to 86 °F (29 to 30 °C). The dry season is from February to May, and the rainy season is from June to October, the most likely period for hurricanes (tropical cyclones). Rainfall varies, being especially heavy in the mountainous interior. Average annual coastal rainfall varies from about 60 inches (1,500 mm) to 145 inches (3,700 mm), but in the mountains average rainfall can reach 250 inches (6,350 mm). Plant and animal life Dominica is the most heavily forested island of the Lesser Antilles. The forest is the habitat of a considerable variety of birds and animals. Two parrots—the imperial parrot, or sisserou (Amazona imperialis), and the smaller red-necked parrot (Amazona arausiaca)—are found only in Dominica. There are many hummingbirds, of which the blue-headed (Cyanophaia bicolor) is native only to Dominica and the neighbouring island of Martinique. The large frog known as crapaud or mountain chicken (Leptodactylus fallax), one of four amphibian species on the island, was long an emblematic part of Dominica’s fauna (and a national dish), but it has become highly endangered because of a fungal disease. People The population is mainly of African descent, with some Europeans, people from the Indian subcontinent, and Caribs. Dominica is the only island with a relatively large and distinctive group of Carib Indians, descendants of the people who inhabited the island before European colonization. Most of the remaining Caribs, a small number of whom are solely of Carib descent, live in the approximately 3,700-acre (1,500-hectare) Carib Territory in the east of the island and are among Dominica’s poorest residents. English is the official language, but a French patois is commonly spoken, and the original Carib language is evidenced in a number of place-names. The majority of the population is Roman Catholic, but there are also Methodists, Pentecostals, and Seventh-day Adventists. Dominica experienced out-migration throughout the 1970s, a trend that culminated with a massive exodus after Hurricane David in 1979. This wave continued in the 1980s but moderated in the 1990s. In 1992 the government initiated a controversial scheme to offer “economic citizenship” to investors from other countries. Economy Dominica is one of the poorest of the Caribbean countries. Its economy is dependent upon agriculture, which is intermittently destroyed by hurricanes. Attempts to diversify have had some success, with a growing tourism industry and a small offshore financial sector. Agriculture, forestry, and fishing Agriculture remains the most important sector of the economy, in terms of both employment and contribution to the gross national product. The main crops are bananas, citrus fruits, and coconuts. Bananas accounted for nearly half of Dominica’s export earnings in the 1980s, but in the late 20th and early 21st centuries the banana crops were devastated repeatedly by hurricanes. Production also fell in the 1990s in part as a result of a World Trade Organization ruling that the European Union had breached free-trade rules by offering Dominica and other former European colonies—notably, other eastern Caribbean banana-producing islands—preferential access to the European market. Cocoa, coffee, and vegetables are also produced. Dominica is self-sufficient in fruit and vegetables and exports foodstuffs to Guadeloupe. The forests have potential for marketable timber. The fishing industry was devastated by Hurricane David in 1979, when nearly all of the island’s fishing boats were destroyed, but, beginning in the 1990s, a new fishing port and market were built at Roseau (and subsequently repaired and renovated) with Japanese financial support. Resources Pumice, a volcanic rock used chiefly for building purposes, is the most important commercial mineral. There are also deposits of clay and limestone. Extensive copper deposits in the northeast have been investigated for possible exploitation. Manufacturing, trade, and services Most of the main products and exports are derived from the agricultural sector; they include copra, coconut oil, soap, bay oil, and fruit juices. Soap, derived from coconut oil, is an important export. There is a small garment-assembly sector. Wood products, including furniture, are produced from local timber. Portsmouth is the main boatbuilding centre. Imports include food, mineral fuels, and manufactured goods. Tourism developed dramatically in the late 20th century despite the island’s poor transportation infrastructure and the relative lack of hotel facilities and good beaches. Approximately 80,000 “stay-over” tourists visit the island each year, while the ports of Prince Rupert Bay and Roseau serve more than 300,000 cruise-ship passengers on day visits annually. The island has sought to develop reserves of its unique flora and fauna to attract tourists and markets itself as the “nature island” of the Caribbean. High rainfall and rugged terrain have impeded road building in Dominica. The first road across the island was not completed until 1956, and it was not until 1984 that a major road-rehabilitation project was launched to greatly improve accessibility. The main airport is Melville Hall, located at Marigot, on the northeast coast. A second airport is at Canefield, near Roseau. Larger vessels use the deepwater port at Woodbridge Bay near Roseau, but Portsmouth remains the major banana-shipping port. Government and society Constitutional framework The constitution adopted at independence provides for a president as head of state and a prime minister as head of government. The legislative branch of government, called Parliament, consists of the president (ex officio) and a single-chamber House of Assembly. Of the 32 total house members, 21 are elected from constituent districts; 9, called senators, are presidential appointees; and 1, the speaker, is elected either from among members who do not belong to the cabinet or from outside the House of Assembly. The attorney general is also considered a member of the house. The president is elected by the legislature, and the prime minister is appointed by the president from among the elected members of the House of Assembly. The prime minister heads a cabinet chosen by the president from among members of the house, although no more than three cabinet members may be senators. Terms of office are for five years, and there is universal adult suffrage. Dominica is a member of the Commonwealth, the United Nations, the Organization of American States, the Caribbean Community, and the Organisation of Eastern Caribbean States (OECS). Dominica uses the Eastern Caribbean dollar (EC$), the common currency of the OECS. Health and welfare There are several major hospitals. Local medical needs are handled by health centres throughout the island. Intestinal diseases, diabetes, anemia, tuberculosis, and sexually transmitted diseases constitute the major health problems of Dominica. Education Primary education is compulsory and free in government-run schools. There are many secondary schools, a teacher-training college, a medical school, a nursing school, and a branch of the University of the West Indies. Literacy is estimated at nearly 90 percent. More … Score: https://www.britannica.com/place/Dominica

