Independence Day of the Democratic Republic of the Congo

Democratic Republic of the Congo, country located in central Africa. Officially known as the Democratic Republic of the Congo, the country has a 25-mile (40-km) coastline on the Atlantic Ocean but is otherwise landlocked. It is the second largest country on the continent; only Algeria is larger. The capital, Kinshasa, is located on the Congo River about 320 miles (515 km) from its mouth. The largest city in central Africa, it serves as the country’s official administrative, economic, and cultural centre. The country is often referred to by its acronym, the DRC, or called Congo (Kinshasa), with the capital added parenthetically, to distinguish it from the other Congo republic, which is officially called the Republic of the Congo and is often referred to as Congo (Brazzaville). Congo gained independence from Belgium in 1960. From 1971 to 1997 the country was officially the Republic of Zaire, a change made by then ruler Gen. Mobutu Sese Seko to give the country what he thought was a more authentic African name. “Zaire” is a variation of a term meaning “great river” in local African languages; like the country’s current name, it refers to the Congo River, which drains a large basin that lies mostly in the republic. Unlike Zaire, however, the name Congo has origins in the colonial period, when Europeans identified the river with the kingdom of the Kongo people, who live near its mouth. Following the overthrow of Mobutu in 1997, the country’s name prior to 1971, the Democratic Republic of the Congo, was reinstated. Congo subsequently was plunged into a devastating civil war; the conflict officially ended in 2003, although fighting continued in the eastern part of the country. Congo is rich in natural resources. It boasts vast deposits of industrial diamonds, cobalt, and copper; one of the largest forest reserves in Africa; and about half of the hydroelectric potential of the continent. Land Congo is bounded to the north by the Central African Republic and South Sudan; to the east by Uganda, Rwanda, Burundi, and Tanzania; to the southeast by Zambia; and to the southwest by Angola. To the west are the country’s short Atlantic coastline, the Angolan exclave of Cabinda, and Congo (Brazzaville). Relief The country’s major topographical features include a large river basin, a major valley, high plateaus, three mountain ranges, and a low coastal plain. Most of the country is composed of the central Congo basin, a vast rolling plain with an average elevation of about 1,700 feet (520 metres) above sea level. The lowest point of 1,109 feet (338 metres) occurs at Lake Mai-Ndombe (formerly Lake Leopold II), and the highest point of 2,296 feet (700 metres) is reached in the hills of Mobayi-Mbongo and Zongo in the north. The basin may once have been an inland sea whose only vestiges are Lakes Tumba and Mai-Ndombe in the west-central region. The north-south Western Rift Valley, the western arm of the East African Rift System, forms the country’s eastern border and includes Lakes Albert, Edward, Kivu, Tanganyika, and Mweru. This part of the country is the highest and most rugged, with striking chains of mountains. The Mitumba Mountains stretch along the Western Rift Valley, rising to an elevation of 9,800 feet (2,990 metres). The snow-covered peaks of the Ruwenzori Range between Lakes Albert and Edward lie astride the Ugandan border and mark the country’s highest elevation of 16,763 feet (5,109 metres) at Margherita Peak. The volcanic Virunga Mountains stretch across the Western Rift Valley north of Lake Kivu. High plateaus border almost every other side of the central basin. In the north the Ubangi-Uele plateaus form the divide between the Nile and Congo river basins. Rising to between 3,000 and 4,000 feet (915 and 1,220 metres), these plateaus also separate the central basin from the vast plains of the Lake Chad system. In the south the plateaus begin at the lower terraces of the Lulua and Lunda river valleys and rise gradually toward the east. In the southeast the ridges of the plateaus of Katanga (Shaba) province tower over the region; they include Kundelungu at 5,250 feet (1,600 metres), Mitumba at 4,920 feet (1,500 metres), and Hakansson at 3,610 feet (1,100 metres). The Katanga plateaus reach as far north as the Lukuga River and contain the Manika Plateau, the Kibara and the Bia mountains, and the high plains of Marungu. The northern escarpment of the Angola Plateau rises in the southwest, while in the far west a coastal plateau zone includes the hill country of Mayumbe and the Cristal Mountains. A narrow coastal plain lies between the Cristal Mountains and the Atlantic Ocean. Drainage and soils The Congo River, including its 1,336,000-square-mile (3,460,000-square-km) basin, is the country’s main drainage system. The river rises in the high Katanga plateaus and flows north and then south in a great arc, crossing the Equator twice. The lower river flows southwestward to empty into the Atlantic Ocean below Matadi. Along its course, the Congo passes through alluvial lands and swamps and is fed by the waters of many lakes and tributaries. The most important lakes are Mai-Ndombe and Tumba; the major tributaries are the Lomami, Aruwimi, and Ubangi rivers and those of the great Kasai River system. In addition, the Lukuga River links the basin to the Western Rift Valley. Soils are of two types: those of the equatorial areas and those of the drier savanna (grassland) regions. Equatorial soils occur in the warm, humid lowlands of the central basin, which receive abundant precipitation throughout the year and are covered mainly with thick forests. This soil is almost fixed in place because of the lack of erosion in the forests. In swampy areas the very thick soil is constantly nourished by humus, the organic material resulting from the decomposition of plant or animal matter. Savanna soils are threatened by erosion, but the river valleys contain rich and fertile alluvial soils. The highlands of the Great Lakes region in eastern Congo are partly covered with rich soil derived from volcanic lava. This is the country’s most productive agricultural area. More … Score:https://www.britannica.com/place/Democratic-Republic-of-the Congo/Settlement-patterns

