Independence day of the Republic of Peru

Peru, country in western South America. Except for the Lake Titicaca basin in the southeast, its borders lie in sparsely populated zones. The boundaries with Colombia to the northeast and Brazil to the east traverse lower ranges or tropical forests, whereas the borders with Bolivia to the southeast, Chile to the south, and Ecuador to the northwest run across the high Andes. To the west, territorial waters, reaching 200 miles (320 km) into the Pacific Ocean, are claimed by Peru. Peru is essentially a tropical country, with its northern tip nearly touching the Equator. Despite its tropical location, a great diversity of climates, ways of life, and economic activities is brought about by the extremes of elevation and by the southwest winds that sweep in across the cold Peru Current (or Humboldt Current), which flows along its Pacific shoreline. The immense difficulties of travel posed by the Andes have long impeded national unity. Iquitos, on the upper Amazon, lies only about 600 miles (965 km) northeast of Lima, the capital, but, before the airplane, travelers between the cities often chose a 7,000-mile (11,250-km) trip via the Amazon, the Atlantic and Caribbean, the Isthmus of Panama, and the Pacific, rather than the shorter mountain route.The name Peru is derived from a Quechua Indian word implying land of abundance, a reference to the economic wealth produced by the rich and highly organized Inca civilization that ruled the region for centuries. The country’s vast mineral, agricultural, and marine resources long have served as the economic foundation of the country, and, by the late 20th century, tourism had also become a major element of Peru’s economic development. Favourite destinations for international travelers include Machu Picchu, a site of ancient Inca ruins located about 50 miles (80 km) northwest of Cuzco, and museums housing artifacts excavated from ancient tombs in northern coastal Peru. Land - Relief Peru is traditionally described in terms of three broad longitudinal regions: the arid Costa on the west; the rugged Sierra, or Andes, system in the centre; and the wet and forested Amazonia—the tropical Amazon Basin—on the east. The Costa The coastal plain can be readily divided into three parts—north, central, and south—on the basis of the amount of level land and the distance between the Andean ranges and the sea. Generally speaking, the amount of level coastal land diminishes from north to south. In the northern region, from Ecuador to Chimbote, the plain is typically some 20 to 30 miles (30 to 50 km) wide, with a maximum width of more than 90 miles (140 km) in the Sechura Desert south of Piura. The central coastal region, which stretches from Chimbote to Nazca, is narrower than the northern region and is characterized by areas of rough hills that extend from the Andes to the shores of the ocean. From Nazca southward to the Chilean border the coast is for the most part lined by low mountains; the southern valleys are narrow, and only in scattered spots are level lands found near the ocean. The Sierra, or Andean, region Along the western edge of South America, the Andes Mountains were created by tectonic activity in which the South American Plate overrode the Nazca Plate. The Peruvian Andes are typical of mountain regions of the Pacific Rim: they are young in geologic terms, and their continuing uplift is manifested by frequent earthquakes and much instability. Three main backbones protrude from the Peruvian Andes; they are commonly called the cordilleras Occidental, Central, and Oriental, although these designations are not used within Peru. Slopes are relatively gentle in northern Peru, and maximum elevations seldom exceed 16,000 feet (about 5,000 metres). The Andes in central Peru are higher and more rugged. The ranges of the central zone form particularly difficult barriers to movement. The main pass east of Lima, for instance, is at an elevation of more than 15,000 feet (4,500 metres)—higher than many of the peaks in the north. Many of the mountains of central Peru are snowcapped and are a popular attraction for climbers and tourists. Of particular fame is the Cordillera Blanca, with the country’s highest peak, Mount Huascarán, at 22,205 feet (6,768 metres), and nearby Huascarán National Park (designated a UNESCO World Heritage site in 1985). In southern Peru the character of the Andes changes to that of a high plateau region; this is the Puna, with vast tablelands and elevations between 13,000 and 16,000 feet (about 4,000 and 5,000 metres). Scattered peaks, with elevations of up to about 21,000 feet (6,400 metres), protrude above the broad southern plateaus. Beginning northwest of Arequipa, many of the southern peaks form a volcanic chain that stretches into northern Chile, including Ampato, Huacla Huacla, and Misti. Amazonia of Peru The lower slopes of the western Andes merge with the heavily forested tropical lowlands of the Amazon Basin to form the region known as Amazonia, which occupies more than three-fifths of the area of Peru. An area of dense cloud forests is found in the zone immediately adjacent to the Andes. This area is referred to as the Montaña; the jungle areas in the eastern part of Amazonia are referred to as the Selva. The physiography of the region is characterized by rolling hills and level plains that extend eastward to the borders with Colombia, Brazil, and Bolivia. Elevations are uniformly low, ranging from about 3,300 feet (1,000 metres) at the eastern edge of the Andes to about 260 feet (80 metres) above sea level along the Amazon River at the Peru–Brazil border. Drainage Distinctive drainage patterns dissect the Costa, the Sierra, and Amazonia. Of the more than 50 rivers that flow west from the Andes across the Costa, most are short (usually less than 200 miles [325 km] long) and precipitous, with highly seasonal rates of flow. Most have a period of peak flow (usually during the December to March rainy season) followed by a long dry period; only the largest of the Costa rivers, such as the Santa, have dependable year-round flows. The Sierra not only contains the headwaters of the streams that flow to both the Pacific and the Amazon but also has a large area of internal drainage. In the south several rivers cross the altiplano in Peru to empty into Lake Titicaca, which is shared with Bolivia and is—at an elevation of 12,500 feet (3,810 metres)—the world’s highest navigable body of water. Amazonia is characterized by great rivers. The Amazon, with the largest volume of flow of any river in the world, has headwaters that rise in several places in the Peruvian Andes; one of the main branches, the Ucayali, originates in southern Peru some 1,700 miles (2,700 km) from its juncture with the main river. The Amazon is navigable, but such large tributaries as the Marañón, Huallaga, and Ucayali can be navigated only for relatively short distances west of the port of Iquitos. These rivers flow northward in long deep valleys before turning east to join the Amazon, forming mostly hindrances to transportation rather than important trade routes. More … Score: https://www.britannica.com/place/Peru

