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Lake Tana Lake Tana, the largest lake in Ethiopia, is the source and from where the famed Blue Nile starts its long journey to Khartoum, and into the Mediterranean Sea. The 37 islands that are scattered the surface of the lake shelter fascinating churches and monasteries. Some of which have histories dating back to the 13th century. A sail on Lake Tana is one of the most pleasant excursions for visitors in Ethiopia. Along the lake shore bird life, both local and migratory visitors, make the site an ideal place for bird-watchers. Bird lovers will not want to miss these islands, which are especially famous as an important wetland. The whole of the Lake Tana region and the Blue Nile gorge host a wide variety of birds both endemic and migratory visitors. The variety of habitats, from rocky crags to riverain forests and important wetlands, ensure that many other different species should be spotted. Abay Gorge It is situated 225 kms north of Addis Ababa. The majestic and enormous gorge is the most captivating in Africa. It has a magnificent, alluring physical feature and natural beauty. At the bottom of the gorge the bridge spans over the Abay (the Blue Nile). Langano Langano is located 212Km South of Addis Ababa. It is a sand beach that attracts many visitors. Along the road to Langano, one can see beautiful landscapes. As you continue driving, the first lake to be seen among the rift valley lakes is Lake Zeway. It is a shelter for a variety of birds and fish. Proceeding further to the South, Lake Abijata and Lake Shala can be reached. These lakes are breeding places for Flamingos and ideal for bird watching. Nearby is Lake Langano, a resort area and a paradise for holiday & Honeymoon makers. Lodges are available her. Lake Awassa is the most studied of the Rift Valley Lakes in Ethiopia, and it is a freshwater lake which indicates that even though it does not have a visible outlet, the water must leave through a subterranean outlet. Set in a volcanic crater, it has an abundance of plankton and fish, and supports a large city of the same name that has grown up on its edges. With a mountainous backdrop and beautiful vegetation, this is a beautiful lake to spend a night by. There is also a dyke which was built to stop flooding, which is perfect for bird watching – walking along it, fish eagle, black-winged lovebirds, yellow-fronted parrots and Ethiopian oriole are a few of the many species of birds that can be seen. Lake Ziway Is also a freshwater lake, and it has five islands of which one is said to have housed the Ark of the Covenant during 16century in order to protect it from an Islamic warrior named Gragn as nickname. The lake is fed by the Meki and Katar Rivers, but does not always have an outflow; sometimes it overflows into Lake Abiata. The lake has plenty of hippo in it, and has a healthy population of birds. With large numbers of Tilapia nilotica, a fish that can weigh up to 1.5 kg, the fishing industry does well here and the fish are served fresh in many of the restaurants in the nearby town. The fish also attract a large number of water-associated birds, which can be seen in the reed-lined fringes of the lake. Lake Abiata is to the south of Lake Ziway, and to the north there are a number of hot springs which are important to the locals, and are also a popular tourist attraction. The lake is saline, and has recently undergone a decline in water level. This has resulted in the loss of fish-eating birds as the fish have died, but an increase in algae-eating birds such as greater and lesser flamingos. Blue Nile The Blue Nile, in Ethiopia, in Amharic: Abbai is a river originating at Lake Tana in Ethiopia. With the White Nile, the river is one of the two major tributaries of the Nile. The upper reaches of the river is called the Abbay in Ethiopia, where it is considered holy by many, and is believed to be the River Gihon(Ghion) mentioned as flowing out of the Garden of Eden in Genesis chapter 2 verse 13. According to materials published by the Ethiopian Central Statistical Agency, the Blue Nile has a total length of 1,450 kilometers (900 mi), of which 800 km (500 mi) are inside Ethiopia. The Blue Nile flows generally south from Lake Tana and then west across Ethiopia and northwest into Sudan. Within 30 kilometers (19 