2025/06/30

Homepage Office National du Tourisme Djibouti

L’office National du Tourisme de Djibouti (ONTD) est l’organe en charge de l’organisation, l’animation et le contrôle du secteur touristique en République de Djibouti en vue du développement d’un tourisme durable.

2025/06/29

Madagascar Treasure Island

Île de passion, Madagascar vous accueille pour vos voyages découvertes. Laissez-vous guider par notre guide de voyage à Madagascar.

2025/06/28

Independence day of Republic of Djibouti

Djibouti, small strategically located country on the northeast coast of the Horn of Africa. It is situated on the Bab el Mandeb Strait, which lies to the east and separates the Red Sea from the Gulf of Aden. Formerly known as French Somaliland (1896–1967) and the French Territory of the Afars and Issas (1967–77), the country took Djibouti as its name when it gained independence from France on June 27, 1977. Djibouti’s capital, Djibouti city, is built on coral reefs that jut into the southern entrance of the gulf; other major towns are Obock, Tadjoura, Ali Sabieh, Arta, and Dikhil. The country’s Lilliputian aspect belies its regional and geopolitical importance. The capital is the site of a modern deepwater port that serves Indian Ocean and Red Sea traffic and hosts a French naval base. Djibouti city is also the railhead for the only line serving Addis Ababa, the capital of neighbouring Ethiopia. Land - Relief Djibouti is bounded by Eritrea to the north, Ethiopia to the west and southwest, and Somalia to the south. The Gulf of Tadjoura, which opens into the Gulf of Aden, bifurcates the eastern half of the country and supplies much of its 230 miles (370 km) of coastline. The landscape of Djibouti is varied and extreme, ranging from rugged mountains in the north to a series of low desert plains separated by parallel plateaus in the west and south. Its highest peak is Mount Moussa at 6,654 feet (2,028 metres). The lowest point, which is also the lowest in Africa, is the saline Lake Assal, 509 feet (155 metres) below sea level. The country is internationally renowned as a geologic treasure trove. Located at a triple juncture of the Red Sea, Gulf of Aden, and East African rift systems, the country hosts significant seismic and geothermal activity. Slight tremors are frequent, and much of the terrain is littered with basalt from past volcanic activity. In November 1978 the eruption of the Ardoukoba volcano, complete with spectacular lava flows, attracted the attention of volcanologists worldwide. Of particular interest was the tremendous seismic activity that accompanied the eruption and led to the widening by more than a metre of the plates between Africa and the Arabian Peninsula. Drainage Besides Lake Assal, the other major inland body of water is Lake Abbe, located on Djibouti’s southwestern border with Ethiopia. The country is completely devoid of any permanent above-ground rivers, although some subterranean rivers exist. Climate The often torrid climate varies between two major seasons. The cool season lasts from October to April and typifies a Mediterranean-style climate in which temperatures range from the low 70s to the mid-80s F (low 20s to low 30s C) with low humidity. The hot season lasts from May to September. Temperatures increase as the hot khamsin wind blows off the inland desert, and they range from an average low in the mid-80s F (low 30s C) to a stifling high in the low 110s F (mid-40s C). This time of year is also noted for days in which humidity is at its highest. Among the coolest areas in the country is the Day Forest, which is located at a high elevation; temperatures in the low to mid-50s F (low to mid-10s C) have been recorded. The average annual precipitation is limited and is usually spread over 26 days. Different regions of the country receive varying amounts of precipitation: the coastal regions receive 5 inches (130 mm) of rainfall per annum, while the northern and mountainous portions of the country receive about 15 inches (380 mm). The rainy season lasts between January and March, with the majority of precipitation falling in quick, short bursts. One outcome of this erratic