2026/11/03

Visit Antigua & Barbuda – The beach is just the beginning

Antigua and Barbuda Tourism Authority (ABTA), the Official source for destination information for a perfect travel experience! Official hashtag ..

2026/11/03

Independence Day of the Republic of Panama

Panama, country of Central America located on the Isthmus of Panama, the narrow bridge of land that connects North and South America. Embracing the isthmus and more than 1,600 islands off its Atlantic and Pacific coasts, the tropical nation is renowned as the site of the Panama Canal, which cuts through its midsection. It is equally well known for its natural beauty, for its diverse plant and animal life, including hundreds of bird and tree species, and for its vibrant music and culture. The home of several Native American peoples, such as the Guaymí, Kuna, and Chocó, Panama became the first Spanish colony on the Pacific. Celebrated as “the door to the seas and key to the universe,” it served in the 1530s as the staging point for the Spanish conquest of the Inca empire, and until the 19th century it was a transshipment point for gold and silver destined for Spain. With the independence of Colombia, which once controlled Panama, from Spain, Panama came to serve as another staging point, this time for oceangoing migrants to the gold fields of California. Since 1914 the 51-mile- (82-km-) long Panama Canal, which connects the Atlantic and Pacific Oceans, has afforded a long-sought shortcut for shipping and assures the country’s standing as one of the most strategic transportation hubs of the world. The canal also secures Panama’s ongoing role in international affairs and world commerce. The United States relinquished jurisdiction of the Panama Canal on December 31, 1999, marking an unprecedented shift in Panamanian society. For the first time in nearly a century as an independent nation, Panama controlled the entirety of its national territory. Panama enjoys a lively mix of cultural influences, expressed in the country’s cuisine, artwork, music, and literature. Its capital, Panama City, is located on the Pacific coast just east of the canal. A cosmopolitan city where skyscrapers tower above whitewashed bungalows, it enjoys a handsome setting and a growing importance as a commercial and financial services centre for the region. However, its economic progress has been hampered periodically by environmental problems and political turmoil. Land - Relief Panama is bounded to the north by the Caribbean Sea (an extension of the Atlantic Ocean) and to the south by the Pacific Ocean. It has an elongated S shape, with its Caribbean coastline stretching some 800 miles (1,290 km) and the Pacific coast some 1,060 miles (1,700 km); however, a line drawn from the Costa Rican frontier in the west to the Colombian border in the east would extend only 480 miles (770 km). The shortest distance across the isthmus is about 30 miles (50 km), from the mouth of the Nergalá (Necategua) River, which flows into the Gulf of San Blas on the Caribbean shore, to the mouth of the Chepo River on the Pacific coast. Nearly as narrow is the portion of the isthmus traversed by the Panama Canal. A central spine of mountain ranges extends almost the entire length of Panama, dividing the country into Atlantic- and Pacific-facing slopes. The two principal ranges, the Tabasará Mountains (Cordillera Central) in the west and the Cordillera de San Blas in the east, are separated near the centre of the country by a saddle of lower land. This depression (the Panama Canal site) divides the country again—roughly into western and eastern halves. Of the four quadrants thus formed, the southwestern has the largest number of settlements; however, the environs of the canal account for most of Panama’s population and commerce. The country’s highest peak is an inactive volcano, Barú (Chiriquí), which reaches an elevation of 11,401 feet (3,475 metres). Paralleling the principal mountain chains, a lower mountain arc extends along Panama’s southern coast. It appears only in well-separated segments—for example, on Azuero Peninsula as the Canajagua Massif and in eastern Panama as the Sierra de Jungurudó, Sapo Mountains, and the Majé Mountains. The highlands and mountains are made up primarily of igneous (volcanic) rocks. The