mi) of its source at Lake Tana, the river enters a canyon about 400 kilometers (250 mi) long. This gorge is a tremendous obstacle for travel and communication from the north half of Ethiopia to the southern half. The power of the Blue Nile is best appreciated at Tis Issat Falls, which are 45 metres (148 ft) high, located about 30 kilometers (20 mi) downstream of Lake Tana. Although there are several feeder streams that flow into Lake Tana, the sacred source of the river is generally considered to be a small spring at Gish Abbai at an altitude of approximately 2,744 metres (9,003 ft). This stream, known as the Lesser Abay, flows north into Lake Tana. There are numerous tributaries of the Abay between Lake Tana and the Sudanese border. Those on its left bank, in downstream order, include the Wanqa River, the Bashilo River, the Walaqa River, the Wanchet River, the Jamma River, the Muger River, the Guder River, the Agwel River, the Nedi River, the Didessa River and the Dabus River. Those on the right side, also in downstream order, include the Handassa, Tul, Abaya, Sade, Tammi, Cha, Shita, Suha, Muga, Gulla River, Temcha, Bachat, Katlan, Jiba, Chamoga, Weter and the Beles. After flowing past Er Roseires inside Sudan, and receiving the Dinder on its right bank at Dinder, the Blue Nile joins the White Nile at Khartoum and, as the River Nile, flows through Egypt to the Mediterranean Sea at Alexandria. The Blue Nile is so-called because during flood times the water current is so high, it changes colour to an almost black; since in the local Sudanese language the word for black is also used for the colour blue. The distance from its source to its confluence is variously reported as 1,460 and 1,600 kilometres (907 and 1,000 miles). The uncertainty over its length might partially result from the fact that it flows through a virtually impenetrable gorges cut in the Ethiopian Highlands to a depth of some 1,500 metres (4,900 ft)—a depth comparable to that of the Grand Canyon of the Colorado River in the United States. The flow of the Blue Nile reaches maximum volume in the rainy season (from June to September), when it supplies about two thirds of the water of the Nile proper. The Blue Nile, along with that of the Atbara River to the north, which also flows out of the Ethiopian Highlands, were responsible for the annual Nile floods that contributed to the fertility of the Nile Valley and the consequent rise of ancient Egyptian civilization and Egyptian Mythology. With the completion in 1970 of the Aswan High Dam in Egypt, the Nile floods ended. The Blue Nile is vital to the livelihood of Egypt. Though shorter than the White Nile, 59% of the water that reaches Egypt originates from the Blue Nile branch of the great river; when combined with the Atbara River, which also has its source in the Ethiopian Highlands, the figure rises to 90% of the water and 96% of transported sediment. The river is also an important resource for Sudan, where the Roseires and Sennar dams produce 80% of the country's power. These dams also help irrigate the Gezira Plain, which is most famous for its high quality cotton. The region also produces wheat and animal feed crops. Blue Nile by European Explorers The first European to have seen the Blue Nile in Ethiopia and the river's source was Pedro Paez, a Spanish Jesuit who reached the river's source 21 April 1613. Nevertheless the Portuguese João Bermudes, the self-described Patriarch of Ethiopia, provided the first description of the Tis Issat Falls in his memoirs (published in 1565), and a number of Europeans who lived in Ethiopia in the late 15th century like Pêro da Covilhã could have seen the river long before Paez, but not reached its places of source. The source of the Blue Nile was also reached in 1629 by the Portuguese Jesuit missionary Jerónimo Lobo and in 1770 by James Bruce. Although a number of European explorers contemplated tracing the course of the Blue Nile from its confluence with the White Nile to Lake Tana, its gorge, which begins a few miles inside the Ethiopian border, has discouraged all attempts since Frédéric Cailliaud's attempt in 1821. The first serious attempt by a non-local to explore this reach of the river was undertaken by the American W.W. Macmillan in 1902, assisted by the Norwegian explorer B.H. Jenssen; Jenssen would proceed upriver