Myanmar Islands, Nyaung Oo Phee, Cock Burn and Pearl Island

Myanmar Islands 2018, เกาะนาวโอพี เกาะค๊อกเบิร์น เกาะมุก

2025/01/03

The Official Travel Guide to Haiti · Visit Haiti

Haiti's official travel and tourist information web site. Everything about vacation in Haiti. Find inspiration and guides for your next trip to Haiti.

2025/01/03

Sudan Visit Online - All you need to visit Sudan

View Culture, View Experiences to Sudan, View Regions. Tourist Business, Trip Help. Travel..

2025/01/03

Slovakia.travel

Visit Slovakia.

2025/01/03

Cuba Travel | Tourism Portal

Cuba Travel has the best tourist guide for your trips to Cuba. Find tourist destinations, attractions, facts and all the right info for your Cuban vacation.

2025/01/03

Malaysia National Day

Malaysia, country of Southeast Asia, lying just north of the Equator, that is composed of two noncontiguous regions: Peninsular Malaysia (Semenanjung Malaysia), also called West Malaysia (Malaysia Barat), which is on the Malay Peninsula, and East Malaysia (Malaysia Timur), which is on the island of Borneo. The Malaysian capital, Kuala Lumpur, lies in the western part of the peninsula, about 25 miles (40 km) from the coast; the administrative centre, Putrajaya, is located about 16 miles (25 km) south of the capital. Malaysia, a member of the Commonwealth, represents the political marriage of territories that were formerly under British rule. When it was established on September 16, 1963, Malaysia comprised the territories of Malaya (now Peninsular Malaysia), the island of Singapore, and the colonies of Sarawak and Sabah in northern Borneo. In August 1965 Singapore seceded from the federation and became an independent republic. Land Peninsular Malaysia occupies most of the southern segment of the Malay Peninsula. To the north it is bordered by Thailand, with which it shares a land boundary of some 300 miles (480 km). To the south, at the tip of the peninsula, is the island republic of Singapore, with which Malaysia is connected by a causeway and also by a separate bridge. To the southwest, across the Strait of Malacca, is the island of Sumatra in Indonesia. East Malaysia consists of the country’s two largest states, Sarawak and Sabah, and is separated from Peninsular Malaysia by some 400 miles (640 km) of the South China Sea. These two states occupy roughly the northern fourth of the large island of Borneo and share a land boundary with the Indonesian portion (Kalimantan) of the island to the south. Surrounded by Sarawak is a small coastal enclave containing the sultanate of Brunei. Of the country’s total area, which includes about 265 square miles (690 square km) of inland water, Peninsular Malaysia constitutes about 40 percent and East Malaysia about 60 percent. Relief The long, narrow, and rugged Malay Peninsula extends to the south and southwest from Myanmar and Thailand. The Malaysian portion of it is about 500 miles (800 km) long and—at its broadest east-west axis—about 200 miles (320 km) wide. About half of Peninsular Malaysia is covered by granite and other igneous rocks, one-third is covered by stratified rocks older than the granite, and the remainder is covered by alluvium. At least half the land area lies more than 500 feet (150 metres) above sea level. Peninsular Malaysia is dominated by its mountainous core, which consists of a number of roughly parallel mountain ranges aligned north-south. The most prominent of these is the Main Range, which is about 300 miles (480 km) long and has peaks exceeding 7,000 feet (2,100 metres). Karst landscapes—limestone hills with characteristically steep whitish gray sides, stunted vegetation, caves created by the dissolving action of water, and subterranean passages—are distinctive landmarks in central and northern Peninsular Malaysia. Bordering the mountainous core are the coastal lowlands, 10 to 50 