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The Great Rift Valley of Ethiopia, (or Main Ethiopian Rift or Ethiopian Rift Valley) is a branch of the East African Rift that runs through Ethiopia in a southwest direction from the Afar Triple Junction . In the past, it was seen as part of a "Great Rift Valley " that ran from Mozambique to Syria . The Great Rift Valley lies between the Ethiopian Plateau to the north and the Somalia Plateau to the south. The rift developed as the Nubian and Somalian plates began to separate during the Miocene Period along the East African rift system. Rift initiation was asynchronous along the Ethiopian rift valley: deformation began around 18 million years ago at the south end, around 11 million years ago close to the Afar depression and probably around 6-8 million years ago in the central sector. The Ethiopian rift valley is about 80 kilometers (50 mi) wide and bordered on both margins by large, discontinuous normal faults that give rise to major tectonic escarpments separating the rift floor from the surrounding plateaus. These faults are now thought to be inactive at the northern rift valley termination, whereas to the south they are still tectonically and seismically active. The rift floor is cut by a series of smaller en echelon, right-stepping, rift basins of Quaternary to recent age. Ethiopian Rift Valley

Ethiopian rift valley

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the Ethiopian rift valley is the only rift valley that can be seen from the space. the origin of humans,that is why Ethiopia is the cradle of human kind!!

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Page 1: Ethiopian rift valley

The Great Rift Valley of Ethiopia, (or Main Ethiopian Rift or Ethiopian Rift Valley) is a branch of the East African Rift that runs through Ethiopia in a southwest direction from the Afar Triple Junction. In the past, it was seen as part of a "Great Rift Valley" that ran from Mozambique to Syria.

The Great Rift Valley lies between the Ethiopian Plateau to the north and the Somalia Plateau to the south. The rift developed as the Nubian and Somalian plates began to separate during the Miocene Period along the East African rift system. Rift initiation was asynchronous along the Ethiopian rift valley: deformation began around 18 million years ago at the south end, around 11 million years ago close to the Afar depression and probably around 6-8 million years ago in the central sector. The Ethiopian rift valley is about 80 kilometers (50 mi) wide and bordered on both margins by large, discontinuous normal faults that give rise to major tectonic escarpments separating the rift floor from the surrounding plateaus. These faults are now thought to be inactive at the northern rift valley termination, whereas to the south they are still tectonically and seismically active. The rift floor is cut by a series of smaller en echelon, right-stepping, rift basins of Quaternary to recent age.

Ethiopian Rift Valley

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These basins are about 20 kilometres (12 mi) wide and 60 kilometres (37 mi) long. In the northern part of the rift, extension within the valley is now thought to be mainly along these faulted and magmatically active segments. These segments are considered to be developing mid ocean ridge spreading centers.

Lucy (Australopithecus)

Lucy is the common name of AL 288-1, several hundred pieces of bone representing about 40% of the skeleton of a female Australopithecus Afarensis. It was discovered in 1974 at Hadar in the Awash Valley of Ethiopia's Afar Depression.

lucy

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ERTA’ALE VOLCANO and DALOLThe Danakil depression in north east of Ethiopia drops to more than 100m below sea level. It is an area continuing seismic activity, with earth tremors frequently felt amidst the hot yellow sulfur fields and several still-active volcanoes.

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Rift valley lakes1.Lake AwassaLake Awasa is an endorheic basin in Ethiopia, located in the Main Ethiopian Rift south of Addis Ababa, the lake is 16 km long and 9 km wide, with a surface area of 129 square kilometers. It has a maximum depth of 10 meters and is located at an elevation of 1,708 meters. Because it is relatively accessible to scientists, Lake Awasa is the most studied of the Rift Valley lakes in Ethiopia.