rainfall pattern is periodic flash floods that devastate those areas located at sea level. Plant and animal life Despite Djibouti’s relatively harsh landscape, abundances of flora and fauna abound. In the northern portion of the country, one finds the ancient Day Forest National Park and a variety of tree species, such as jujube, fig, olive, juniper, and momosa. To the south and southwest of the Gulf of Tadjoura, the vegetation is similar to that found in other arid regions of Africa, inclusive of acacia and doum palm trees. Among the types of fauna are a wide variety of bird species, numerous types of antelopes and gazelles, and more limited numbers of carnivores (such as cheetahs) and scavengers (such as hyenas), as well as monkeys, squirrels, and warthogs. Perhaps most spectacular is the extremely rich diversity of marine life found along Djibouti’s coastline and coral reefs, a factor that has made the country a special point of interest for international scuba-diving associations. People - Ethnic groups On the basis of linguistic criteria, the two largest ethnic groups are the Somali and the Afar. Both groups speak related, but not mutually intelligible, eastern Cushitic languages. The Afar (Denakil, or Danakil) speak a language that forms a dialect continuum with Saho. Saho-Afar is usually classified as an Eastern Cushitic language of the Afro-Asiatic language phylum. The Afar live in the sparsely populated areas to the west and north of the Gulf of Tadjoura. This region includes parts of several former as well as extant Afar sultanates. The sultans’ roles are now largely ceremonial, and the social divisions within the traditional Afar hierarchy are of diminished importance. The Afar are also found across the border in neighbouring Ethiopia. Their population distribution in the two countries forms a pattern that is somewhat elongated and triangular in shape and is often referred to as the “Afar triangle.” The Somali, who also speak an Eastern Cushitic language, are concentrated in the capital and the southeastern quarter of the country. Their social identity is determined by clan-family membership. More than half the Somali belong to the Issa, whose numbers exceed those of the Afar; the remaining Somali are predominately members of the Gadaboursi and Isaaq clans that migrated from northern Somalia during the 20th century to work on the construction of the Djibouti–Addis Ababa railway and Djibouti city’s port expansion. Djibouti city is home to a long-established community of Yemeni Arabs and houses a sizable contingent of French technical advisers and military personnel. In recent decades these groups have been joined by small but significant numbers of ethnic Ethiopians as well as Greek and Italian expatriates. Language of Djibouti The republic recognizes two official languages: French and Arabic. However, Somali is the most widely spoken language, although it is rarely written and is not taught in the schools. The use of Afar is mostly restricted to Afar areas. Many Djiboutians are multilingual. Fluency in French is particularly important for those with political aspirations. French is the means of instruction in primary and secondary schools, although Arabic is also taught as the first language at both these levels. Religion More than nine-tenths of the population is Muslim; nearly all adhere to the Sunni branch of Islam. Some Christian religions are represented in Djibouti, including Eastern Orthodoxy and Roman Catholicism. More: Score: https://www.britannica.com/place/Djibouti

2025/06/27

I feel Slovenia: Uradni slovenski turistični portal

Visit the gems of Slovenian culture, gastronomy and nature. Discover the traditions and customs of the Slovenian people, interesting stories and legends, and ...

2025/06/27

Travel Discover Mozambique

The climate in Mozambique, influenced by the monsoons of the Indian Ocean and the warm current of the Mozambique Channel, is generally tropical and humid, with ...

2025/06/27

Official website of the Croatian National Tourist Board

You will find all relevant information related to your next summer (or winter) vacation in Croatia right here. Welcome!

