Independence day of the Republic of Angola
Angola, country located in southwestern Africa. A large country, Angola takes in a broad variety of landscapes, including the semidesert Atlantic littoral bordering Namibia’s “Skeleton Coast,” the sparsely populated rainforest interior, the rugged highlands of the south, the Cabinda exclave in the north, and the densely settled towns and cities of the northern coast and north-central river valleys. The capital and commercial centre is Luanda, a large port city on the northern coast that blends Portuguese-style colonial landmarks with traditional African housing styles and modern industrial complexes. Angola at the beginning of the 21st century was a country ravaged by war and the related effects of land mines and malnutrition, and it was often dependent on the international community for the basics of survival. It is a country that is nevertheless rich in natural resources, including precious gems, metals, and petroleum; indeed, it ranks among the highest of the oil-producing countries in sub-Saharan Africa. It is the largest and wealthiest of the Portuguese-speaking African states, and Portuguese influences have been felt for some 500 years, although Angola acquired its present boundaries only in 1891. An anticolonial struggle that began in 1961 finally led to independence in 1975. In “We Must Return,” a poem he wrote from prison in 1956, the Angolan poet Agostinho Neto, who was also the country’s first president, described Angola as “red with coffee / white with cotton / green with maize” and as “our land, our mother.” Unfortunately, Neto’s happiness with a “liberated Angola—Angola independent” did not last long, and a civil war that went on 27 years left much of the country in ruins. Beginning in 2002, however, with the ending of the war, Angola had more hope for a peaceful future than it had in the previous quarter century. Land Angola is roughly square in shape, with a maximum width of about 800 miles (1,300 km), including the Cabinda exclave, which is located along the Atlantic coast just north of Angola’s border with the Democratic Republic of the Congo. Angola is bordered to the far northwest by the Republic of the Congo, to the north and northeast by the Democratic Republic of the Congo, to the southeast by Zambia, to the south by Namibia, and to the west by the Atlantic Ocean. Relief From a narrow coastal plain, the land rises abruptly to the east in a series of escarpments to rugged highlands, which then slope down toward the centre of the continent. The coastal plain varies in width from about 125 miles (200 km) in the area south of Luanda to about 15 miles (25 km) near Benguela. The Bié Plateau to the east of Benguela forms a rough quadrilateral of land above the 5,000-foot (1,500-metre) mark, culminating at about 8,600 feet (2,600 metres) and covering about one-tenth of the country’s surface. The Malanje highlands in the north-central part of the country are less extensive and lower in elevation, while the Huíla plateau in the south is smaller still but rises steeply to an elevation of approximately 7,700 feet (2,300 metres). The almost featureless plateau that covers the eastern two-thirds of Angola gradually falls away to between 1,650 and 3,300 feet (500 and 1,000 metres) at the eastern border. The highest point in the country is Mount Moco, near the city of Huambo, which reaches an elevation of 8,596 feet (2,620 metres). Drainage The Lunda Divide forms a watershed on the plateau, separating north- and south-flowing rivers. In the northeast, rivers such as the Cuango (Kwango) flow out of Angola into the mighty Congo River, which forms the boundary between Angola and the Democratic Republic of the Congo for the final 90 miles (145 km) of its course. The central part of the plateau is drained by the Cuanza (Kwanza), the largest river entirely within Angola’s frontiers, which is about 620 miles (1,000 km) in length. It runs for roughly half its length in a northerly direction before bending westward through a break in the escarpment between the Malanje highlands and the Bié Plateau, and it flows into the sea about 40 miles (65 km) south of Luanda. The southwestern part of the country is drained by the Cunene River (Kunene), which heads south before turning west and breaking through the escarpment at the Ruacana Falls, after which it marks the boundary between Angola and Namibia to the Atlantic Ocean. Some rivers in the southeast of the plateau flow into the Zambezi River, which itself crosses the Cazombo region in the far eastern extension of the country. Other rivers in this area feed the Okavango Swamps of northwestern Botswana. Small rivers in the south run into the internal drainage system of the Etosha Pan in Namibia, while others, often seasonal in nature, drain the steep western slopes of the escarpment. Soils The coastal plain consists of alluvia, chalk, and sand, underlain by oil-bearing formations over the northern two-thirds. Crystalline bedrock of Precambrian age (between about 540 million and 4 billion years old) emerges along the escarpment, and mineral deposits sometimes lie close to the surface. Considerable erosion has occurred in