Sunset at lake AwssaMalachite Kingfisher at Lake Awassa

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Lakes Abaya & Chamo Arba Minch , Ethiopia

Divided by the lyrical ‘Bridge of God’, Lakes Abaya and Chamo are both beautiful. Measuring 1160 sq km, Lake Abaya is Ethiopia’s second-largest lake. Its peculiar reddish-brown waters are a result of elevated natural concentrations of suspended sediments. While the more conventionally colored Lake Chamo supports a much larger population of crocodiles, Abaya’s are more aggressive against people and animals because the lake has few fish, their preferred food.

BROWN LAKE ABAYA

crocodile and hippo at chamo

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Lake LanganoAccording to figures published by the Central Statistical Agency, Lake Langano is 18 kilometers long and 16 km wide, with a surface area of 230 square kilometers and a maximum depth of 46 meters. The lake has a catchment 1600 square kilometers in size, and is drained by the Hora Kallo river which empties into the adjacent Lake Abijatta. As it is free of Bilharzia (schistosomiasis), unlike all other freshwater lakes in Ethiopia, Lake Langano is popular with tourists and city-dwellers. The lake is brown in color. There are a number of resorts around the lake and water sports are popular. There is a variety of wildlife around the lake, which include hippos (rare), monkeys, baboons, warthogs, and a huge variety of birds. The area around the lake is largely deforested, however, and a large number of herders live around the area.

Lake Langano

Lake Langano at the sunset

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Abijatta-Shalla Lakes National Park is in Ethiopia. Thousands of flamingos create pink carpets in the blue bays of the lake; great white pelicans soar in the lake.

Abijatta-Shalla Lakes National ParkThe park was created for the many aquatic bird species that use the lakes, particularly great white pelicans and greater and lesser flamingo. Shalla’s islands are used as breeding sites by many birds, and is home to the continent's most important breeding colony of great white pelicans. Because of the lake's lack of fish, the birds fly to Lake Abijatta — which has no islands — to feed. Other birds include white-necked cormorant, African fish eagle, Egyptian geese, various plover species, and herons. Although renowned for its bird life, Abijatta is now outclassed by Lake Awasa farther to the south.Local mammals are not numerous but include Grant's gazelle — the northern limit for this species — greater kudu, oribi, warthog, and golden jackal.

Ostrich

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Lake Beseka In the Rift Valley has grown to its largest size ever amid irrigation runoff and seismic shifts in past years. Should salt waters contaminate the Awash River, they would risk Ethiopia’s oldest state-owned sugar estate and an India-funded project downstream that’s key to the government’s $5 billion plan to turn the country into a top sugar exporter. Beseka, fed by hot springs at 954 meters (3,130 feet), has swollen from a 3-square-kilometer pond in the 1960s to 45 square kilometers, causing the diversion of a road from Addis Ababa to Djibouti’s port, a main trade route in landlocked Ethiopia.

Lake Beseka

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High land lakes of EthiopiaLake TanaRivalling the attraction of the Blue Nile Falls are the thirty-seven islands scattered about on the 3,000-square-kilometre (1,860-square-mile) surface of Ethiopia's largest body of water: Lake Tana, which gives birth to the Blue Nile. Some twenty of these shelter churches and monasteries of immense historical and cultural interest; decorated with beautiful paintings and housing innumerable treasures.Lake Tana, largest lake of Ethiopia, located in a depression of the northwest plateau, 6,000 feet (1,800 meters) above sea level. It forms the main reservoir for the Blue Nile (Abbay) River, which drains its southern extremity near Bahir Dar. The lake's surface covers 1,418 square miles (3,673 square km), with a surrounding drainage of 4,500 square miles (11,650 square km); its maximum depth is 45 feet (14 metres. The islands and peninsulas of Lake Tana are most conveniently approached by boat from Bahir Dar on the southern side of the lake, though boats can often also be obtained at Gorgora on the northern shore.The many interesting and historic locations on or around the lake include the islands of Birgida Maryam, Dega Estefanos, Dek, Narga, Tana Cherkos, Mitsele Fasilidas, Kebran, and Debre Maryam, as well as the Gorgora, Mandaba, and Zeghe peninsulas. All have fine churches. Though founded much earlier, most of the actual buildings date from the late sixteenth or early seventeenth centuries. Many have beautiful mural paintings and church crosses, and house crowns and clothes of former kings.