2025/06/27

2025/06/26

Independence Day of Republic of Madagascar

Madagascar, island country lying off the southeastern coast of Africa. Madagascar is the fourth largest island in the world, after Greenland, New Guinea, and Borneo. Although located some 250 miles (400 km) from the African continent, Madagascar’s population is primarily related not to African peoples but rather to those of Indonesia, more than 3,000 miles (4,800 km) to the east. The Malagasy peoples, moreover, do not consider themselves to be Africans, but, because of the continuing bond with France that resulted from former colonial rule, the island developed political, economic, and cultural links with the French-speaking countries of western Africa. The animal life and vegetation of the island are equally anomalous, differing greatly from that of nearby Africa and being in many respects unique. Although the coastlands have been known to Europeans for more than 400 years and to Arabs for much longer, recent historical development has been more intense and concentrated in the central plateau, which contains the capital city of Antananarivo (formerly Tananarive). Land Madagascar is located in the southwestern Indian Ocean and is separated from the African coast by the 250-mile- (400-km-) wide Mozambique Channel. Relief Madagascar consists of three parallel longitudinal zones—the central plateau, the coastal strip in the east, and the zone of low plateaus and plains in the west. Situated between 2,500 and 4,500 feet (800 and 1,400 metres) above sea level, the plateau has been uplifted and worn down several times and is tilted to the west. Three massifs are more than 8,500 feet (2,600 metres) high. The Tsaratanana region in the north is separated from the rest of the plateau by the Tsaratanana Massif, whose summit, Maromokotro, reaches 9,436 feet (2,876 metres) and is the highest point on the island. Ankaratra Massif in the centre is an enormous volcanic mass whose summit, Tsiafajavona, is 8,671 feet (2,643 metres) high. Ankaratra is a major watershed divide separating three main river basins. Farther south, Andringitra is a vast granite massif north of Tôlan̈aro (Faradofay); it rises to 8,720 feet (2,658 metres) at Boby Peak. The plateau slopes with some regularity toward the extreme southern plain, but its boundaries to the east and west are more abrupt. To the east it descends in a sharp fault, by vertical steps of 1,000 to 2,000 feet (300 to 600 metres). This cliff, which is called the Great Cliff or the Cliff of Angavo, is often impassable and is itself bordered by the Betsimisaraka Escarpment, a second and lower cliff to the east, which overhangs the coastal plain. Behind the scarp face are the remains of ancient lakes, including one called Alaotra. To the south the two steep gradients meet and form the Mahafaly and the Androy plateaus, which overhang the sea in precipitous cliffs. Toward the west the descent is made in a series of steps. However, in places the central plateau is bordered by an impassable escarpment, such as the Cliff of Bongolava in the west-central part of the island. To the extreme north the plateau is bordered by the low belt of the Ambohitra Mountains, which include a series of volcanic craters. The coastal strip has an average width of about 30 miles (50 km). It is a narrow alluvial plain that terminates in a low coastline bordered with lagoons linked together by the Pangalanes (Ampangalana) Canal, which is more than 370 miles (600 km) long. To the south of Farafangana the coast becomes rocky, and in the southeast there occur many little bays. To the northeast is the deep Bay of Antongil (Antongila). The western zone is between 60 and 125 miles (100 and 200 km) wide. Its sedimentary layers slope toward the Mozambique Channel and produce a succession of hills. The inland (eastern) side of these steep hills dominates the hollows formed in the soft sediments of the interior, while the other side descends to the sea in rocky slopes. The coastline is straight, bordered by small dunes and fringed with mangroves. The currents in the Mozambique Channel have favoured the offshore deposit of alluvium and the growth of river deltas. On the northwestern coast there are a number of estuaries and bays. This coast is bordered by coral reefs and volcanic islands, such as Nosy Be (Nossi-Bé), which protects Ampasindava Bay. Drainage The steep eastern face of the plateau is drained by numerous short, torrential rivers, such as the Mandrare, the Mananara, the Faraony, the Ivondro, and the Maningory, which discharge either into the coastal lagoons or directly into the sea over waterfalls and rapids. The more gently sloping western side of the plateau is crossed by longer and larger rivers, including the Onilahy, the Mangoky, the Tsiribihina, and the Betsiboka, which bring huge deposits of fertile alluvium down into the vast plains and many-channeled estuaries; the river mouths, while not completely blocked by this sediment, are studded with numerous sandbanks. There