lowlands include the plains of Panamá and Chiriquí provinces, the plains and hills of Colón province, the Chepo and Chucunaque river basins in the east, and the narrow northeastern plains of the Caribbean region. Sedimentary rocks such as slates and shales underlie most of the lowland zones. The Pacific coastline is extended by the Azuero Peninsula and the Gulf of Panama and by numerous headlands and bays, whereas the largest embayment on the Caribbean side is Chiriquí Lagoon. The Pacific coastline is more indented and irregular, and its continental shelf is much wider than that on the Atlantic side. In addition, most of the republic’s more than 1,600 islands lie off its Pacific coast; they include the Perlas Archipelago (Pearl Islands) and the islands of Taboga, Cébaco, Parida, Jicarón, and Coiba, the largest. The principal archipelagoes off the Caribbean coast are those of Bocas del Toro and San Blas. Drainage and soils Of Panama’s many short rivers, those that flow to the Caribbean include the Sixaola, Changuinola, Indio, Cricamola, La Miel, and Chagres. Rivers flowing to the Pacific include the Chiriquí Viejo, Santa María, Chepo, Chucunaque, and Tuira. During the rainy season the Tuira is navigable for some 40 miles (60 km) and the Chepo for 20 miles (30 km). Water in the Panama Canal does not flow from coast to coast; rather, it is released from the rain-fed Gatún and Alajuela (Madden) lakes in the central highlands. In effect, the water flows to both coasts simultaneously via the canal’s system of locks and dams. For details on the engineering and operation of the waterway, see Panama Canal. Soils are commonly reddish to brown and rich in clay. They vary in fertility, and in many areas crops can be grown continuously only if fertilizers are applied. On poorer soils, a shifting subsistence agriculture is practiced. Under this system small plots are cleared, cropped for a few years, then abandoned until their natural fertility is restored—a practice called roza in Panama. Areas of alluvial soils (which develop from clay, silt, sand, and gravel deposited by streams) are especially fertile but are limited to the lower parts of river valleys. The commercial banana plantations around Puerto Armuelles and in western Bocas del Toro province are mainly on alluvial soils. Some of the soils along the inland edges of coastal mangrove swamps have also proved productive. In some areas, exceptionally fertile soils have developed from volcanic ash. Climate of Panama Climatic conditions are markedly different on the Atlantic and Pacific sides of western Panama, especially in the amount and seasonal distribution of rainfall. On the Caribbean slopes of the Tabasará Mountains, which face the rain-bearing trade winds, average rainfall is approximately twice as heavy as on the leeward Pacific slopes. The Caribbean coast receives 60–140 inches (1,500–3,550 mm) per year, while the more populated Pacific region receives 45–90 inches (1,140–2,290 mm). Furthermore, on the Caribbean side rain falls almost throughout the year, while on the Pacific side there is more seasonal variation—in Chiriquí province, for example, there is a pronounced dry season lasting from January to April, and March is usually the driest month. In accordance with this rainfall pattern, tropical rainforests are typical on Caribbean slopes, whereas savannas (tropical grasslands) are more common southward in the seasonally dry areas between the Tabasará Mountains and the Pacific shoreline. Toward the Colombian border both sides of the isthmus have year-round rainfall. Because of Panama’s tropical location, the mean temperature of the coldest month seldom drops below 78 °F (26 °C) on either coast. The Panamanian mountain slopes create three climatic zones: a low, hot zone, lying at elevations below 2,300 feet (700 metres), which makes up nearly nine-tenths of the country’s territory; a temperate zone, at elevations ranging from 2,300 to 4,900 feet (700 to 1,500 metres), which accounts for most of the rest of the land; and a tiny cold zone, lying above 4,900 feet. Each zone has its characteristic plant growth and crops; cacao and bananas are produced mainly in the hot lowlands, whereas coffee is grown in the temperate zone. More … Score: https://www.britannica.com/place/Panama  