from Khartoum while Macmillan sailed downstream from Lake Tana. However Jenssen's boats were blocked by the rapids at Famaka short of the Sudan-Ethiopian border, and Macmillan's boats were wrecked shortly after they had been launched. Macmillan encouraged Jenssen to try to sail upstream from Khartoum again in 1905, but he was forced to stop 300 miles short of Lake Tana. Consul Cheesman, who records his surprise on arriving in Ethiopia at finding that the upper waters of "one of the most famous of the rivers of the world, and one whose name was well known to the ancients" was in his lifetime "marked on the map by dotted lines", managed to map the upper course of the Blue Nile between 1925–1933. He did this not by following the river along its banks and through its impassible canyon, but following it from the highlands above, travelling some 5,000 miles (8,000 km) by mule in the adjacent country. River Awash The Awash (sometimes spelled Hawash; Afar We'ayot) is a major river of Ethiopia. Its course is entirely contained within the boundaries of Ethiopia, and empties into a chain of interconnected lakes that begin with Lake Gargori and end with Lake Abbe (or Abhe Bad) on the border with Djibouti, some 100 kilometers (60 or 70 miles) from the head of the Gulf of Tadjoura. It is the principal stream of an endorheic drainage basin covering parts of the Amhara, Oromia and Somali Regions, as well as the southern half of the Afar Region. The Awash rises south of Mount Warqe, west of Addis Ababa in the woreda of Ejerie, Mirab (West) Shewa Zone, Oromia. Thence the Awash flows south to loop around Mount Zuqualla in an easterly then northeasterly direction, passing the Awash National Park, and joined on its left bank by its chief affluent, the Germama (or Kasam) River, before turning northeast at approximately 11° N 40° 30' E as far north as 12° before turning completely east to reach lake Gargori. According to materials published by the Ethiopian Central Statistical Agency, the Awash River is 1200 kilometers long. The author of the 1911 Encyclopedia Britannica article describes its middle portion as "a copious stream nearly 200 feet [60 meters] wide and 4 feet [1.2 meters] deep in the dry season, and during the floods rising 50 or 60 feet [15 to 20 meters] above low-water mark, thus inundating the plains for many miles along both its banks." River Baro The Baro River is a river in southwestern Ethiopia, which defines part of Ethiopia's border with Sudan. From its source in the Ethiopian Highlands it flows west for 306 kilometres (190 mi) to join the Pibor River. The Baro river is created by the confluence of the Birbir and Gebba Rivers, east of Metu in the Illubabor Zone of the Oromia Region. It then flows west through the Gambela Region to join with the Pibor River, both of them creating the Sobat. Other notable tributaries of the Baro include the Alwero and Jikawo Rivers. Of the Sobat River's tributaries, the Baro River is by far the largest, contributing 83% of the total water flowing into the Sobat. During the rainy season, between June and October, the Baro River alone contributes about 10% of the Nile's water at Aswan, Egypt. In contrast, these rivers have very low flow during the dry season. The only navigable river in Ethiopia, the Baro's most important city is Gambela, which served as a port from 1907 until the 1990s when civil war in Ethiopia and Sudan forced shipping on the river to be halted. The second-longest bridge in Ethiopia crosses the Baro, connecting two parts of the Gambela Region. This bridge is 305 meters long. Omo River The Omo River is an important river of southern Ethiopia. Its course is entirely contained within the boundaries of Ethiopia, and empties into Lake Turkana on the border with Kenya. It is the principal stream of an endorheic drainage basin; the part that the Omo drains includes part of the western Oromia Region and the middle of the Southern Nations, Nationalities, and People's Region. During his second expedition (1895–1897), Vittorio Bottego was the first European explorer to follow the course of the lower Omo River to its confluence with Lake Turkana. This river rises in the Shewan highlands and is a perennial river. Its course is generally to the south, however with a major bend to the west at about 7° N 37° 30' E to about 36° E where