miles (15 to 80 km) wide along the west coast of the peninsula but narrower and discontinuous along the east coast. East Malaysia is an elongated strip of land approximately 700 miles (1,125 km) long with a maximum width of about 170 miles (275 km). The coastline of 1,400 miles (2,250 km) is paralleled inland by a 900-mile (l,450-km) boundary with Kalimantan. For most of its length, the relief consists of three topographic features. The first is the flat coastal plain. In Sarawak, where the coastline is regular, the plain averages 20 to 40 miles (30 to 60 km) in width, while in Sabah, where the coastline is rugged and deeply indented, it is only 10 to 20 miles (15 to 30 km) wide. Inland from the coastal plain is the second topographic feature, the hill-and-valley region. Elevations there generally are less than 1,000 feet (300 metres), but isolated groups of hills reach heights of 2,500 feet (750 metres) or more. The terrain in this region is usually irregular, with steep-sided hills and narrow valleys. The third topographic feature is the mountainous backbone that forms the divide between East Malaysia and Kalimantan. This region, which is higher and nearer to the coast in Sabah than in Sarawak, is composed of an eroded and ill-defined complex of plateaus, ravines, gorges, and mountain ranges. Most of the summits of the ranges are between 4,000 and 7,000 feet (1,200 and 2,100 metres). Mount Kinabalu towers above this mountain complex; at 13,455 feet (4,101 metres), it is the highest peak in Malaysia and in the Southeast Asian archipelago as a whole. Drainage Peninsular Malaysia is drained by an intricate system of rivers and streams. The longest river—the Pahang—is only 270 miles (434 km) long. Streams flow year-round because of the constant rains, but the volume of water transported fluctuates with the localized and torrential nature of the rainfall. Prolonged rains often cause floods, especially in areas where the natural regimes of the rivers have been disrupted by uncontrolled mining or agricultural activities. As in Peninsular Malaysia, the drainage pattern of East Malaysia is set by the interior highlands, which also form the watershed between Malaysia and Indonesia. The rivers, also perennial because of the year-round rainfall, form a dense network covering the entire region. The longest river in Sarawak, the Rajang, is about 350 miles (563 km) long and is navigable by shallow-draft boats for about 150 miles (240 km) from its mouth; its counterpart in Sabah, the Kinabatangan, is of comparable length but is navigable only for about 120 miles (190 km) from its mouth. The rivers provide a means of communication between the coast and the interior, and historically, most settlement has taken place along the rivers. Soils The soils of both portions of Malaysia have been exposed for a long period of time to intense tropical weathering, with the result that most of their plant nutrients have been leached out. Soils typically are strongly acidic and coarse-textured and have low amounts of organic matter. Any organic matter is rapidly oxidized when exposed to weathering, and the soils consequently become even poorer. Soil erosion is always a danger on sloping ground, where such preventive measures as building contour embankments or planting protective cover crops are required. Only a small proportion of the soils of Peninsular Malaysia is fertile, necessitating regular application of fertilizer to sustain crop yields. Generally, soil conditions in Sarawak and Sabah do not differ greatly from those on the peninsula. Of these three regions, only Sabah has appreciable areas of fertile soils. These are found in the southeastern coastal areas, where the parent substance from which the soil is formed is composed of chemically basic volcanic materials. More … Score: https://www.britannica.com/place/Malaysia