2026/11/03

We Are Micronesia

A slide show of some beautiful images of the Federated States of Micronesia in the Pacific.

2026/11/02

The best things to do in Dominica

Dominica is fast becoming my favourite country in the Caribbean. Unlike a lot of other islands around with beautiful pristine beaches and packed holiday resorts, Dominica is a million miles away from that.

2026/11/02

Welcome to Panama

Watch the diversity KLM's destination Panama has to offer. Panama A Unique Experience. Visit Panama will give you a taste of Panama with the old and new Panama city, the Panama Canal, Rain Forest, the Caribbean and Pacific Coasts. Special attention is given to the Caribbean archipelagos Bocas Del Toro and San Blas.

2026/11/02

Independence Day of Antigua and Barbuda

Antigua and Barbuda, islands that form an independent state in the Lesser Antilles in the eastern Caribbean Sea, at the southern end of the Leeward Islands chain. There is one dependency, the small island of Redonda. The capital is St. John’s, on Antigua. Land Antigua’s coastline is intricate, with bays and headlands fringed with reefs and shoals; several inlets, including Parham and English Harbour, afford anchorage for shipping, and St. John’s has a deepwater harbour. The island has an area of 108 square miles (280 square km). It is mostly low and undulating, but in the west there are volcanic rocks that rise to 1,330 feet (405 metres) at Mount Obama (formerly Boggy Peak). An absence of mountains and forests distinguishes Antigua from the other Leeward Islands. Because there are no rivers and few springs, droughts occur despite a mean annual rainfall of some 40 inches (1,000 mm). The average January temperature is around 77 °F (25 °C); that of August, 82 °F (28 °C). Summer highs can reach 90 °F (32 °C). Barbuda, formerly Dulcina, lies 25 miles (40 km) north of Antigua. A coral island, flat and well-wooded, with highlands rising to 143 feet (44 metres) at Lindsay Hill in the northeast, it is 62 square miles (161 square km) in area. Barbuda is without streams or lakes and receives less rainfall than Antigua. Codrington, the only settlement, lies on a lagoon to the west. The climate is similar to that of Antigua. Redonda, an uninhabited rock, lies 25 miles (40 km) southwest of Antigua. It rises sheer to a height of 1,000 feet (305 metres) and is 0.5 square mile (1.25 square km) in area. Phosphate deposits are located there. People The majority of the population is of African descent. Most of Antigua’s inhabitants live in St. John’s. The language is English, and some two-thirds of the people are Christian. The single largest denomination is Anglicanism. There are also large proportions of Seventh-day Adventists, Pentecostals, Moravians, and Methodists. Economy Agriculture, once the mainstay of the economy, has been largely supplanted by tourism. Sugarcane was long the dominant crop on Antigua, but its production is now insignificant. Barbuda was never involved in the sugar plantation system, its inhabitants always having been fishermen and subsistence farmers. Their traditional system of land tenure is threatened by tourism development. Fruits and vegetables, including citrus fruits, mangoes, and eggplants, are now cultivated on the islands. Manufacturing plays a small role in the economy; most activity involves processing agricultural products and making clothing and textiles and concrete blocks. An international airport is near St. John’s. Government and society Antigua and Barbuda is a constitutional monarchy with a parliamentary form of government. The British monarch is nominal head of state, represented by a governor-general. The constitution allows for a two-chamber legislature, consisting of a Senate and a House of Representatives. Executive power is vested in a Council of Ministers