Republic of Yemen Reunification Day

Yemen, country situated at the southwestern corner of the Arabian Peninsula. It is mostly mountainous and generally arid, though there are broad patches with sufficient precipitation to make agriculture successful. The people speak various dialects of Arabic and are mostly Muslims (see Islam). The history, culture, economy, and population of Yemen have all been influenced by the country’s strategic location at the southern entrance of the Red Sea—a crossroads of both ancient and modern trade and communications routes. In the ancient world, the states that occupied the area known today as Yemen controlled the supply of such important commodities as frankincense and myrrh and dominated the trade in many other valuable items, such as the spices and aromatics of Asia. Because of its fertility as well as its commercial prosperity, Yemen was the location of a number of ancient kingdoms; for that same reason, it was known to the ancient Romans as Arabia Felix (Latin: “Fortunate Arabia”) to distinguish it from the vast forbidding reaches of Arabia Deserta (“Desert Arabia”). Later, Yemen was the place where coffee (Arabic: qahwah) was first cultivated commercially, and, before the introduction of coffee plants to other parts of the world, it was long the sole source of that precious bean. The present Republic of Yemen came into being in May 1990, when the Yemen Arab Republic (North Yemen) merged with the People’s Democratic Republic of Yemen (South Yemen). By stipulation of the unification agreement, Sanaa, formerly the capital of North Yemen, functions as the political capital of the country, while Aden, formerly the capital of South Yemen, functions as the economic centre. The two components of Yemen underwent strikingly different histories: whereas North Yemen never experienced any period of colonial administration at the hands of a European power, South Yemen was a part of the British Empire from 1839 to 1967. The contemporary borders are largely a product of the foreign policy goals and actions of Britain, the Ottoman Empire, and Saudi Arabia. Postunification Yemen has been burdened by chronic corruption and economic hardship. Divisions based on religion, tribalism, and geography continue to play an important role in Yemeni politics, sometimes leading to violence. Even during the age of colonial hegemony, Yemen remained for the most part one of the most secluded regions of the world. Much the same can be said today; few outsiders travel Yemen’s rugged hinterland, many parts of which have been little influenced by central government authority. It is perhaps this splendid isolation that has captivated the imagination of many from abroad. For all its remoteness, Yemen is likewise a country of great physical beauty, photogenic and picturesque, with a life and verdancy in the highlands unlike that found elsewhere on the Arabian Peninsula. Walter B. Harris, a journalist and traveler, visited Yemen in 1892. One of the first Westerners to see many parts of the country, he recounted his impressions in the book A Journey Through the Yemen, in which he says: Nothing can be imagined more beautiful than the scenery of the mountains of the Yemen. Torn into all manner of fantastic peaks, the rocky crags add a wildness to a view that otherwise possesses the most peaceful charms. Rich green valleys, well timbered in places, and threaded by silvery streams of dancing water; sloping fields, gay with crops and wildflowers; the terraced or jungle-covered slopes,—all are so luxuriant, so verdant, that one’s ideas as to the nature of Arabia are entirely upset. Well known as is, and always has been, the fertility of this region, its extent is almost startling, and