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Access to the churches is, for the most part, closed to women; they are allowed to land on the banks of the islands but not permitted to proceed any further. The clergy sometimes agree to bring some of their treasures to the water's edge for women visitors to inspect. Women are, however, permitted to visit churches on the Zeghe peninsula, the nearby church of Ura Kidane Mehret, and Narga Selassie.Kebran Gabriel, the nearest monastery to Bahir Dar, is a principal tourist attraction. Established in the fourteenth century and rebuilt during the reign of Emperor lyasu I (1682-1 706), it is an unassuming but nevertheless impressive building with a distinct cathedral atmosphere.Lira Kidane Mehret is another popular attraction, with the added advantage that women are allowed inside. Located on the Zeghe peninsula, the monastery is an integral part of the local community. The church design dates from the same time as that of the Kebran Gabriel church, but it is a more decorative building, with colourful frescoes depicting biblical scenes from biblical lore and the history of the Ethiopian Orthodox Church.The third principal attraction is Dega Estefanos, which is also closed to women. Although farther away from Bahir Dar, it is well worth visiting. A steep trek up a winding path leads towards the monastery on the summit. Some ninety metres (300 feet) above the lake's surface are low, round, thatched-roof buildings that house the monks, and nearby an arch set into a high stone wall leads to a grassy clearing, at the centre of which stands the church of St Stephanos, a relatively new building erected about a century ago after the original structure had burned down in a grass fire.

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The real historic interest in Dega Estefanos, however, lies in its treasury. Here, together with numerous piles of brightly coloured ceremonial robes, are coffins containing the mummified remains of several former emperors: Yekuno Amlak, who restored the Solomonic dynasty in 1270; Dawit, late fourteenth century; Zara Yaqob, fifteenth century; Za Dengel, early seventeenth century; and Fasilidas, also seventeenth century. The modern, glass-sided coffins allow visitors to view the mummified bodies.Dega Estefanos is also said to have served as a temporary hiding place for Ethiopia's most jealously guarded religious relic - the Ark of the Covenant. Tradition has it that the Ark was brought to the island for safekeeping in the sixteenth century, when the Muslim forces of warlord Ahmed Gragn attacked and occupied Axum, where the Ark normally rested.History aside, bird lovers should make a point to visit Fasilidas Island, near the eastern side of the lake. And, of course, when moving around on the lake, be sure to notice the interesting tankwa boats, which may be seen making their way between the islands and the mainland. These little papyrus boats, open at the back end, appear dangerously unwaterworthy as they slide over the surface, but they continue to carry passengers and goods to and from the islands as they have done for centuries.

Sunset at lake Tana

monasteries

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Lake Ashenge (also Lake Ashangi) is a lake in the northern Tigray Region of Ethiopia. Located in the Ethiopian highlands at an elevation of 2409 meters, it has no outlet. According to the Statistical Abstract of Ethiopia for 1967/68, Lake Ashenge is five kilometers long and four wide, with a surface area of 20 square kilometers.The British explorer Henry Salt, who notes that the Tigrinya name of the lake is Tsada Bahri ("White Sea") from the number of birds which cover its surface, records a local tradition that a large city once stood on the site of Ashenge, but "it was destroyed, in his displeasure, by the immediate hand of God.

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Hayq, EthiopiaFrom Wikipedia, the free encyclopedia

                                             Hayq (or Haik) it is a town in northern Ethiopia. It is named after Lake Hayq, which lies two kilometers east of the city and is the home of Istifanos Monastery, an important landmark in Ethiopian Church history. Located 28 kilometers north of Dessie in the Tehuledere woreda of the Debub Wollo Zone of the Amhara Region, the town has a latitude and longitude of 11°18′N 39°41′E and an elevation of 2030 meters above sea level.Notable landmarks include the churches Hayq Timhirt and Hayq Yohannis. Near the town is the church of Hayq Tekle Haymanot, founded according to tradition in 862 by Saint Kalae Salama during the reign of king Dil Na'od.During the mid-1980s, local educational services was augmented by the Swedish Wello Environment Education Project, which ran a secondary school. Hayq was formerly the capital of the Amba Sel woreda or district in Wollo.