this area, and laterite formations are common. Most of the plateau in the eastern two-thirds of the country lies buried under deep deposits of infertile windblown Kalahari sands. The river gravels of the northeast contain diamonds, and rare kimberlite pipes occur in this area. Climate Angola has a tropical climate with a marked dry season. The climate is largely affected by the seasonal movements of the rain-bearing intertropical convergence zone, the northward flow of the cold Benguela Current off the coast, and elevation. Rainfall is the key determinant of climatic differentiation, and it decreases rapidly from north to south and in proximity to the coast. The Maiombe forest in the northern part of the Cabinda exclave receives the greatest amount of rainfall, about 70 inches (1,800 mm) per year, and Huambo, on the Bié Plateau, receives 57 inches (1,450 mm). In contrast, Luanda, on the dry coast, receives about 13 inches (330 mm), while the southernmost part of the coastal plain gets as little as 2 inches (50 mm). The rainy season lasts from September to May in the north and from December to March in the south. Droughts frequently afflict the country, especially in the south. Temperatures vary much less than rainfall, however, and generally decrease with distance from the Equator, proximity to the coast, and increasing elevation. The average annual temperature in Soyo, for example, at the mouth of the Congo, is 79 °F (26 °C), whereas in Huambo, on the Bié Plateau, it is 67 °F (19 °C). More … Score: https://www.britannica.com/place/Angola
Czytaj więcej2024/11/11
The Official Site for Tourism of Cambodia
Agency offering information about Cambodia on tourism, culture, history, visa, attractions, province guides, trip planner, hotels, flights, cars, tours, news, ...
Czytaj więcej2024/11/11
Odkryj Polskę / Explore Poland
Najpiękniejszy film o Polsce 2018. Niezwykła, zachwycająca, wyjątkowa i niepowtarzalna - POLSKA!
Czytaj więcej2024/11/10
Independence day of the Kingdom of Cambodia
Cambodia, country on the Indochinese mainland of Southeast Asia. Cambodia is largely a land of plains and great rivers and lies amid important overland and river trade routes linking China to India and Southeast Asia. The influences of many Asian cultures, alongside those of France and the United States, can be seen in the capital, Phnom Penh, one of a handful of urban centres in the largely rural country. For 2,000 years Cambodia’s civilization absorbed influences from India and China and, in turn, transferred them to other Southeast Asian civilizations. From the Hindu-Buddhist kingdoms of Funan and Chenla (1st–8th century) through the classical age of the Angkor period (9th–15th century), it held sway over territories that are now part of Thailand, Vietnam, and Laos. The Khmer (Cambodian) empire reached its apex in the 12th century, a time marked by the construction of the massive temple complexes known as Angkor Wat and Bayon and the imperial capital of Angkor Thom. Following 400 years of decline, Cambodia became a French colony and during the 20th century experienced the turmoil of war, occupation by the Japanese, postwar independence, and political instability. Between 1975 and 1979 the country was devastated by the reign of the Khmer Rouge, a rural communist guerrilla movement. During the Khmer Rouge’s period of power, at least 1.5 million Cambodians were killed or died, a monumental tragedy from which the country still suffers. Cambodia began the process of recovery under the Vietnam-backed regime of the People’s Republic of Kampuchea (1979–89), and in the 1990s it regained political autonomy, reestablished a constitutional government, and subsequently instituted free elections. The Cambodian economy has steadily improved, and the country seems to be living by the words of the Cambodian proverb, "Fear not the future, weep not for the past." Land Cambodia, about one-third the size of France and somewhat larger than the U.S. state of Missouri, is bordered to the west and northwest by Thailand, to the northeast by Laos, to the east and southeast by Vietnam, and to the southwest by the Gulf of Thailand. The country’s maximum extent is about 280 miles (450 km) from north to south and 360 miles (580 km) from east to west. Get a Britannica Premium subscription and gain access to exclusive content. Relief Cambodia’s landscape is characterized by a low-lying central alluvial plain that is surrounded by uplands and low mountains and includes the Tonle Sap (Great Lake) and the upper reaches of the Mekong River delta. Extending outward from this central region are transitional plains, thinly forested and rising to elevations of about 650 feet (200 metres) above sea level. To the north the Cambodian plain abuts a sandstone escarpment, which forms a southward-facing cliff stretching more than 200 miles (320 km) from west to east and rising abruptly above the plain to heights of 600 to 1,800 feet (180 to 550 metres). This escarpment marks the southern limit of the Dangrek (Khmer: Dângrêk) Mountains. Flowing south through the country’s eastern regions is the Mekong River. East of the Mekong the transitional plains gradually merge with the