it turns south until 5° 30' N where it makes a large S- bend then resumes its southerly course to Lake Turkana. According to materials published by the Ethiopian Central Statistical Agency, the Omo River is 760 kilometers long. In its course the Omo has a total fall of about 6000 ft (2,000 m), from an elevation of 7600 ft at its source to 1600 ft at lake-level, and is consequently a very rapid stream, being broken by the Kokobi and other falls, and navigable only for a short distance above where it empties into Lake Turkana, one of the lakes of the Great Rift Valley. The Spectrum Guide to Ethiopia describes it as a popular site for white-water rafting in September and October, when the river is still high from the rainy season.Its most important tributary is the Gibe River; smaller tributaries include the Wabi, Denchya, Gojeb, Mui and Usno rivers. On the banks of the Omo River archeologists have found fossil fragments of Olduwan hominids from the early Pleistocene era and up to the Pliocene era. An important finding is Australopithecus man, now extinct. The lower valley of the Omo is currently believed by some to have been a crossroads for thousands of years as various cultures and ethnic groups migrated around the region. To this day, the people of the Lower Valley of the Omo, including the Mursi, Surma, Nyangatom, Dizi Me'en, Karo, Dassench … are studied for their diversity. The entire Omo river basin is also important geologically and archaeologically. Several hominid fossils and archaeological localities, dating to the Pliocene and Pleistocene, have been excavated by French and American teams. Fossils belonging to the genera Australopithecine and Homo have been found at several archaeological sites, as well as tools made from quartzite, the oldest of which date back to about 2.4 million years ago. Because of this, the site was designated a UNESCO World Heritage Site in 1980. When they were discovered it was thought that the tools may have been part of a so-called pre-Oldowan industry, even more primitive than what was found in the Olduvai Gorge. Later research has shown that the crude looks of the tools were in fact caused by very poor raw materials, and that the techniques used and the shapes permit their inclusion in the Oldowan. Wabi Shebelle River The Wabi Shebelle River begins in the highlands of Ethiopia, and then flows southeast into Somalia towards Mogadishu. Near Mogadishu, it turns sharply southwest, where it follows the coast. Below Mogadishu, the river becomes seasonal. During most years, the river dries up near the mouth of the Jubba River, while in seasons of heavy rainfall; the river actually reaches the Jubba and thus the Indian Ocean. The Wabi Shebelle River’s name is derived from the Somali term Wabi Shabeelle, meaning "Leopard/Tiger River". According to materials published by the Ethiopian Central Statistical Agency, the Shebelle is 1130 kilometers long, extending for 1000 km inside Ethiopia and 130 km inside Somalia. The source of the Shebelle River is venerated by both the Arsi Oromo and the Sidamo people. It is surrounded by a sacred enclosure wooded with juniper trees, which as of 1951 was under the protection of a Muslim member of the Arsi. Tekezé River The Tekezé River is a major river of Ethiopia, and forms a section the westernmost border of Ethiopia and Eritrea for part of its course. The river is also known as the Setit in Eritrea, western Ethiopia, and eastern Sudan. According to materials published by the Ethiopian Central Statistical Agency, the Tekezé River is 608 kilometers long.The canyon which it has created is the deepest in Africa and one of the deepest in the world, at some points having a depth of over 2000 meters. The earliest known mention of the Tekezé is in an inscription from Axum of king Ezana of Axum, where he boasts of a victory in a battle on its lower banks, near "the ford of Kemalke".[4] The Tekezé served as an early link between Ethiopia and Egypt; for example, the Kebra Nagast, which received its current form in the 13th century, states that king Menelik I returned to Ethiopia by following this river from Egypt (ch. 53). Augustus B. Wylde records a related tradition that near the source of the Tekezé, at the location of Eyela Kudus Michael church, is the true resting-place of the Ark of the Covenant. Contact Us |