2024/07/28

Visit Maldives - The Sunny Side of Life

Tourism website as well as Visit Maldives website, and it shall be revised every two ... This form is accessible on https://www.ivisa.com/maldives-.

2024/07/28

Let's Go - Peru

Let's Go' adventure through the many unique and diverse activities found throughout Peru. In July, the Beautiful Destinations team went to Peru with 10 creators to explore & document different facets of Peru with the Luxury Collection. The intent was to bring together a diverse group of people in hopes that they could collaborate and learn from one another, to take something tangible home both from an experiential perspective and creative.

2024/07/27

Independence day of the Republic of Liberia

Liberia, country along the coast of western Africa. Liberia’s terrain ranges from the low and sandy coastal plains to rolling hills and dissected plateau further inland. The country is home to a lush rainforest containing a rich diversity of flora and fauna. Liberia is the only Black state in Africa never subjected to colonial rule and is Africa’s oldest republic. It was established on land acquired for freed U.S. slaves by the American Colonization Society, which founded a colony at Cape Mesurado in 1821. In 1824 the territory was named Liberia, and its main settlement was named Monrovia, which is the present-day capital. Liberian independence was proclaimed in 1847, and its boundaries were expanded. The country enjoyed relative stability until a rebellion in 1989 escalated into a destructive civil war in the 1990s that did not fully cease until 2003. The country’s first post-conflict elections, held in 2005, were noteworthy for the election of Ellen Johnson Sirleaf to the presidency, as she was the first woman to be elected head of state in Africa. Land Liberia is bounded by Sierra Leone to the northwest, Guinea to the north, Côte d’Ivoire to the east, and the Atlantic Ocean to the south and west. Relief The four physiographic regions of Liberia parallel the coast. The coastal plains are about 350 miles (560 km) long and extend up to 25 miles (40 km) inland. They are low and sandy, with miles of beaches interspersed with bar-enclosed lagoons, mangrove swamps, and a few rocky promontories—the highest being Cape Mount (about 1,000 feet [305 metres] in elevation) in the northwest, Cape Mesurado in Monrovia, and Cape Palmas in the southeast. Parallel to the coastal plains is a region of rolling hills some 20 miles (32 km) wide with an average maximum elevation of about 300 feet (90 metres); a few hills rise as high as 500 feet (150 metres). It is a region suitable for agriculture and forestry. Behind the rolling hills, most of the country’s interior is a dissected plateau with scattered low mountains ranging from 600 to 1,000 feet (180 to 305 metres) in elevation; some mountains rise to 2,000 feet (600 metres). A striking feature of the mountainous northern highlands along the Guinea frontier is Mount Nimba. Drainage The Mano and Morro rivers in the northwest and the Cavalla in the east and southeast are major rivers and form sections of Liberia’s boundaries. Other major rivers are the Lofa in the north and, moving southward, the St. Paul, St. John, and Cestos, all of which parallel each other and flow perpendicular to the coast. The Farmington River is a source of hydroelectric power. Waterfalls, rapids, rocks, and sandbanks occur frequently in upstream sections of most rivers, inhibiting river traffic, and limiting navigation inland to short distances. During the rainy season there is often severe flooding in the coastal plains. Liberia forms part of the West African Shield, a rock formation 2.7 to 3.4 billion years old, composed of granite, schist, and gneiss. In Liberia the shield has been intensely folded and faulted and is interspersed with iron-bearing formations known as itabirites. Along the coast lie beds of sandstone, with occasional crystalline-rock outcrops. Monrovia stands on such an outcropping, a ridge of diabase (a dark-coloured, fine-grained rock). Soils Four types of soil are found in Liberia. Latosols of low to medium fertility occur in rolling hill country and cover about three-fourths of the total land surface. Shallow, coarse lithosols, in the hilly and rugged terrain, cover about