headed by the prime minister, who is the head of government. Primary and postprimary education is compulsory. History of Antigua and Barbuda Antigua was visited in 1493 by Christopher Columbus, who named it for the Church of Santa Maria de la Antigua in Sevilla, Spain. It was colonized by English settlers in 1632 and remained a British possession although it was raided by the French in 1666. The early colonizers were also attacked by Caribs, who were once one of the dominant peoples of the West Indies. At first tobacco was grown, but in the later 17th century sugar was found to be more profitable. The nearby island of Barbuda was colonized in 1678. The crown granted the island to the Codrington family in 1685. It was planned as a slave-breeding colony but never became one; the slaves who were imported came to live self-reliantly in their own community. The emancipation in 1834 of slaves, who had been employed on the profitable sugar estates, gave rise to difficulties in obtaining labour. An earthquake in 1843 and a hurricane in 1847 caused further economic problems. Barbuda reverted back to the crown in the late 19th century, and its administration came to be so closely related to that of Antigua that it eventually became a dependency of that island. The Leeward Islands colony, of which the islands were a part, was defederated in 1956, and in 1958 Antigua joined the West Indies Federation. When the federation was dissolved in 1962, Antigua persevered with discussions of alternative forms of federation. Provision was made in the West Indies Act of 1967 for Antigua to assume a status of association with the United Kingdom on February 27, 1967. As an associated state, Antigua was fully self-governing in all internal affairs, while the United Kingdom retained responsibility for external affairs and defense. By the 1970s Antigua had developed an independence movement, particularly under its prime minister George Walter, who wanted complete independence for the islands and opposed the British plan of independence within a federation of islands. Walter lost the 1976 legislative elections to Vere Bird, who favoured regional integration. In 1978 Antigua reversed its position and announced it wanted independence. The autonomy talks were complicated by the fact that Barbuda, long a dependency of Antigua, felt that it had been economically stifled by the larger island and wanted to secede. Finally, on November 1, 1981, Antigua and Barbuda achieved independence, with Vere Bird as the first prime minister. The state obtained United Nations and Commonwealth membership and joined the Organization of Eastern Caribbean States. Bird’s Antigua Labour Party (ALP) won again in 1984 and 1989 by overwhelming margins, giving the prime minister firm control of the islands’ government. Richard Tolson David Lawrence Niddrie Janet D. Momsen The postindependence political landscape of Antigua and Barbuda remained relatively stable, although the government was the subject of intermittent scandals and corruption allegations. The country also acquired a reputation as a somewhat lax tax haven. Bird retained office until his retirement in 1994, after which his son, Lester, served as prime minister from 1994 to 2004. He was succeeded by Baldwin Spencer of the United Progressive Party, who also spent a decade in office. In 2009 the economy suffered after one of the country’s largest investors, U.S. financier Robert Allen Stanford, was arrested and charged with fraud; in 2012 a Texas court found him guilty of having run a Ponzi scheme from his offshore bank on Antigua. In the June 2014 legislative elections the ALP regained power under Gaston Browne. Browne and the ALP then retained power in early elections held in March 2018. More … Score: https://www.britannica.com/place/Antigua-and-Barbuda    