it can little be wondered at that Alexander the Great intended, after his conquest of India, to take up his abode in the Yemen. … Land of Yemen Most of Yemen’s northern frontier with Saudi Arabia traverses the great desert of the peninsula, the Rubʿ al-Khali (“Empty Quarter”), and until 2000 remained undemarcated, as did the eastern frontier with Oman until 1992. Yemen is bounded to the south by the Gulf of Aden and the Arabian Sea and to the west by the Red Sea. Yemen’s territory includes a number of islands as well, including the Kamarān group, located in the Red Sea near Al-Ḥudaydah; the Ḥanīsh Islands, in the southern Red Sea; Perim (Barīm) Island, in the Bab el-Mandeb Strait, which separates the Arabian Peninsula from Africa; Socotra (Suquṭrā), Yemen’s most important and largest island, located in the Arabian Sea nearly 620 miles (1,000 km) east of Aden; and the Brothers (Al-Ikhwān), a group of small islets near Socotra. Relief and drainage Yemen may be divided into five major regions: a coastal plain running north-south known as the Tihāmah (an extension of the Tihāmat ʿAsīr), the western highlands, the central mountains (the Yemen Highlands), the eastern highlands, and finally the eastern and northeastern desert regions. The coastal plain ranges in width from 5 miles (8 km) to as much as 40 miles (65 km). Low mountains rising from 1,000 to 3,500 feet (300 to 1,100 metres) lie between the low hills of the plain and the great central massif, which has many peaks in excess of 10,000 feet (3,000 metres); the highest is Mount Al-Nabī Shuʿayb, which rises to 12,336 feet (3,760 metres). Toward the east-northeast, the mountains subside rather rapidly into the eastern highlands (2,500–3,500 feet [750–1,100 metres]), which drop off to the sandy hills of the Rubʿ al-Khali. Yemen is an arid country, and there are no permanent watercourses. The regular rainfall that occurs in some areas drains, in the northern part, westward toward the Red Sea through five major watercourses (wadis) and, in the southern part, southward into the Gulf of Aden and the Arabian Sea through three major watercourses. The largest of the latter is the Wadi Ḥaḍramawt (Hadhramaut Valley), which has been renowned since antiquity for its frankincense trees and which historically has been the locus of a number of sophisticated city-states. Together with their tributaries and lesser neighbours, these intermittently flowing channels slice the highlands and central massif into a large number of plateaus and ridges. In many places there is evidence of volcanic activity from as recently as a few hundred years ago; the existence of hot springs and fumaroles (volcanic vents) attests to continued subterranean activity. Moreover, the country sits astride one of the most active fault lines in the Red Sea region (Great Rift Basin) and has experienced several severe earthquakes in modern times, including one that shook the Dhamar area in December 1982, killing about 3,000 people and largely destroying several villages and hundreds of smaller settlements. Soils throughout the country vary from sandy to loamy, and most are low in organic matter, thus limiting agricultural options. In some areas, however, elaborate agricultural terraces cover the mountains from base to peak. The high agricultural productivity of this system is largely attributable to the soil that has been collected and enriched with compost over a period of centuries. In the modern period, neglect and civil conflict have taken their toll on the earthworks, which are particularly vulnerable to erosion. Still, the terraces are largely intact and are a breathtaking feature of mountainous Yemen. More … Score: https://www.britannica.com/place/Yemen