eastern highlands, a region of forested mountains and high plateaus that extend into Laos and Vietnam. In southwestern Cambodia two distinct upland blocks, the Krâvanh (Cardamom) Mountains and the Dâmrei (Elephant) Mountains, form another highland region that covers much of the land area between the Tonle Sap and the Gulf of Thailand. In this remote and largely uninhabited area, Mount Aôral, Cambodia’s highest peak, rises to an elevation of 5,949 feet (1,813 metres). The southern coastal region adjoining the Gulf of Thailand is a narrow lowland strip, heavily wooded and sparsely populated, which is isolated from the central plain by the southwestern highlands. Drainage The two dominant hydrological features of Cambodia are the Mekong River and the Tonle Sap. Rising in the Plateau of Tibet and emptying into the South China Sea, the Mekong enters Cambodia from Laos at the Khone Falls and flows generally southward to the border with Vietnam, a distance within Cambodia of approximately 315 miles (510 km). The Mekong is connected to the Tonle Sap by the Sab River. During the rainy season (mid-May to early October), the Mekong’s enormous volume of water backs up into the Sab and flows up into the Tonle Sap 65 miles (105 km) to the northwest, expanding the lake’s surface area from a dry-season minimum of 1,200 square miles (3,100 square km) to a rainy-season maximum of more than 3,000 square miles (7,800 square km). As the water level of the Mekong falls during the dry season, the process is reversed: water drains from the Tonle Sap back down into the Mekong, switching the direction of its flow. As a result of this annual phenomenon, the Tonle Sap is one of the world’s richest sources of freshwater fish. Soils Most of Cambodia’s soils are sandy and poor in nutrients. The so-called red-soil areas in the eastern part of the country, however, are suitable for commercial crops such as rubber and cotton. The annual flooding of the Mekong during the rainy season deposits a rich alluvial sediment that accounts for the fertility of the central plain and provides natural irrigation for rice cultivation. Climate of Cambodia Cambodia’s climate is governed by the monsoon winds, which define two major seasons. From mid-May to early October, the strong prevailing winds of the southwest monsoon bring heavy rains and high humidity. From early November to mid-March, the lighter and drier winds of the northeast monsoon bring variable cloudiness, infrequent precipitation, and lower humidity. The weather between these seasons is transitional. Maximum temperatures are high throughout the year, ranging from about 82 to 83 °F (28 °C) in January, the coolest month, to about 95 °F (35 °C) in April. Annual precipitation varies considerably throughout the country, from more than 200 inches (5,000 mm) on the seaward slopes of the southwestern highlands to about 50–55 inches (1,270–1,400 mm) in the central lowland region. Three-fourths of the annual rainfall occurs during the months of the southwest monsoon. Plant and animal life Although much of Cambodia is heavily forested, the central lowland region is covered with rice paddies, fields of dry crops such as corn (maize) and tobacco, tracts of tall grass and reeds, and thinly wooded areas. Savanna grassland predominates in the transitional plains, with the grasses reaching a height of 5 feet (1.5 metres). In the eastern highlands the high plateaus are covered with grasses and deciduous forests. Broad-leaved evergreen forests grow in the mountainous areas to the north, with trees 100 feet (30 metres) high emerging from thick undergrowths of vines, rattans, palms, bamboos, and assorted woody and herbaceous ground plants. In the southwestern highlands, open forests of pines are found at the higher elevations, while the rain-drenched seaward slopes are blanketed with virgin rainforests growing to heights of 150 feet (45 metres) or more. Vegetation along the coastal strip ranges from evergreen forests to nearly impenetrable mangroves. The northeastern forests of Cambodia—like the neighbouring areas of Laos and Vietnam—once sheltered large populations of wild animals such as elephants, wild oxen, rhinoceroses, and several species of deer, but the loss of forest cover, combined with warfare and unregulated hunting in the region, sharply reduced those numbers. Small populations of most of these species may still be found, along with some tigers, leopards, bears, and many small mammals. Among the more common birds are herons, cranes, grouse, pheasant, peafowl, pelicans, cormorants, egrets, and wild ducks. Four varieties of snakes are especially dangerous: the Indian cobra, the king cobra, the banded krait, and Russell’s viper. More … Score: https://www.britannica.com/place/Cambodia
Czytaj więcej2024/11/09
קמבודיה ומקדשי אנקור וואט
סרט הסבר על המקדשים המדהימים בקמבודיה אנגקור וואט כמה טיפים ממני ומידע על המקום המדהים הזה!!
Czytaj więcej2024/11/08
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Panama 2019 | 4K | must see places | travel guide
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Bethlehem, Palestine: Church of the Nativity
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