2025/01/01

Feast of the Throne of Kingdom of Morocco

Morocco, mountainous country of western North Africa that lies directly across the Strait of Gibraltar from Spain. The traditional domain of indigenous peoples now collectively known as Berbers (self-name Imazighen; singular, Amazigh), Morocco has been subject to extensive migration and has long been the location of urban communities that were originally settled by peoples from outside the region. Controlled by Carthage from an early date, the region was later the westernmost province of the Roman Empire. Following the Arab conquest of the late 7th century ce, the broader area of North Africa came to be known as the Maghrib (Arabic: “the West”), and the majority of its people accepted Islam. Subsequent Moroccan kingdoms enjoyed political influence that extended beyond the coastal regions, and in the 11th century the first native Amazigh dynasty of North Africa, the Almoravids, gained control of an empire stretching from Andalusian (southern) Spain to parts of sub-Saharan Africa. Attempts by Europeans to establish permanent footholds in Morocco beginning in the late 15th century were largely repulsed, but the country later became the subject of Great Power politics in the 19th century. Morocco was made a French protectorate in 1912 but regained independence in 1956. Today it is the only monarchy in North Africa. Although the country is rapidly modernizing and enjoys a rising standard of living, it retains much of its ancient architecture and even more of its traditional customs. Morocco’s largest city and major Atlantic Ocean port is Casablanca, an industrial and commercial centre. The capital, Rabat, lies a short distance to the north on the Atlantic coast. Other port cities include Tangier, on the Strait of Gibraltar, Agadir, on the Atlantic, and Al-Hoceïma, on the Mediterranean Sea. The city of Fès is said to have some of the finest souks, or open-air markets, in all of North Africa. Scenic and fertile, Morocco well merits the praise of a native son, the medieval traveler Ibn Baṭṭūṭah, who wrote that “it is the best of countries, for in it fruits are plentiful, and running water and nourishing food are never exhausted.” Land Morocco borders Algeria to the east and southeast, Western Sahara to the south, the Atlantic Ocean to the west, and the Mediterranean Sea to the north. It is the only African country with coastal exposure to both the Atlantic Ocean and the Mediterranean Sea. Its area—excluding the territory of Western Sahara, which Morocco controls—is slightly larger than the U.S. state of California. Two small Spanish enclaves, Ceuta and Melilla, are situated on the country’s northern coast. Relief of Morocco Most of Morocco lies at high elevations, averaging about 2,600 feet (800 metres) above sea level. Two chains of mountains divide eastern from Atlantic Morocco: the Rif Mountains in the north form a buffer along the Mediterranean coastline, whereas the Atlas Mountains create a barrier across the centre. The two parts of the country are connected by the narrow Taza Gap in the northeast as well as by roads that follow older traditional routes. The Atlas and Rif ranges were formed during the Paleogene and Neogene periods (between about 65 to 2.6 million years ago) by the folding and uplifting of sediment that had accumulated in the Tethys Sea, which, at that time, bordered the northern coast of Africa. The Rif Mountains are geologically part of the cordilleras (mountain chains) reaching southward from the Iberian Peninsula of Europe, from which Africa was separated only after the Neogene Period (i.e., during the past 2.6 million years). The crescent-shaped range rises abruptly from a narrow Mediterranean coastal plain. Most of the limestone peaks in the Rif Mountains surpass 4,900 feet (1,500 metres) and rise to 8,058 feet (2,456 metres) at Mount Tidirhine.The Atlas Mountains comprise three distinct chains. The High Atlas (Haut Atlas), 460 miles (740 km) long, begins as small hills at the edge of the Atlantic, rises rapidly to more than 6,500 feet (2,000 metres), and reaches 13,665 feet (4,165 metres) at Mount