one-eighth of the land. Infertile regosols, or sandy soils, are found along the coastal plains. Highly fertile alluvial soils represent a small percentage of the land area and are utilized largely for agriculture. Climate The climate, especially on the coast, is warm and humid year-round, dominated by a dry season from November to April and by a rainy season from May to October. The dusty and dry harmattan (desert winds) blow from the Sahara to the coast in December, bringing relief from the high relative humidity. Deforestation and drought in the Sahel have affected the climate, lengthening the dry season by almost a month in some areas. Mean annual temperatures range between 65° F (18° C) in the northern highlands to 80° F (27° C) along the coast. Rainfall is irregular, and the rainy season varies in intensity and begins earlier at the coast than in the interior. The greatest amount of rainfall, 205 inches (5,200 mm), occurs at Cape Mount and diminishes inland to about 70 inches (1,800 mm) on the central plateau. The interior has hot but pleasant days and cool nights during the dry season. Plant and animal life Liberia has year-round evergreen vegetation. Many trees—such as red ironwood, camwood, whismore, teak, and mahogany—are valuable, but occur with other species, preventing easy harvest. Other trees of value are rubber, cacao, coffee, and the raffia palm. Liberia’s rainforest used to abound with animals such as monkeys, chimpanzees, small antelopes, pygmy hippopotamuses, and anteaters. However, these animals, along with the already threatened elephants, bush cows (short-horned buffalo), and leopards, were hunted for food during the civil war; their populations are recovering. There are many reptiles, including three types of crocodiles and at least eight poisonous snakes. There are several unique species of bats and birds, and scorpions, lizards, and fish are numerous. Sapo National Park, established in 1983 in the country’s southeast, was expanded in 2003 to encompass an area of some 700 square miles (1,800 square km). The 2000s saw an expansion of protected regions in Liberia, with new and enlarged wildlife reserves at Gola National Forest, the Wonegizi National Forest Reserve, and Lake Piso, and ecotourism was seen as a potential growth industry for the country. People of Liberia - Ethnic groups and languages The people of Liberia are classified into three major groups: the indigenous people, who are in the majority and who migrated from the western Sudan in the late Middle Ages; Black immigrants from the United States (known historically as Americo-Liberians) and the West Indies; and other Black immigrants from neighbouring western African states who came during the anti-slave-trade campaign and European colonial rule. The Americo-Liberians are most closely associated with founding Liberia. Most of them migrated to Liberia between 1820 and 1865; continued migration has been intermittent. Americo-Liberians controlled the government until a military coup in 1980. Liberia’s indigenous ethnic groups may be classified into three linguistic groups, all belonging to the Niger-Congo language family: the Mande, Kwa, and Mel (southern Atlantic). The Mande are located in the northwest and central regions of Liberia and also in Senegal, Mali, Guinea, and Sierra Leone. Prominent among them are the Vai, who invented their own alphabet and who, in addition, use Arabic and English; the Kpelle, the largest Mande group, who are also found in Guinea; Loma (also found in Guinea); Ngbandi; Dan (Gio); Mano; Mende; and Malinke. Kwa-speaking peoples include the Bassa, the largest group in this category and the largest ethnic group in Monrovia; the Kru and Grebo, who were among the earliest converts to Christianity; the De; Belleh (Belle); and Krahn. The Kwa-speaking group occupies the southern half of the country. The Mel group includes the Gola and Kisi, who are also found in Sierra Leone and are known to be the oldest inhabitants of Liberia. These people live in the north and in the coastal region of the northwest. More than two dozen languages are spoken in Liberia. English is the official language. Predominant languages include Kpelle, Bassa, Grebo, Dan, Kru, Mano, Loma, and Mandingo (spoken by the Malinke). Religion About