Ethiopia physical map Click to see large. After a winding course of about 800 km (497 mi), the Awash River passes (in its lower reaches) through a series of badds (lagoons) to Lake Abhe Bad (or Abhe Bid) on the border with Djibouti and some 100 to 110 km (62 to 68 mi) from the head of the Gulf of Tadjoura. Mica-schists form the prevalent rocks. Ethiopia has small reserves of gold, platinum, copper, potash, and natural gas. 2500x1920 / 549 Kb Go to Map. The East African tableland is continued into Ethiopia. Regional Directory of EuropeInformation and guide about Europe and websites with European topics. The upper (Magdala group) contains much trachytic rock of considerable thickness, lying perfectly horizontally, and giving rise to a series of terraced ridges characteristic of central Ethiopia. They range from the tropical lowlands to heights of 3,000 m (9,843 ft). Read more about Ethiopia here. Learn how to create your own. Great numbers of eagles, vultures, hawks, bustards and other birds of prey are met with; and partridges, duck, teal, guineafowl, sandgrouse, curlews, woodcock, snipe, pigeons, thrushes and swallows are very plentiful. Such are the Tekezé River in the north, the Abay in the center, and the Sobat in the south, and about four-fifths of the entire drainage is discharged through these three arteries. In the region of the headwaters of the Sobat the rains begin earlier and last longer. A season of light rain may be sufficient for the needs of Ethiopia, but there is little surplus water to find its way to the Nile; and a shortness of rain means a low Nile, as practically all the flood water of that river is derived from the Ethiopian tributaries. Elevation is generally highest just before the point of descent to the Great Rift Valley, which splits the plateau diagonally. Full size detailed physical map of Ethiopia. Winter, or the cold season, lasts from October to February. The Bale Mountains are separated from the larger part of the Ethiopian highlands by the Great Rift Valley, one of the longest and most profound chasms in Ethiopia. The people from Ethiopia are called Ethiopians. Boars and badgers are more rarely seen. The Akobo, in about 7°47′N 33°3′E / 7.783°N 33.050°E / 7.783; 33.050, joins the Pibor, which in about 8°30′N 33°20′E / 8.500°N 33.333°E / 8.500; 33.333 unites with the Baro, the river below the confluence taking the name of Sobat. Regions of Ethiopia Map Eleven Regions of Ethiopia. Ethiopia is located in the Horn of Africa.It is bordered by Eritrea to the north, Djibouti and Somalia to the east, Sudan and South Sudan to the west, and Kenya to the south. However, in the deep valleys of the Tekezé and Abay, and generally in places below 1,200 m (3,937 ft), the conditions are tropical and diseases such as malaria are prevalent. The capital is Addis Ababa (‘New Flower’), located almost at the center of the country. Lions abound in the low countries and in Somaliland. It is bordered by Eritrea to the north, Djibouti and Somalia to the east, Sudan and South Sudan to the west, and Kenya to the south. The Beles, however, is perennial, and the Rahad and Dinder are important rivers in flood-time. 1915x1651 / 0,98 Mb Go to Map. Ethiopia Facts and Country Information... Ethiopia is situated in Northeast Africa bordered by Sudan, Kenya, Eritrea, Somalia and Djibouti, offering some of the highest and fascinating sites in Africa. On its northern face, the plateau falls in terraces to the level of the eastern Sudan. It reaches the Sudanese plains near Kassala, beyond which place its waters are dissipated in the sandy soil. In the former provinces of Gojjam and Welega, heavy rains continue till the middle of September. There are numerous hot springs in Ethiopia, such as Sodere. the "Terrible") rises some 5 m (16.4 ft) above its normal level, and at this time forms an impassable barrier between the northern and central regions. But the rainy season proper, caused by the southwest monsoon, lasts from June to mid-September, and commencing in the north moves southward. North of 11° N the hills turn more to the east and fall more gradually to the East Sudanian savanna plains at their base. Go back to see more maps of Ethiopia  Cities of Ethiopia. The following formations are represented: Archaean.– The metamorphic rocks compose the main mass of the tableland, and are exposed in every deep valley in Tigre and along the valley of the Blue Nile. On nearly every side, the walls of the plateaus rise abruptly from the plains, constituting outer mountain chains. Leopards, both spotted and black, are numerous and often of great size; hyenas are found everywhere and are hardy and fierce; the lynx, wolf, wild dog and jackal are also common. Among the varieties are the greater and lesser kudu (both rather rare); the duiker, gemsbuck, hartebeest, gerenuk (the most common—it has long thin legs and a camel-like neck); klipspringer, found on the high plateaus as well as in the lower districts; and the dik-dik, the smallest of the antelopes, its weight rarely exceeding 5 kg (11 lb), common in the low countries and the foothills. In this chain of scenic upland lakes – some fresh, some brackish, some completely closed, others connected by short channels – the chief links in their order from north to south are: Zway, communicating southwards with Hara and Lamina, all in the Arsi Zone; then Abijatta with an outlet to a smaller turn to the Baroda and Gamo areas, skirted on the west sides by grassy slopes and wooded ranges from 2,000 m (6,562 ft) to nearly 3,000 m (9,843 ft) high; lastly, Lake Chew Bahir (formerly known as Lake Stephanie) which is completely closed and falling to a level of about 550 m (1,804 ft) above sea level. East of the highlands towards the Red Sea there is a strip of lowland semi-desert, the Ethiopian xeric grasslands and shrublands. Squirrels and hares are numerous, as are several kinds of monkeys, notably the guereza, gelada, guenon and dog-faced baboon. The rain is heaviest in the Tekezé basin in July and August. All these are perennial rivers. This lake receives at its northern end the waters of the Omo, which rises in the Shoan highlands and is a perennial river with many affluents. There are in the south large forests of valuable timber trees; and the coffee plant is indigenous in the Kaffa country, whence it takes its name. Jurassic.– The fossiliferous Antalo Limestones are generally horizontal, but are in places much disturbed when interstratified with Mekelle Dolerite. [2], Of the total land area, about 20 percent is under cultivation, although the amount of potentially arable land is larger. The highest peaks are found in the Semien and Bale ranges. (adsbygoogle = window.adsbygoogle || []).push({}); Description: Detailed clear large road map of Ethiopia with road routes from cities to towns, road intersections to provinces and perfectures. Some land is too rugged, dry, or infertile for agriculture or any other use. Administrative map of Ethiopia. The Somali Region and the Danakil Depression in the Afar Region have a hot, sunny and dry climate producing fully desert or semi-desert conditions. The Semien Mountains lie northeast of Lake Tana and culminate in the snow-covered peak of Ras Dashen, which has an altitude of 4,550 m (14,928 ft). [2] Questions remain about the precise location of small parcels along the border with Sudan as well. The folia of the schists strike north and south.

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