Toubkal, Morocco’s highest point. The Middle Atlas (Moyen Atlas) trends away from the High Atlas in a northerly direction, rising to 10,958 feet (3,340 metres) at its crest. The Anti-Atlas extends southwestward from the High Atlas to the Atlantic.East of the Rif and Atlas ranges is the Moulouya basin, a semiarid lowland created by the eroding force of the Moulouya River. Farther east are the High Plateaus (Hauts Plateaux) of eastern Morocco, which lie roughly between 3,900 and 4,250 feet (1,200 and 1,300 metres) in elevation and are extensions of landforms in neighbouring Algeria. The arid regions to the south and southeast of the Atlas constitute the northwestern limit of the Sahara, whereas a narrow transitional band at the base of the mountains is called the pre-Sahara. Atlantic Morocco consists of plains formed of relatively fine sediments and plateaus of coarser deposits. The Sebou River basin, which lies in the northwest between the Rif Mountains and a line running roughly from Rabat to Fès, is a large alluvial plain. Its agricultural heart is known as the Gharb plain. South of the Rabat-Fès line, between the Atlas and the Atlantic Ocean, are a series of high plains known collectively as the Moroccan Plateau. These include the Saïs Plain near Fès and Meknès, the Tadla Plain to the northeast of Marrakech, the Haouz Plain west of Marrakech, and the broad Chaouïa, Doukkala, and Abda plains south of Casablanca. Between the High Atlas and Anti-Atlas ranges is the Sous River valley. Morocco’s coastline is regular and has few natural harbours. Before modern ports were constructed, sandbars and rocky reefs offshore made navigation difficult. Drainage Morocco’s mountains capture significant amounts of rain and snow on their windward slopes from storms coming in off the North Atlantic and give rise to numerous perennial watercourses. Indeed, the country has the most-extensive stream network in North Africa. Most streams arise either on the western slopes of the Atlas Mountains or on the southern slopes of the Rif Mountains and flow westward to the Atlantic Ocean. The Sebou is some 280 miles (450 km) long and has the largest volume of any Moroccan river. With its tributaries, the Sebou accounts for almost half of Morocco’s surface water resources. The Drâa, which rises in the High Atlas at the confluence of the Dadès and the Imini, is Morocco’s longest river, approximately 685 miles (1,100 km) in length; all but the headstreams and upper course are usually dry. At 345 miles (555 km) long, the Oum el-Rbia is another significant river, flowing from the Middle Atlas to the Atlantic. The Moulouya is the only major river flowing to the Mediterranean Sea; it originates on the eastern slopes of the Middle Atlas and flows about 320 miles (515 km) to its mouth, which lies near the Algerian frontier. The northern slopes of the Rif are drained by several short streams that also empty into the Mediterranean. Several minor streams originate on the dry eastern slopes of the High Atlas and flow into the Sahara; these include the Guir, the Rheris, and the Ziz. Although their volume is small, they have cut deep gorges. Since the 1930s Morocco’s streams have progressively been dammed for irrigation, hydroelectricity, and flood control. Soils A dark clay-marl soil known as tirs, which is found on the Chaouïa, Doukkala, and Abda plains, produces good yields of wheat and barley when precipitation is sufficient and can retain enough moisture to support summer pasture. Hamri, a light reddish siliceous soil found throughout the Saïs Plain surrounding Meknès and Fès, supports productive vineyards and can also produce good cereal yields, though it has poor moisture retention. Dhess is the main soil type of the Sebou basin. A silt-rich alluvial soil, it provides the foundation for much of Morocco’s modern irrigated agriculture. Other major soil types, less suitable for agriculture, are rmel, a sandy soil found in the Mamora Forest region east of Rabat and along much of the northern coast, and haroucha, a rocky soil found throughout Morocco’s semiarid regions. More … Score: https://www.britannica.com/place/Morocco