four-fifths of Liberians are Christian, about one-tenth are Muslim, and a small number profess other religions—primarily traditional beliefs—or are nonreligious. The largest number of Christians are Kpelle, followed by the Bassa. Some Liberians who identify themselves primarily as Christian incorporate traditional beliefs into their personal theologies. The Muslims are found predominantly among the Mande peoples in the northwest region of the country. Settlement patterns The present pattern of population distribution in Liberia is both a reflection of its migration history and a response to such social, economic, and cultural factors as war, employment, and superstition. Migrants from north-central Africa, who began to arrive in the 13th century, originally settled in the hinterlands but were driven by overcrowding to the coast. Immigrants from the United States and the West Indies, and from neighbouring African countries, also settled on the coast. The former migrated mostly to selected areas such as Monrovia (the oldest immigrant settlement), Buchanan, Edina, Greenville, Harper, Robertsport, and Marshall. Scattered settlements were created along newly constructed or improved roads, while plantation and mining activities encouraged larger settlements in a few interior and coastal areas. There are more than 2,000 villages, the majority of which are concentrated in central Liberia, in the northwest, and in the coastal region near Monrovia. The predominantly forested regions of south-central and northern Liberia have remained sparsely populated. There is a strong rural-to-urban movement, especially to Monrovia. Other destinations include enclaves around rubber plantations and mines. The trend toward urbanization has had little impact on the villages. The result has been the segmentation of Liberian society into two coexisting subsystems—traditional-rural and modern-urban. Monrovia, founded in 1822, is the focal point of political, economic, and cultural activities. Situated on the left bank of the St. Paul River on the ridge formed by Cape Mesurado, it commands an imposing view of the Atlantic Ocean and the coastal plains. The city and its outlying districts and suburbs occupy five square miles. The old style of architecture that once characterized it, reminiscent of that of the southern United States before 1860, is giving way to contemporary styles. All of the ethnic groups of Liberia are represented in its population, as are refugees, African nationals from other countries, and Europeans. Demographic trends More than two-fifths of the population of Liberia is under age 15; only about 5 percent is older than 60. The country’s birth and death rates are similar to or greater than those of other sub-Saharan African countries and are among the highest in the world. Life expectancy, about 57 years for males and 60 years for females, is similar to that of neighbouring countries and is among the lowest in the world. It fell as a result of the civil war and strife that began in the late 1980s and continued until 2003. Economy of Liberia The Liberian economy is predominantly agrarian, and raw materials, equipment, and consumer goods are imported. Production for export is carried out on a large scale through foreign investment in rubber, forestry, and mining. Foreign ships registering under a Liberian “flag of convenience” have made Liberia one of the world’s foremost countries in registered shipping tonnage. Liberia nevertheless remains primarily agricultural. The distribution of wealth is uneven, the coastal districts receiving a greater share of economic benefits than the hinterland, after which the administrative centres are the next beneficiaries. After the mid-1970s the once-vibrant economy took a sharp downturn. Between 1976 and 1980 sluggish demand and low prices stagnated the economy and the annual growth rate plunged. But gradual signs of recovery appeared, especially in agriculture and forestry. In the early 1990s, however, civil war disrupted Liberia’s economy. Since the end of the conflict in 2003, and particularly after a democratically elected government was inaugurated in early 2006, efforts to rebuild the country’s economic infrastructure have been under way. More … Source: https://www.britannica.com/place/Liberia