are many lakes of volcanic origin on the island, such as Lake Itasy. Alaotra is the last surviving lake of the eastern slope. Lake Tsimanampetsotsa, near the coast south of Toliara (formerly Tuléar), is a large body of saline water that has no outlet. Soils The central plateau and the eastern coast are mainly composed of gneiss, granite, quartz, and other crystalline rock formations. The gneiss decomposes into red murrum, laterite, and deeper and more fertile red earths, giving Madagascar its colloquial name the Great Red Island. Fertile alluvial soils in the valleys support intensive cultivation. There also are scattered volcanic intrusions that produce fertile but easily erodible soils. Lake Alaotra is a large sedimentary pocket in the central plateau containing some of the island’s most productive farmland. The western third of the island consists entirely of deposits of sedimentary rock, giving rise to soils of medium to low fertility. Climate of Madagascar The hot, wet season extends from November to April and the cooler, drier season from May to October. The climate is governed by the combined effects of the moisture-bearing southeast trade and northwest monsoon winds as they blow across the central plateau. The trade winds, which blow throughout the year, are strongest from May to October. The east coast is to the windward and has a high annual rate of precipitation, reaching nearly 150 inches (3,800 mm) at Maroantsetra on the Bay of Antongil. As the winds cross the plateau, they lose much of their humidity, causing only drizzle and mists on the plateau itself and leaving the west in a dry rain shadow. The southwest in particular is almost desert, with the dryness aggravated by a cold offshore current. The monsoon, bringing rain to the northwest coast of Madagascar and the plateau, is most noticeable during the hot, humid season. The wind blows obliquely onto the west coast, which receives a moderate amount of precipitation annually; the southwest, which is protected, remains arid. Annual precipitation drops from about 80 inches (about 2,000 mm) on the northwestern island of Nosy Be to about 40 inches (1,000 mm) at Maintirano on the west coast to about 14 inches (360 mm) at Toliara in the southwest. The plateau receives moderate levels of precipitation, with about 50 inches (1,200 mm) falling annually at both Antananarivo and Fianarantsoa, which lies about 200 miles (320 km) farther south. July is the coolest month, with mean monthly temperatures around the island ranging from the low 50s F (low 10s C) to the high 70s F (mid-20s C), and December is the hottest month, with temperatures between the low 60s and mid-80s F (mid 10s and high 20s C). Temperatures generally decrease with elevation, being highest on the northwest coast and lowest on the plateau. Tropical cyclones are an important climatic feature. They form far out over the Indian Ocean, especially from December to March, and approach the eastern coast, bringing torrential rains and destructive floods. Plant and animal life Much of the island was once covered with evergreen and deciduous forest, but little now remains except on the eastern escarpment and in scattered pockets in the west. The plateau is particularly denuded and suffers seriously from erosion. The forest has been cut in order to clear rice fields, to obtain fuel and building materials, and to export valuable timber such as ebony, rosewood, and sandalwood. About seven-eighths of the island is covered with prairie grasses and bamboo or small thin trees. There also are screw pines, palms, and reeds on the coasts. In the arid south of the island grow thorn trees, giant cacti, dwarf baobab trees, pachypodium succulents, and other xerophytes (drought-resistant plants) that are peculiar to the island. Because of the island’s isolation, many zoologically primitive primates have survived and evolved into unique forms. About 40 species of lemurs are indigenous to Madagascar. Several unique hedgehoglike insectivores, such as the tenrec, have evolved there, and there are also many kinds of chameleons of varying size. Birds are numerous and include guinea fowl, partridges, pigeons, herons, ibis, flamingos, egrets, cuckoos, Asian robins, and several kinds of birds of prey. There are about 800 species of butterflies, many moths, and a variety of spiders. The only large or dangerous animals are the crocodiles, which occupy the rivers. The snakes, including the do, which is 10 to 13 feet (3 to 4 metres) in length, are harmless. Inland waters contain tilapia (an edible perchlike fish), rainbow trout, and black bass. Marine fish and crustaceans abound on the coasts and in the lagoons, estuaries, and even in some upland streams. They include groupers, giltheads, tuna, sharks, sardines, whitings, crayfish, crabs, shrimps, mussels, and oysters. The coelacanth, referred to as a living fossil and once thought extinct for millions of years, inhabits offshore waters. More … Score: https://www.britannica.com/place/Madagascar

2025/06/26