2026/05/22

Cameroon Tourism Information – Destination Cameroon

In Africa, Cameroon represents a country of its own, enriched with a cultural diversity. This exceptional heritage offers a mosaic of cultures ...

2026/05/22

The beautiful Yemen

In ancient Yemen, named by the ancient Romans "Arabia Felix" ;Happy Arabia, there were 6 principal kingdoms: the Sabaean, Awsanian, Minaean, Qatabanian, Hadhramawtian, Himyarite. Sabaean was the oldest and one of the most powerful. Saba in Hebrew is "Sheba". Thus the fabled Queen of Sheba came from Sabaean kingdom.

2026/05/21

Anniversary of the Constitution the Republic of Cameroon

Cameroon, country lying at the junction of western and central Africa. Its ethnically diverse population is among the most urban in western Africa. The capital is Yaoundé, located in the south-central part of the country. The country’s name is derived from Rio dos Camarões (“River of Prawns”)—the name given to the Wouri River estuary by Portuguese explorers of the 15th and 16th centuries. Camarões was also used to designate the river’s neighbouring mountains. Until the late 19th century, English usage confined the term “the Cameroons” to the mountains, while the estuary was called the Cameroons River or, locally, the Bay. In 1884 the Germans extended the word Kamerun to their entire protectorate, which largely corresponded to the present state. Land Cameroon is triangular in shape and is bordered by Nigeria to the northwest, Chad to the northeast, the Central African Republic to the east, the Republic of the Congo to the southeast, Gabon and Equatorial Guinea to the south, and the Atlantic Ocean to the southwest. Relief Cameroon can be divided into northern, central, southern, and western geographic regions. North of the Benue (Bénoué) River, the savanna plain that occupies the country’s centre declines in elevation as it approaches the Lake Chad basin. The region contains scattered inselbergs, mounds of erosion-resistant rock that rise above the plains. The Gotel Mountains of the Adamawa Plateau trend from south to north, culminating in the Mandara Mountains of the northwest. The central region extends east from the western highlands and from the Sanaga River north to the Benue River. The land rises progressively to the north and includes the Adamawa Plateau, with elevations between 2,450 and 4,450 feet (750 and 1,350 metres). The southern region extends from the Sanaga River to the southern border and from the coast eastward to the Central African Republic and the Republic of the Congo. It consists of coastal plains that are about 25 miles (40 km) wide and a densely forested plateau with an average elevation of a little more than 2,000 feet (600 metres). The western region extends north and west from the Sanaga River and continues north along the Nigerian border as far as the Benue River. The relief is mostly mountainous, the result of a volcanic rift that extends northward from the island of Bioko. Near the coast, the active volcanic Mount Cameroon rises to the highest elevation in western Africa—13,435 feet (4,095 metres). Drainage The rivers of Cameroon form four large drainage systems. In the south the Sanaga, Wouri, Nyong, and Ntem rivers drain into the Atlantic Ocean. The Benue River and its tributary, the Kébi, flow into the Niger River basin of Nigeria. The Logone and Chari rivers—which form part of the eastern border with Chad—drain into Lake Chad, whereas the Dja River joins the Sangha River and flows into the Congo River basin. Soils The soils of Cameroon may be roughly divided into three groups. The first soil group, developed primarily in the higher-precipitation south and south-centre, is composed of soils with strong physical makeup but weaker chemical properties. With good depth, high permeability, and stable structure, these soils are less prone to erosion. They rely on the input of organic matter to replenish nutrient levels; interruption of this cycle leads to swift depletion and decrease in fertility. The second soil group is present mainly in the lower-precipitation northern regions. Weathering by water is not as significant a problem for that soil group as mechanical weathering. A lower iron content dictates the soils’ colouring, which ranges from gray to brown. Though more fertile than their counterparts in the south, these soils are susceptible to nutrient imbalances that can impede productivity. The third soil group is a general gathering of a number of young soils, including andosols, which are developed from volcanic ash and other matter, and the dark, clay-laden vertisols. Incidence of these soils varies by region. More … Score: https://www.britannica.com/place/Cameroon

2026/05/20

WELCOME TO CAMEROON : CAN 2022 - MAKULI MA NLIMA

Notre Belle Afrique est le berceau et l'avenir de la race humaine! Ce n'est pas un débat. Montrons nous dignes durant cet évènement majeur: pas de dépravation des mœurs, pas de musique immorales pour exprimer notre joie. Honorons Dieu par des louanges...

2026/05/19

Visit Norway | Official travel guide to Norway

Plan your holiday in Norway with free guides and videos. Learn about fjords, northern lights, midnight sun, where to stay, walking, fishing and more.