2025/01/01

Independence day of the Republic of Haiti

Haiti, country in the Caribbean Sea that includes the western third of the island of Hispaniola and such smaller islands as Gonâve, Tortue (Tortuga), Grande Caye, and Vache. The capital is Port-au-Prince. Haiti, whose population is almost entirely descended from African slaves, won independence from France in 1804, making it the second country in the Americas, after the United States, to free itself from colonial rule. Over the centuries, however, economic, political, and social difficulties as well as a number of natural disasters have beset Haiti with chronic poverty and other serious problems. Land Haiti is bordered to the east by the Dominican Republic, which covers the rest of Hispaniola, to the south and west by the Caribbean, and to the north by the Atlantic Ocean. Cuba lies some 50 miles (80 km) west of Haiti’s northern peninsula, across the Windward Passage, a strait connecting the Atlantic to the Caribbean. Jamaica is some 120 miles (190 km) west of the southern peninsula, across the Jamaica Channel, and Great Inagua Island (of The Bahamas) lies roughly 70 miles (110 km) to the north. Haiti claims sovereignty over Navassa (Navase) Island, an uninhabited U.S.-administered islet about 35 miles (55 km) to the west in the Jamaica Channel. Relief and drainage The generally rugged topography of central and western Hispaniola is reflected in Haiti’s name, which derives from the indigenous Arawak place-name Ayti (“Mountainous Land”); about two-thirds of the total land area is above 1,600 feet (490 metres) in elevation. Haiti’s irregular coastline forms a long, slender peninsula in the south and a shorter one in the north, separated by the triangular-shaped Gulf of Gonâve. Within the gulf lies Gonâve Island, which has an area of approximately 290 square miles (750 square km). Haiti’s shores are generally rocky, rimmed with cliffs, and indented by a number of excellent natural harbours. The surrounding seas are renowned for their coral reefs. Plains, which are quite limited in extent, are the most productive agricultural lands and the most densely populated areas. Rivers are numerous but short, and most are not navigable. The backbone of the island of Hispaniola consists of four major mountain ranges that extend from west to east. The most northerly range, known as the Cordillera Septentrional in the Dominican Republic, occurs in Haiti only on Tortue Island, off the northern coast. Tortue Island has an area of about 70 square miles (180 square km). In the 17th century it was a stronghold of privateers and pirates from various countries. The second major range, Haiti’s Massif du Nord (“Northern Massif”), is a series of parallel chains known in the Dominican Republic as the Cordillera Central. It has an average elevation of some 4,000 feet (1,200 metres). The Citadel (Citadelle Laferrière), a fortress built by Haitian ruler Henry Christophe in the early 19th century, stands atop one of the peaks overlooking the city of Cap-Haïtien and the narrow coastal plain. An interior basin, known as the Central Plateau in Haiti and the San Juan Valley in the Dominican Republic, occupies about 150 square miles (390 square km) in the centre of the country. The plateau has an average elevation of about 1,000 feet (300 metres), and access to it is difficult through winding roads. It is bounded by two minor mountain ranges on the west and south—respectively, the Cahos Mountains and the Noires Mountains. The Artibonite River—the island’s longest, approximately 175 miles (280 km) long—rises in the western Dominican Republic in the Cordillera Central and follows a southwestward course along the border with Haiti. Its tributaries flow eastward and southward through Haiti’s Central Plateau to a point near the Dominican border, where they join the river proper as it turns westward. The Artibonite then skirts the Noires Mountains as it flows to the Gulf of Gonâve. In eastern Haiti the river was impounded as Lake Péligre in the mid-20th century; a hydroelectric complex began operating at Péligre in 1971, but its power output has been unreliable