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Bale Mountains National ParkThe Bale Mountains, The Bale Mountains National Park is located 400 km southeast of Addis Ababa in Oromia National Regional State in south-eastern Ethiopia. It was established in 1970, this park covers about 2,200 square kilometers of the Bale Mountains to the west and southwest of Goba in the Bale Zone It belongs to the Bale-Arsi massif, which forms the western section of the south - eastern Ethiopian highlands. And it is the largest area of Afro-alpine habitat in the whole of the continent.It is a home for various flora and fauna species. The park which comprises reverie plains, woodlands and bush land, is a home for several endemic species like Mountain Nyala and Semien Fox, where the park is believed to be established to protect these two animals. Bale-Park National Park is home to high mountains, The local boundary of the BMNP lies within five woredas: Adaba (west), Dinsho (north), Goba (northeast), Mana-Angetu (south) and Berbere (east). The park area is encompassed within geographical coordinates of 6º29' – 7º10'N and 39º28' – 39º57'E and covers the largest area above 3000 m asl. in Africa. Tullu Dimtuu, altitude 4377m a.s.l., is the highest peak in the park and the second highest peak in Ethiopia. The park includes a major Afro alpine plateau over 3500 m a.s.l. as well the slopes to the south that include low land tropical moist forest down to 1500 m as.l,.

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The forest is also a home for different pig species, lions, leopards, spotted hyenas, African hunting dogs and many others. More over the Bale Mountains are home for 16 endemic bird species. The park is among the most suitable walking areas in the country with a chance to see several endemic and common species at a closer distanceFaunaThe BMNP encompasses a broad range of habitats between 1,500 and 4,377 m altitude. These provide a large number of niches for animals, and as a result there is great variety in the fauna. Much of the original stimulus for making a National Park in the Bale Mountains was the plights of the endemic Mountain Nyala and the Ethiopian wolf. There are, in fact, at least 46 mammal species, and 160 bird species, in addition to the numbers of species from other animal orders-reptiles, amphibians etc., that all have a part in the complex ecosystems that have evolved in this unusual area.A large proportion of the Bale Mountains fauna is endemic- found nowhere else in the world, and in some cases nowhere else in Ethiopia. The variety of species and high rate of endemicity is due to the wide variety of habitats conserved in BMNP and to the isolation of the highland areas of Ethiopia from other similar highlands in Eastern Africa, by the surrounding hot dry lands. Ethiopia as a whole has a large number of endemic species.

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FloraThe three main sub-sections of the park Northern Gaysay area, Central peaks and Sannetti plateau area and Southern Harenna area are demarcated by altitude, and this also controls vegetation zonation. Thus the central peaks and plateau area consists of Afroalpine vegetation; the northern Gaysay area of grassland, swamp and woodlands; and the southern Harenna area of dense forest.1. Northern grasslandsThis very small, but very important zone comprises the flat land each side of the Gaysay River, and on the west bank of the Web River. The area occurs in the extreme north of the park, between Gaysay Mountain and the Adelay Ridge.These grasslands lie on almost flat land, whose drainage is poor, and inundation is frequent in the west season. Many places are, therefore, dominated by swamp grasses and sedges, especially of the Cyperus and Sciripus genera. Relatively higher parts are covered with low bush vegetation, dominated by Artemesia afra and Helichrysum splendium. Common grasses of these areas include those of the genera Andropogon, Bromus, Festuca and Poa.The bush species Helichrysum splendium has been almost totally eradicated outside the park boundaries by domestic sheep and goats. Protection by the park fences has allowed it to re-grow in the park, to a point where it appears to be taking over from the Artemesia. Both species are important food plants for Mountain Nyala, and shelter for several species.