2026/05/19

Anniversary of the Constitution The Kingdom of Norway

Norway, country of northern Europe that occupies the western half of the Scandinavian peninsula. Nearly half of the inhabitants of the country live in the far south, in the region around Oslo, the capital. About two-thirds of Norway is mountainous, and off its much-indented coastline lie, carved by deep glacial fjords, some 50,000 islands.             Indo-European peoples settled Norway’s coast in antiquity, establishing a permanent settlement near the present capital of Oslo some 6,000 years ago. The interior was more sparsely settled, owing to extremes of climate and difficult terrain, and even today the country’s population is concentrated in coastal cities such as Bergen and Trondheim. Dependent on fishing and farming, early Norwegians developed a seafaring tradition that would reach its apex in the Viking era, when Norse warriors regularly raided the British Isles, the coasts of western Europe, and even the interior of Russia; the Vikings also established colonies in Iceland and Greenland and explored the coast of North America (which Leif Eriksson called Vinland) more than a thousand years ago. This great tradition of exploration by such explorers as Leif Erikkson and his father, Erik the Red, continued into modern times, exemplified by such men as Fridtjof Nansen, Roald Amundsen, and Thor Heyerdahl. Weakened by plague and economic deterioration in the late Middle Ages and dominated by neighbouring Denmark and Sweden, Norwegians turned to trading in fish and lumber, and modern Norway, which gained its independence in 1905, emerged as a major maritime transporter of the world’s goods as well as a world leader in specialized shipbuilding. In the 1970s the exploitation of offshore oil and natural gas became the major maritime industry, with Norway emerging in the 1990s as one of the world’s leading petroleum exporters. Lying on the northern outskirts of the European continent and thus avoiding the characteristics of a geographic crossroads, Norway (the “northern way”) has maintained a great homogeneity among its peoples and their way of life. Small enclaves of immigrants, mostly from southeastern Europe and South Asia, established themselves in the Oslo region in the late 20th century, but the overwhelming majority of the country’s inhabitants are ethnically Nordic. The northern part of the country, particularly the rugged Finnmark Plateau, is home to the Sami (also called Lapps or Laplanders), a Uralic people whose origins are obscure. Life expectancy rates in Norway are among the highest in the world. The main political division reflects differing views on the importance of free-market forces; but the socialists long ago stopped insisting on nationalization of the country’s industry, and the nonsocialists have accepted extensive governmental control of the country’s economy. Such evident national consensus—along with abundant waterpower, offshore oil, and peaceful labour relations—was a major factor in the rapid growth of Norway as an industrial nation during the 20th century and in the creation of one of the highest standards of living in the world, reinforced by a comprehensive social welfare system. Norway’s austere natural beauty has attracted visitors from all over the world. The country has also produced many important artists, among them composer Edvard Grieg, painter Edvard Munch, novelists Knut Hamsun and Sigrid Undset, and playwright Henrik Ibsen. Of his country and its ruminative people, Ibsen observed, “The magnificent, but severe, natural environment surrounding people up there in the north, the lonely, secluded life—the farms are miles apart—forces them to…become introspective and serious.…At home every other person is a philosopher!” Land With the Barents Sea to the north, the Norwegian Sea and the North Sea to the west, and Skagerrak (Skager Strait) to the south, Norway has land borders only to the east—with Sweden, Finland, and Russia. Norway occupies part of northern Europe’s Fennoscandian Shield. The extremely hard bedrock, which consists mostly of granite and other heat- and pressure-formed materials, ranges from one to two billion years in age. Relief Glaciation and other forces wore down the surface and created thick sandstone, conglomerate, and limestone deposits known as sparagmite. Numerous extensive areas called peneplains, whose relief has been largely eroded away, also were formed. Remains of these include the Hardanger Plateau—3,000 feet (900 metres) above sea level—Europe’s largest mountain plateau, covering about 4,600 square miles (11,900 square km) in southern Norway; and the Finnmark Plateau (1,000 feet [300 metres] above sea level), occupying most of Finnmark, the northernmost and largest county of Norway. From the Cambrian through the Silurian geologic period (i.e., from about 540 to 415 million years ago), most of the area was below sea level and acquired a layer of limestone, shale, slate, and conglomerate from 330 to 525 feet (100 to 160 metres) thick. Folding processes in the Earth then gave rise to a mountain system that is a continuation of the Caledonian orogenic belt. Norway has an average elevation of 1,600 feet (500 metres), compared with 1,000 feet (300 metres) for Europe as a whole. Rivers running westward acquired tremendous erosive power. Following fracture lines marking weaknesses in the Earth’s crust, they dug out gorges and canyons that knifed deep into the jagged coast. To the east the land sloped more gently, and broader valleys were formed. During repeated periods of glaciation in the Great Ice Age of the Quaternary Period (i.e., about the last 2.6 million years), the scouring action of glaciers tonguing down the V-shaped valleys that were then part of the landscape created the magnificent U-shaped drowned fjords that now grace the western coast of Norway. Enormous masses of soil, gravel, and stone were also carried by glacial action as far south as present-day Denmark and northern Germany. The bedrock, exposed in about 40 percent of the area, was scoured and polished by the movements of these materials. There are four traditional regions of Norway, three in the south and one in the Arctic north. The three main regions of the south are defined by wide mountain barriers. From the southernmost point a swelling complex of ranges, collectively called Lang Mountains, runs northward to divide eastern Norway, or Østlandet, from western Norway, or Vestlandet. The narrow coastal zone of Vestlandet has many islands, and steep-walled, narrow fjords cut deep into the interior mountain region. The major exception is the wide Jæren Plain, south of Stavanger. An eastward sweep of the mountains separates northern Østlandet from the Trondheim region, or Trøndelag. Northern Norway, or Nord-Norge, begins almost exactly at the midpoint of the country. Most of the region is above the Arctic Circle, and much of it is filled with mountains with jagged peaks and ridges, even on the many islands. More … Score: https://www.britannica.com/place/Norway

2026/05/17

Visit Paraguay

Paraguay fue descubierto en el año 1524 por el adelantado español, Alejo García, formando la “Provincia Gigante de las Indias”. Entre el descubrimiento y ...

2026/05/17

Norway Promotional Video - Powered by Nature

Norway Promotional Video - Powered by Nature

2026/05/16