during the dry season. Just upstream from the Artibonite’s delta in the Gulf of Gonâve, some of its waters are used to irrigate the triangular Artibonite Plain. The third major range, known as the Matheux Mountains (Chaîne des Matheux) in west-central Haiti and the Trou d’Eau Mountains (Chaîne du Trou d’Eau) farther east, corresponds to the Sierra de Neiba in the Dominican Republic. The range forms the northern boundary to the narrow Cul-de-Sac Plain, which is immediately adjacent to Port-au-Prince and includes the brackish Lake Saumâtre on the Dominican border. South of the Cul-de-Sac Plain is the fourth major range, called the Massif de la Selle in Haiti and the Sierra de Baoruco in the Dominican Republic. It rises to 8,773 feet (2,674 metres) at Mount Selle, the highest point in the country. The range’s western extension on the southern peninsula is called the Massif de la Hotte (Massif du Sud), which rises to 7,700 feet (2,345 metres) at Macaya Peak. The Cayes Plain lies on the coast to the southeast of the peak. Haiti’s mountains are mainly limestone, although some volcanic formations can be found, particularly in the Massif du Nord. Karstic features, such as limestone caves, grottoes, and subterranean rivers, are present in many parts of the country. A long fault line crosses the southern peninsula and passes just south of Port-au-Prince. Haiti is subject to periodic seismic activity; earthquakes destroyed Cap-Haïtien in 1842 and Port-au-Prince in 1751 and 1770. In January 2010 another catastrophic earthquake and its aftershocks resulted in severe damage to Port-au-Prince. Buildings collapsed throughout the capital and surrounding region, including many homes as well as large public structures such as the National Palace, the city’s cathedral, and hospitals. Estimates of the number of people killed ranged upward of 200,000, and several hundred thousand others were injured. More than a million people were made homeless. To the west of the capital, near the quake’s epicentre, the city of Léogâne was almost completely ruined. Soils The soils in the mountains are thin and lose fertility quickly when cultivated. The lower hills are covered with red clays and loams. The alluvial soils of the plains and valleys are fertile but overcultivated, owing to high population densities in those areas. Deforestation has caused much soil erosion, and as much as one-third of Haiti’s land may have eroded beyond recovery. Climate of Haiti Haiti has a warm, humid tropical climate characterized by diurnal temperature variations that are greater than the annual variations; temperatures are modified by elevation. Average temperatures range from the high 70s F (about 25 °C) in January and February to the mid-80s F (about 30 °C) in July and August. The village of Kenscoff, at some 4,700 feet (1,430 metres), has an average temperature of about 60 °F (16 °C), whereas Port-au-Prince, at sea level, has an average of 79 °F (26 °C). In winter, frost can occur at high elevations. Haiti is located on the leeward side of the island, which means that the influence of humid trade winds is not as great as in the Dominican Republic. The more humid districts are found on the northern and eastern slopes of the mountains. Some portions of the island receive less than 28 inches (700 mm) of rainfall per year. The northwestern peninsula and Gonâve Island are particularly dry. Some regions have two rainy seasons, lasting from April to June and from August to October, whereas other regions experience rainfall from May to November. Annual variations of precipitation can cause droughts, widespread crop failures, and famine. The southern peninsula, which is more vulnerable to hurricanes (tropical cyclones) than other parts of Haiti, suffered heavy damage from Hurricanes Allen (1980), Gilbert (1988), and Georges (1998). All parts of the country, however, can be hit by tropical storms and hurricanes. During August and September 2008 a series of severe storms that included Hurricanes Hanna and Ike caused widespread damage and the loss of some 800 lives. More … Source: https://www.britannica.com/place/Haiti  