2024/07/26

Independence day of the Republic of Maldives

Maldives, in full Republic of Maldives, also called Maldive Islands, independent island country in the north-central Indian Ocean. It consists of a chain of about 1,200 small coral islands and sandbanks (some 200 of which are inhabited), grouped in clusters, or atolls. The islands extend more than 510 miles (820 km) from north to south and 80 miles (130 km) from east to west. The northernmost atoll is about 370 miles (600 km) south-southwest of the Indian mainland, and the central area, including the capital island of Male (Male’), is about 400 miles (645 km) southwest of Sri Lanka. Land The Maldive Islands are a series of coral atolls built up from the crowns of a submerged ancient volcanic mountain range. All the islands are low-lying, none rising to more than 6 feet (1.8 metres) above sea level. Barrier reefs protect the islands from the destructive effects of monsoons. The rainy season, from May to August, is brought by the southwest monsoon; from December to March the northeast monsoon brings dry and mild winds. The average annual temperature varies from 76 to 86 °F (24 to 30 °C). Rainfall averages about 84 inches (2,130 mm) per year. The atolls have sandy beaches, lagoons, and a luxuriant growth of coconut palms, together with breadfruit trees and tropical bushes. Fish abound in the reefs, lagoons, and seas adjoining the islands; sea turtles are caught for food and for their oil, a traditional medicine. People The population of Maldives belongs almost entirely to the Maldivian ethnic group, which is the result of various peoples settling in the islands successively through the country’s history. The first settlers, it is generally believed, were Tamil and Sinhalese peoples from southern India and Sri Lanka. Traders from Arab countries, Malaya, Madagascar, Indonesia, and China visited the islands through the centuries. The official language is an Indo-European language called Dhivehi (or Maldivian); Arabic, Hindi, and English are also spoken. Islam is the state religion. More than half of the population is considered rural. With the exception of those living in Male, the only relatively large settlement in the country, the inhabitants of the Maldives live in villages on small islands in scattered atolls. Only about 20 of the islands have more than 1,000 inhabitants, and the southern islands are more densely populated than the northern ones. The birth rate for the Maldives is somewhat higher than the world average, but the death rate is lower. More than one-fifth of the total population is under 15 years of age. Life expectancy is about 74 years for men and 79 for women. Economy Since the 1970s the economy of the Maldives has developed rapidly. Annual growth of gross domestic product (GDP) has been high, averaging about 6 percent in the 2010s, and the gross national income (GNI) per capita—among the lowest in the world in the 1970s—reached the level of upper middle-income countries by the late 2010s. The economy is based on tourism, fishing, boatbuilding, and boat repairing, with the tourism sector driving the rapid growth. Agriculture, forestry, and fishing Fishing, long the traditional base of the economy, has been far surpassed by tourism as the main source of gross domestic product (GDP). While the sector still produces the bulk of the country’s exports and continues to grow (albeit at a slower pace than the tourism industry), it employs less than one-fifth of the labour force and contributes less than one-tenth of the GDP. Tuna is the predominant fish caught, traditionally by the pole-and-line method, although a good deal of the fishing fleet has been mechanized. Most of the fish catch is sold to foreign companies for processing and export. Although formal businesses have seen rapid growth in the country, especially on the main islands, much of the population subsists outside the money economy on fishing, coconut collecting, and the growing of vegetables and melons, roots and tubers (cassava, sweet potatoes, and yams), and tropical fruits. Cropland, scattered over many small islands, is minimal, and nearly all the staple foods must be imported. Manufacturing Industries are largely of the handicraft or cottage type, including the making of coir (coconut-husk fibre) and coir products, fish canning, and boatbuilding. Textile and garment manufacturing was among the more lucrative industries from the mid-1990s until the 2005 expiry of an import quota regime in international textile trade left factories in the Maldives unable to compete. Construction makes up the bulk of the industrial sector. Trade Maldives entered the South Asian Free Trade Area (SAFTA) in 2006 and signed a free trade agreement with China in 2017. Imports include consumer goods such as food (principally rice), textiles, medicines, and petroleum products. Fish—mostly dried, frozen, or canned skipjack tuna—accounts for the bulk of exports. China, India, the United Arab Emirates, Thailand, Sri Lanka, and Singapore are among the main trading partners. Services The tourism industry, although nonexistent before 1972, underpins the services sector. Annually, more than 1.5 million tourists visit the Maldives. Its more than 130 resort islands include high-end hotel brands, and its marine geography offers unique diving and water sports opportunities as well as undersea accommodations, restaurants, and spas. By the mid-2010s the service sector accounted for four-fifths of the country’s GDP. Labour and taxation The rapid growth of the tourism industry left its mark on the labour market, which saw a dramatic shift away from agriculture and toward services. In part because of lack of training among the general population, a number of foreign workers from South Asia provide skills needed to help develop businesses. As businesses on resort islands away from the general populace demanded an increasing share of the total labour force, the participation rate of women, who are discouraged by the culture from living away from their families, fell substantially. About three-fifths of women participated in the labour force in the 1970s, but the rate dipped as low as one-fifth of women in the mid-1990s. By the 2010s, however, the participation rate had recovered to about half of women. Beginning in 2011, the Maldives collected taxes primarily on the profits of businesses and financial institutions and on goods and services within the tourism sector. An income tax was implemented in 2020. Transportation Transportation between islands and atolls is vital for the country. China and India, competing for influence over the strategically located Maldive Islands, have provided significant foreign direct investment to develop infrastructure that would further connect the islands. Boats provide the principal means of transport between the atolls, and scheduled shipping services link the country with Sri Lanka, Singapore, and India. The national airline carries passengers between several airports in the country as well as internationally. The airport at Male handles most international traffic, although there are other airports that serve limited international travel. More … Score: https://www.britannica.com/place/Maldives    

