Physical Map Of Africa With Rivers And Mountains And Deserts Pdf – The African Transitional Zone divides North Africa from the rest of Africa due to climate and cultural dynamics. There are frequent cultural and desert conflicts in the region. Dry climates, type B drought, common in the Sahara Desert, dominate the north of the region. Tropical type A climates prevail in the south of the region. Global climate change continues to shape the continent. The shifting sands of the Sahara are slowly moving south towards the airfields. Desertification in the region continues as natural conditions and human activity put pressure on the region through drought and lack of precipitation. Climate type B also returns to the south of the tropics in southern latitudes. The Kalahari and Namib deserts are located in Southern Africa, especially in the countries of Botswana and Namibia.
For a continent as large as Africa, sub-Saharan Africa does not have high mountain ranges similar to ranges in North or South America, Europe, Asia or Antarctica. However, on the Ethiopian Highlands, the Ethiopian Plateau reaches as high as 15,000 feet in elevation. East Africa has many known volcanic peaks that are very high. The highest point in Africa, Mount Kilimanjaro in Tanzania near the border with Kenya, is 19,340 feet high. Near Kenya, Mount Kenya is 17,058 meters high. The Rwenzori Mountains on the Congo/Uganda border reach more than 16,000 feet in elevation and create a rain shadow effect for the region. There should be glaciers on these ranges even though they are near the equator. In the western part of the continent, Mt. Cameroon in Central Africa is more than 13,000 feet in elevation. The Cape Ranges of South Africa are low mountains that do not rise above about 6,000 feet. The continent of Africa consists of basins and plateaus without mountain ranges. Plateaus can be more than 1,000-2,500 feet in height. The only consistent feature is the eastern rifts that run along the tectonic plate boundaries from the Red Sea to South Africa.
Physical Map Of Africa With Rivers And Mountains And Deserts Pdf
The main rivers of Africa are the Nile, Niger, Congo and Zambezi. The Nile competes with the Amazon for the position as the longest river in the world; The White Nile branch originates from Lake Victoria in East Africa, and the Blue Nile branch originates in Lake Tana in Ethiopia. The Niger flows through West Africa; Your mouth is in Nigeria. The Congo River crosses the equator with a large watershed that creates a watershed second only to the Amazon in volume. The Zambezi River in the south is famous for Victoria Falls which crosses the border of Zambia and Zimbabwe. Victoria Falls is called the largest waterfall in the world. There are other important rivers such as the Orange River which is part of the border between South Africa and Namibia.
Political Map Of West Africa
There are a number of great lakes in sub-Saharan Africa. The largest is Lake Victoria, which is connected to the countries in East Africa, and is considered the second largest lake in the world. Only Lake Superior in North America has a larger area. There are a number of large lakes in the East Rift Valley. Three of the largest lakes in the west are Lake Malawi, Lake Tanganyika and Lake Albert. To the north-east of those in Kenya is Lake Turkana, which reaches the border of Ethiopia. Lake Chad is located in the African transitional zone on the border between Chad, Mali and Nigeria. Lake Chad has greatly decreased in size in recent years.
The equator runs through the center of sub-Saharan Africa, providing tropical climates a. These areas tend to have more rainfall, resulting in lighter, more porous soil that cannot function as well. Tollies. Root crops are traditional in Africa, such as millet and maize (corn). The savanna areas of the east and south have seasonal rains that affect the growing season. Soils in savanna areas are often not productive and cannot be relied upon to fulfill the agricultural needs of the growing population. Savannas are usually grasslands or dry forests with a seasonal rainfall pattern. Animal and livestock grazing is common in the savanna, and movements are frequent to follow seasonal grazing conditions. In certain areas of South Africa there are large agricultural activities in climates of type C. But West Africa is not blessed with the large areas of fertile lands found in the northern hemisphere. The ever-growing agrarian population is always dependent on the land for food and supplies, but these conditions do not bode well for the future of Africa. The population is growing faster than any increase in agricultural production.
The growing population in sub-Saharan Africa is paying the natural environment tax. Where carrying capacity is exceeded, capital is depleted at an unsustainable rate. Deforestation occurs in areas where firewood is in greatest demand, and trees are cut down faster than they can grow back. The increasing human population is also taking a toll on the natural biodiversity for which the African continent is famous. Big game animals such as rhinos, elephants and lions are hunted or poached with devastating results. The creation of game preserves and national parks has fueled this wave, but poaching is a serious problem even in the protected areas. Gorilla and chimpanzee populations have also been stressed by human population growth. People kill the animals for bushmeat, and human activities reduce their habitat.
An Introduction to Global Geography by R. Adam Dastrup, MA, GISP is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License, except where noted. described in the previous section. The continent, which is mostly composed of our own rigid block of ancient rock, has geologically zero mountains at its extremities in the mountains of the Atlas Mountains in the north and the Cape Ranges in the south. Between these mountainous regions there are a series of plains, with large areas or smaller masses, above which sometimes stand heavier and more resistant masses. Around these places is an area of low plateaus that are wide coastal belts along the Mediterranean coast, the coasts of Tanzania and Mozambique, a narrow belt between the rivers Niger and Kunene (Kunene), and the area north of Gambia and Senegal. Inge people.
Eswatini Maps & Facts
Kilimanjaro (19,340 feet [5,895 meters]) is the highest point on the continent; The lowest is Lake Assal (157 meters below sea level) in Djibouti. Relative to its size, Africa has fewer high mountains and lower plains than any other continent. The limited areas above 8,000 feet are either volcanic peaks or igneous masses. All land below 500 feet occurs within 500 miles of the coast, except for two small basins in the Sahara.
The higher areas of the south and east are in marked contrast to the lower elevation of the western and northern parts of the continent. South of a line drawn from the mouth of the Congo River to the Gulf of Aden, most of the land is 1,000 feet or more above sea level, and much of it is above 3,000 and even 4,000 feet. The northern line consists of low country above 3,000 feet, most of the area being between 500 and 1,000 feet above sea level; There are also coastal plains, except in the area of the Atlas Mountains and, in the east, beyond the Nile River.
The highest altitude areas are to be found in Ethiopia, some of which exceed 15,000 feet. In South East Africa the highest plateau is in Kenya, where it is often 8,000 feet or more above sea level; There are occasional volcanic peaks that are much higher, such as Kilimanjaro, Mount Kenya (17,058 feet), Meru (14,978 feet), and Elgon (14,178 feet). The Rwenzori Range (Rwenzori) – sometimes called the Moon Mountains – the highest of which is Margherita Peak (16,795 feet) on the borders of the Democratic Republic of Congo and Uganda, is not volcanic in origin. From East Africa, the plain extends south, often with a well-defined though not continuous escarpment particularly noticeable in the Drakensberg of Southern Africa, where Ntleniana, or Nchoniana, is 11,424 feet and Mont-aux-Fountain 10,823 feet high. There they marked the sides of the plane mainly because the rocks are very hard and they are crossed, while in Ethiopia they appeared because of mistakes. Where the rocks are soft and less resistant, the escarpment is not so pronounced and forms less of a barrier to atmospheric forces and to human movement.
To the north and west of the plateau region of the southern parts of the continent there is a general proximity to the small areas of the basins of the Congo, Niger, and Nile rivers. Only large areas extending above 3,000 feet are included
Cameroon Maps & Facts
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