2025/01/01

Anniversary of the Proclamation of Independence Republic of Sudan

South Sudan, also called Southern Sudan, country located in northeastern Africa. Its rich biodiversity includes lush savannas, swamplands, and rainforests that are home to many species of wildlife. Prior to 2011, South Sudan was part of Sudan, its neighbour to the north. South Sudan’s population, predominantly African cultures who tend to adhere to Christian or animist beliefs, was long at odds with Sudan’s largely Muslim and Arab northern government. South Sudan’s capital is Juba. South Sudan was settled by many of its current ethnic groups during the 15th–19th centuries. After the Sudan region was invaded in 1820 by Muḥammad ʿAlī, viceroy of Egypt under the Ottoman Empire, the southern Sudan was plundered for slaves. By the end of the 19th century the Sudan was under British-Egyptian rule. Although the north accepted British rule relatively quickly, there was greater resistance in the south. Because of this, British energies in the north were free to be directed toward modernization efforts, whereas in the south they were more focused on simply maintaining order, leading to a dichotomy of development between north and south that continued for several decades. After Sudan became independent in 1956, numerous governments over the years found it difficult to win general acceptance from the country’s diverse political constituencies, especially in the south. An early conflict arose between those northern leaders who hoped to impose the vigorous extension of Islamic law and culture to all parts of the country and those who opposed this policy. The latter group included the majority of southern Sudan’s population, many of whom were already up in arms over fears that the south would be further marginalized by the northern-based government; those fears led to a lengthy civil war (1955–72). The Addis Ababa Agreement of 1972 ended the conflict only temporarily, and in the next decade widespread fighting resumed with the second civil war (1983–2005). Numerous discussions, cease-fires, and agreements between southern leaders and their northern counterparts occurred but yielded very little success until the 2005 Comprehensive Peace Agreement (CPA), which ended warfare and generated an outline of new measures to share power, distribute wealth, and provide security in Sudan. Significantly, it also granted southern Sudan semiautonomous status and stipulated that a referendum on independence for the region would be held in six years. Despite some obstacles, the eagerly awaited referendum did take place: a weeklong vote on independence for southern Sudan was held January 9–15, 2011, with the results indicating the south’s overwhelming preference to secede. The country of South Sudan declared independence on July 9, 2011. Land South Sudan is bounded on the north by Sudan; on the east by Ethiopia; on the south by Kenya, Uganda, and the Democratic Republic of the Congo; and on the west by the Central African Republic. Relief South Sudan’s vast plains and plateaus are drained by the Nile River and its tributaries. This river system runs from south to north across the entire length of the east-central part of the country. At the heart of the country is a clay plain, the centre of which is occupied by an enormous swampy region known as Al-Sudd (the Sudd). There are two contrasting upland areas. The Ironstone Plateau lies between the Nile-Congo watershed and the clay plain; its level country is marked with inselbergs (isolated hills rising abruptly from the plains). On the Uganda border there are massive ranges with peaks rising to more than 10,000 feet (3,000 metres). The Imatong Mountains contain Mount Kinyeti (elevation 10,456 feet [3,187 metres]), the highest point in South Sudan. Drainage and soils The Nile River system is the dominant physical feature, and all streams and rivers of South Sudan drain either into or toward the Nile. The White Nile (Baḥr Al-Abyaḍ) enters the country as the Mountain Nile (Baḥr Al-Jabal) from the south through rapids at Nimule on the Uganda border. After its confluence with the left- (west-) bank tributary known as the Baḥr Al-Ghazāl, the Mountain Nile becomes the White Nile. A little farther north along its course, the White Nile receives much of its water from the right-bank Sobat River, which flows from the Ethiopian Plateau to join the Nile near Malakal. Drainage in the country does not always reach the Nile rivers; the rivers of the southwest, for example, infrequently reach the Baḥr Al-Ghazāl system. In 1978 construction began on the Jonglei (Junqalī) Canal, which was planned to bypass Al-Sudd swamp and provide a straight well-defined channel for the Mountain Nile River to flow northward until its junction with the White Nile. It also would have drained the swamplands of the Sudd for agricultural use. The project was suspended in 1983 because of disruptions arising from the civil war between the north and the south. After the CPA was signed in 2005, there was discussion about resuming work on the canal, spearheaded by the Egyptian government and Sudan’s Khartoum government, although the government of southern Sudan (GoSS) was hesitant to embrace the project and deferred making a decision about it until they could give the matter further study; a decision had not been made at the time of independence. The southern plains consist of an alkaline soil that is a heavy cracking clay. The clays of Al-Sudd were deposited in the area of impeded drainage. Climate of South Sudan South Sudan has a tropical climate with wet and dry seasons. The seasons are characterized by the oscillation, north and south, of the boundary between moist southerly air and dry northerly air. This phenomenon, more specifically, involves the seasonal migration and pulsation of the northern tropical continental air mass and the southern maritime continental air mass, which are divided by the intertropical convergence zone. In winter the north winds of the tropical air mass blow across the country toward the front, which may be as far south as the Tropic of Capricorn. These winds are relatively cool and dry and usually bring no rain. By April the front begins to move northward, and the moist southerly air of the maritime air mass is drawn in from the South Atlantic Ocean. Because of this, South Sudan has a rainy season, the total length of which varies according to latitude and is generally no more than eight to nine months a year, beginning as early as April and continuing as late as December. South Sudan’s lowest annual temperatures are in the high 60s to high 70s F (low to mid-20s C) in the centre and north of the country, while the lowest annual temperatures in the outlying areas are slightly cooler, about high 50s to high 60s F (mid-10s to low 20s C). The highest annual temperatures for most of South Sudan generally range from the mid-80s to the mid-90s F (low to mid-30s C), although some areas toward the north of the country range from the mid-90s to mid-100s F (mid- to upper 30s C). The highest temperatures normally occur just before the rainy season. In South Sudan, most precipitation usually occurs during the summer months and varies across the country. The majority of the country receives about 30–40 inches (750–1,000 mm) annually. Areas in the western part of the country receive slightly more, about 40–60 inches (1,000–1,500 mm) annually, while some areas in the northeastern and southeastern parts of the country receive less, about 20–30 inches (500–750 mm). Some areas in the extreme southeast receive fewer than 20 inches (500 mm). More … Score: https://www.britannica.com/place/South-Sudan

2025/01/01