2026/11/01

Anniversary of the Algerian Revolution of the Democratic People's Republic

Algeria, large, predominantly Muslim country of North Africa. From the Mediterranean coast, along which most of its people live, Algeria extends southward deep into the heart of the Sahara, a forbidding desert where Earth’s hottest surface temperatures have been recorded and which constitutes more than four-fifths of the country’s area. The Sahara and its extreme climate dominate the country. The contemporary Algerian novelist Assia Djebar has highlighted the environs, calling her country “a dream of sand.”History, language, customs, and an Islamic heritage make Algeria an integral part of the Maghreb and the larger Arab world, but the country also has a sizable Amazigh (Berber) population, with links to that cultural tradition. Once the breadbasket of the Roman Empire, the territory now comprising Algeria was ruled by various Arab-Amazigh dynasties from the 8th through the 16th century, when it became part of the Ottoman Empire. The decline of the Ottomans was followed by a brief period of independence that ended when France launched a war of conquest in 1830. By 1847 the French had largely suppressed Algerian resistance to the invasion and the following year made Algeria a département of France. French colonists modernized Algeria’s agricultural and commercial economy but lived apart from the Algerian majority, enjoying social and economic privileges extended to few non-Europeans. Ethnic resentment, fueled by revolutionary politics introduced by Algerians who had lived and studied in France, led to a widespread nationalist movement in the mid-20th century. A war of independence ensued (1954–62) that was so fierce that the revolutionary Frantz Fanon noted, Terror, counter-terror, violence, counter-violence: that is what observers bitterly record when they describe the circle of hate, which is so tenacious and so evident in Algeria. Negotiations ended the conflict and led to Algerian independence, and most Europeans left the country. Although the influence of the French language and culture in Algeria remained strong, since independence the country consistently has sought to regain its Arab and Islamic heritage. At the same time, the development of oil and natural gas and other mineral deposits in the Algerian interior brought new wealth to the country and prompted a modest rise in the standard of living. In the early 21st century Algeria’s economy was among the largest in Africa. The capital is Algiers, a crowded bustling seaside metropolis whose historic core, or medina, is ringed by tall skyscrapers and apartment blocks. Algeria’s second city is Oran, a port on the Mediterranean Sea near the border with Morocco. Less hectic than Algiers, Oran has emerged as an important centre of music, art, and education. Algeria is bounded to the east by Tunisia and Libya; to the south by Niger, Mali, and Mauritania; to the west by Morocco and Western Sahara (which has been virtually incorporated by the former); and to the north by the Mediterranean Sea. It is a vast country—the largest in Africa and the 10th largest in the world—that may be divided into two distinct geographic regions. The northernmost, generally known as the Tell, is subject to the moderating influences of the Mediterranean and consists largely of the Atlas Mountains, which separate the coastal plains from the second region in the south. This southern region, almost entirely desert, forms the majority of the country’s territory and is situated in the western portion of the Sahara, which stretches across North Africa. Relief The main structural relief features in Algeria were produced by the collision of the African and Eurasian tectonic plates along the Mediterranean margin, giving the country its two geographic regions. The Tell, home to most of the country’s population, contains two geologically young massifs, the Tell Atlas (Atlas Tellien) and the Saharan Atlas (Atlas Saharien), that run generally parallel from east to west and are separated by the High Plateau (Hauts Plateaux). The south, consisting of the Sahara, is