2024/07/26

Liberia Tourism, West Africa - Unravel Travel TV

Liberia, officially the Republic of Liberia, is a country in West Africa bordered by Sierra Leone to its west, Guinea to its north and Cote d'Ivoire to its east. It covers an area of 111,369 km sq and is home to about 3.7 million people.

2024/07/25

Visit Maldives

A promo video of Visit Maldives.

2024/07/25

Egyptian Tourism Authority

Egypt, a country linking northeast Africa with the Middle East, dates to the time of the pharaohs.

2024/07/25

Anniversary of the Revolution Arab Republic of Egypt

Egypt, country located in the northeastern corner of Africa. Egypt’s heartland, the Nile River valley and delta, was the home of one of the principal civilizations of the ancient Middle East and, like Mesopotamia farther east, was the site of one of the world’s earliest urban and literate societies. Pharaonic Egypt thrived for some 3,000 years through a series of native dynasties that were interspersed with brief periods of foreign rule. After Alexander the Great conquered the region in 323 bce, urban Egypt became an integral part of the Hellenistic world. Under the Greek Ptolemaic dynasty, an advanced literate society thrived in the city of Alexandria, but what is now Egypt was conquered by the Romans in 30 bce. It remained part of the Roman Republic and Empire and then part of Rome’s successor state, the Byzantine Empire, until its conquest by Arab Muslim armies in 639–642 ce. Until the Muslim conquest, great continuity had typified Egyptian rural life. Despite the incongruent ethnicity of successive ruling groups and the cosmopolitan nature of Egypt’s larger urban centres, the language and culture of the rural, agrarian masses—whose lives were largely measured by the annual rise and fall of the Nile River, with its annual inundation—had changed only marginally throughout the centuries. Following the conquests, both urban and rural culture began to adopt elements of Arab culture, and an Arabic vernacular eventually replaced the Egyptian language as the common means of spoken discourse. Moreover, since that time, Egypt’s history has been part of the broader Islamic world, and though Egyptians continued to be ruled by foreign elite—whether Arab, Kurdish, Circassian, or Turkish—the country’s cultural milieu remained predominantly Arab. Egypt eventually became one of the intellectual and cultural centres of the Arab and Islamic world, a status that was fortified in the mid-13th century when Mongol armies sacked Baghdad and ended the Abbasid caliphate. The Mamluk sultans of Egypt, under whom the country thrived for several centuries, established a pseudo-caliphate of dubious legitimacy. But in 1517 the Ottoman Empire defeated the Mamluks and established control over Egypt that lasted until 1798, when Napoleon I led a French army in a short occupation of the country. The French occupation, which ended in 1801, marked the first time a European power had conquered and occupied Egypt, and it set the stage for further European involvement. Egypt’s strategic location has always made it a hub for trade routes between Africa, Europe, and Asia, but this natural advantage was enhanced in 1869 by the opening of the Suez Canal, connecting the Mediterranean Sea to the Red Sea. The concern of the European powers (namely France and the United Kingdom, which were major shareholders in the canal) to safeguard the canal for strategic and commercial reasons became one of the most important factors influencing the subsequent history of Egypt. The United Kingdom occupied Egypt in 1882 and continued to exert a strong influence on the country until after World War II (1939–45). In 1952 a military coup installed a revolutionary regime that promoted a combination of socialism and Pan-Arab nationalism. The new regime’s extreme political rhetoric and its nationalization of the Suez Canal Company prompted the Suez Crisis of 1956, which was only resolved by the intervention of the United States and the Soviet Union, whose presence in the Mediterranean region thereafter kept Egypt in the international spotlight. During the Cold War, Egypt’s central role in the Arabic-speaking world increased its geopolitical importance as Arab nationalism and inter-Arab relations became powerful and emotional political forces in the Middle East and North Africa. Egypt led the Arab states in a series of wars