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2. Northern WoodlandsThis vegetation zone occupies a narrow belt in the northern west, north and north east of the park. The upper limit is the tree line at 3,400 m, and the lower is the grasslands in flat valley bottoms at around 3,000 m. The term “woodland” has been used here, as opposed to forest, since tree cover is sparse with an incomplete canopy, a high inter-tree distance and only a single canopy layer for the most part. Ground cover by herbs and grasses is good. This vegetation zone is found on slopes that are relatively steep (20 - 30º), and has, in many places, been affected by man’s activities.The species that dominate the northern woodlands are the trees Juniperus procera and Hagenia abyssinica. Most Junipers are relatively small (15-20 m tall) since the area is the upper limit to the species growth, and few are found near the upper tree line.The species Hypericum revolutum, produces a dense bush growth at the lower edge of the woodlands, while at the upper tree line the species grows as a tall, slender tree to at least 5 m.Extensive grass area occurs within the woodland especially on the steepest slopes. These contain similar species to the flat areas below, with the exception of the sedges. Some such areas have been artificially induced on high, flat ridges that were used for settlement in the past.

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3. Heather moorlandsVarious heather species dominate the areas immediately above the tree line, from 3,400 to about 3,800 m altitude. Heathers in the genera Erica and Philipia cover all but the inundated valley bottoms. These plants will grow to over 5 m in height, but only exhibit this in a few places in the mountains. This vegetation is repeatedly burnt by local people, mainly to make the area more accessible and generate plants of a height that can be browsed by livestock. As a result the plants are rarely more than 1.5 m in height, and often much less.Mature heather stands exhibit a good grass and herb layer beneath the canopy. Frequently burnt areas have a poor ground cover, of low species diversity. 4. Afro alpine moorlandsThis broad term covers a great range of microhabitats, controlled by a variety of soils, drainage, exposure and aspect in the high mountain area. Plant species diversity is low, and vegetation cover varies from 100% at the lower end of the altitude range and in sheltered areas, to less than 10% at the highest and exposed altitudes. Steep, rocky slopes and cliffs support very little vegetation growth. The higher in altitude a plant species is found, the smaller the growth form is likely to be as a protection against wind and frost. An additional factor that a major effect on vegetation at these altitudes, is the very high density of rodents, particularly the Giant Molerat (Tachyoryctes macrocephalus). The soil is constantly turned over and the plants cropped by the activities of these animals, such that many places on the Sanetti Plateau look as though they have been ploughed.

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There are many flat areas on the plateau which become quickly inundated in the wet season, or remain wet year round. These swampy areas are dominated by the sedge Carex monostachya.A distinctive feature of the vegetation of these altitudes is the giant plant Lobelia rynchopetalum. This species is found from 3,100 to 4,377 m, but the largest forms are found at the highest altitudes. The plant itself is unbranched, but reaches a height of 2-3 m before flowering, then sends up a tall flower spike to a total of 6 m or more. The dead flower spikes last for several years and are a characteristic sight of many parts of the central plateau and peak area.5. Harenna ForestThe Harenna Forest covers almost half of the park in area, at the southern park boundary and is a magnificent example of moist tropical forest, about which very little is known. It extends over a wide range of altitude, from 1,500 to 3,500 m, bridging the gap between Combretum/Terminalia dry, wooded grasslands and Afro alpine moor lands in just 60 km, probably the only place in Africa where this still occurs.The upper part of this forest area is on steep slopes and differs little from the northern woodlands. A notable absence is Juniperus. The tree cover is very high and dense stands of Mountain Bamboo (Arundinaria alpine) cover large areas.Below about 2,200 m, the slope is much gentler, and larger tree species appear, Podocarpus gracilior in particular. Trees over 30 m in height are common, there is good shrub undergrowth, a secondary canopy, lianes and dense epiphytic growths on all larger trees.

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The steeper slopes of the forest on the Harenna Escarpment are swathed in mist for much of the year, often all day. There are no rainfall records for the area, but it is evident from the many small streams, dense epiphytes, and the dense forest and undergrowth, that this area receives, retains, and slowly releases