a solid and ancient platform of basement rock, horizontal and uniform. This region is uninhabited desert with the exception of several oases, but it conceals rich mineral resources, most significantly petroleum and natural gas. The Tell In succession from north to south are intermittent coastal folded massifs and coastal plains. Along with the Tell Atlas, High Plateau, and Saharan Atlas, they form a sequence of five geographically variegated zones that roughly parallel the coast. The coastal ridges and massifs are indented with numerous bays and are often separated from each other by plains—such as the plains of Oran and Annaba—that extend inland. In the same way, the Tell Atlas is not continuous; in the west it forms two distinct ranges separated by interior plains. Thus, the Maghnia Plain separates the Tlemcen Mountains to the south from the Traras Mountains to the northwest. Similarly, the plains of Sidi Bel Abbès and Mascara are nestled between hill ranges to the north and south. The Dahra Massif forms a long range extending from the mouth of the Chelif River in the west to Mount Chenoua in the east; it is separated from the Ouarsenis Massif to the south by plains of the Chelif valley. The relief as a whole, therefore, does not constitute a barrier to communications in the western Tell. However, this is not the case in the central Tell, where the Blida Atlas merges with the Titteri Mountains and the mountainous block of Great Kabylia (Grande Kabylie) joins with the Bibans and Hodna mountains to make north-south communications more difficult. Only the valley of the Wadi Soummam permits communication with the port of Bejaïa. Farther east, from Bejaïa to Annaba, one mountain barrier follows another to separate the plains of Constantine from the sea. The lands south of the plains are dominated by the Hodna, Aurès, and Nemencha ranges. The plains themselves, which have long been used for growing cereal grains, have a distinct local topography and do not present the same features as the High Plateau, which extends westward from the Hodna Mountains into Morocco. The latter is broken by sabkhahs (lake beds encrusted with salt) and is much less favourable to agriculture because it receives less precipitation. To the south of the High Plateau and the plains of Constantine runs the Saharan Atlas, which is formed from a series of ranges oriented southwest to northeast. These decline in elevation from the west, where Mount Aïssa reaches 7,336 feet (2,236 metres) in the Ksour Mountains, to lower summits in the Amour and Oulad Naïl mountains. Higher summits are again found in the Aurès Mountains, where the highest peak in northern Algeria, Mount Chelia, which reaches 7,638 feet (2,328 metres), is located. Only the northern Tell ranges, lying along the tectonic plate boundary, experience much seismic activity. Severe earthquakes there have twice destroyed the town of Chlef (El-Asnam), in 1954 and 1980. An earthquake in 1989 caused severe damage in the zone between the Chenoua massif and Algiers, as did another in 2003 just east of Algiers. The Sahara The Algerian Sahara may be divided roughly into two depressions of different elevation, separated from one another by a central north-south rise called the Mʾzab (Mzab). Each zone is covered by a vast sheet of sand dunes called an erg. The Great Eastern Erg (Grand Erg Oriental) and the Great Western Erg (Grand Erg Occidental), which average 1,300 to 2,000 feet (400 to 600 metres) in height, decline in elevation northward from the foot of the Ahaggar (Hoggar) Mountains to below sea level in places south of the Aurès Mountains. The Ahaggar Mountains in the southern Sahara rise to majestic summits; the tallest, Mount Tahat, reaches an elevation of 9,573 feet (2,918 metres) and is the highest peak in the country. More … Score: https://www.britannica.com/place/Algeria    

2026/11/01

Visit Antigua & Barbuda

Antigua and Barbuda are two magical gems in the heart of the Caribbean. With some of the most stunning spots on earth filled with 80,000 new friends, Antigua and Barbuda makes for an epic paradisical adventure!.

2026/10/31