against Israel but was the first of those states to make peace with the Jewish state, which it did in 1979. Egypt’s authoritarian political system was long dominated by the president, the ruling party, and the security services. With opposition political activity tightly restricted, decades of popular frustration erupted into mass demonstrations in 2011. The uprising forced Pres. Hosni Mubarak to step down, leaving a council of military officers in control of the country. Power was transferred to an elected government in 2012, and a new constitution was adopted at the end of the year. This elected government, however, was toppled a year later when the military intervened to remove the newly elected president, Mohamed Morsi, a member of the Islamist Muslim Brotherhood, following a series of massive public demonstrations against his administration. (For a discussion of unrest and political change in Egypt in 2011, see Egypt Uprising of 2011.) The ancient Greek historian Herodotus called Egypt the “gift of the Nile.” Indeed, the country’s rich agricultural productivity—it is one of the region’s major food producers—has long supported a large rural population devoted to working the land. Present-day Egypt, however, is largely urban. The capital city, Cairo, is one of the world’s largest urban agglomerations, and manufacturing and trade have increasingly outstripped agriculture as the largest sectors of the national economy. Tourism has traditionally provided an enormous portion of foreign exchange, but that industry has been subject to fluctuations during times of political and civil unrest in the region. Land of Egypt Egypt’s land frontiers border Libya to the west, Sudan to the south, and Israel to the northeast. Egypt’s border with Sudan is notable for two areas, the Ḥalāʾib Triangle along the Red Sea and Biʾr Ṭawīl further inland, that are subject to differing claims by the two countries (see Researcher’s Note). In the north its Mediterranean coastline is about 620 miles (1,000 km), and in the east its coastline on the Red Sea and the Gulf of Aqaba is about 1,200 miles (1,900 km). Relief The topography of Egypt is dominated by the Nile. For about 750 miles (1,200 km) of its northward course through the country, the river cuts its way through bare desert, its narrow valley a sharply delineated strip of green, abundantly fecund in contrast to the desolation that surrounds it. From Lake Nasser, the river’s entrance into southern Egypt, to Cairo in the north, the Nile is hemmed into its trenchlike valley by bordering cliffs, but at Cairo these disappear, and the river begins to fan out into its delta. The Nile and the delta form the first of four physiographic regions, the others being the Western Desert (Arabic Al-Ṣaḥrāʾ al-Gharbiyyah), the Eastern Desert (Al-Ṣaḥrāʾ al-Sharqiyyah), and the Sinai Peninsula. The Nile divides the desert plateau through which it flows into two unequal sections—the Western Desert, between the river and the Libyan frontier, and the Eastern Desert, extending to the Suez Canal, the Gulf of Suez, and the Red Sea. Each of the two has a distinctive character, as does the third and smallest of the Egyptian deserts, the Sinai. The Western Desert (a branch of the Libyan Desert) is arid and without wadis (dry beds of seasonal rivers), while the Eastern Desert is extensively dissected by wadis and fringed by rugged mountains in the east. The desert of central Sinai is open country, broken by isolated hills and scored by wadis. Egypt is not, as is often believed, an entirely flat country. In addition to the mountains along the Red Sea, mountainous areas occur in the extreme southwest of the Western Desert and in the southern Sinai Peninsula. The high ground in the southwest is associated with the ʿUwaynāt mountain mass, which lies just outside Egyptian territory. The coastal regions of Egypt, with the exception of the delta, are everywhere hemmed in either by desert or by mountain; they are arid or of very limited fertility. The coastal plain in both the north and east tends to be narrow; it seldom exceeds a width of 30 miles (48 km). With the exception of the cities of Alexandria, Port Said, and Suez and a few small ports and resorts such as Marsā Maṭrūh and Al-ʿAlamayn (El-Alamein), the coastal regions are sparsely populated and underdeveloped. More … Score: https://www.britannica.com/place/Egypt

2024/07/23