Geography Of Oromia Region
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Geography Of Oromia Region
Geography of Oromia Region, the largest regional state of Ethiopia, is highly diverse. Occupying 353,690 square kilometers, it is bordered by Somalia, to the east, Afar Region to the north, Djibouti to north-east, Kenya, to the south, Amhara Region to the north, Benishangul-Gumuz to the north-west, Sudan to the north-west, Gambela to the west, and South Sudan to the west. The region is situated between 2° and 12°N, 34° and 44°E with varied landscape ranging from rugged mountain ranges in the center and the north, to flat grassland to the south-east. Oromia has varied climate grouped into three categories: dry climate, tropical rainy climate and temperate rainy climate. with the mean annual rainfall of 410-820 mm with noticeable variability from year to year. The region has enormous lakes and rivers: the Awash River is the largest responsible for source of electric power. Lakes including Bishoftu, Kuriftu and Ziway is the basis for agro-industrial and fishery production. ...
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Oromia IMG 5276 Ethiopia (27908694669)
Oromia (Amharic: ) ( om, Oromiyaa) is a regional state in Ethiopia and the homeland of the Oromo people. The capital of Oromia is Addis Ababa. It is bordered by the Somali Region to the east; the Amhara Region, the Afar Region and the Benishangul-Gumuz Region to the north; Dire Dawa to the northeast; the South Sudanese state of Upper Nile, Gambela Region, South West Ethiopia Region, Southern Nations, Nationalities, and Peoples' Region and Sidama Region to the west; the Eastern Province of Kenya to the south; as well as Addis Ababa as an enclave surrounded by a Special Zone in its centre and the Harari Region as an enclave surrounded by East Hararghe in its east. In August 2013, the Ethiopian Central Statistics Agency projected the 2022 population of Oromia as 35,467,001; making it the largest regional state by population. It is also the largest regional state covering Oromia is the world's 42nd most populous subnational entity, and the most populous subnational entity in ...
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Bale Mountains National Park
Bale Mountains National Park (BMNP) is a national park in Ethiopia. The park encompasses an area of approximately in the Bale Mountains and Sanetti Plateau of the Ethiopian Highlands. The park's Afromontane habitats have one of the highest incidences of animal endemicity of any terrestrial habitat in the world. The park was nominated to the World Heritage Tentative List in 2009. Geography Bale Mountains National Park is located in southeastern Ethiopia, 400 km southeast of Addis Ababa and 150 km east of Shashamene in the Oromia Region National State. The boundary of the BMNP lies within five woredas (districts): Adaba (west), Dinsho (north), Goba (northeast), Delo-Mena-Angetu and Harena-Buluk (southeast). The park area is encompassed within geographical coordinates of 6º29' – 7º10'N and 39º28' – 39º57'E. The Bale Mountains are part of the Bale-Arsi massif, which forms the western section of the southeastern Ethiopian Highlands. Hydrology The Bale Moun ...
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Baro River
The Baro River ( am, ባሮ ወንዝ) or Baro/Openo Wenz, known to the Anuak as Openo River, is a river in southwestern Ethiopia, which defines part of Ethiopian border with South Sudan. From its source in the Ethiopian Highlands it flows west for to join the Pibor River. The Baro-Pibor confluence marks the beginning of the Sobat River, a tributary of the White Nile. The Baro and its tributaries drain a watershed in size. The river's mean annual discharge at its mouth is 241 m³/s (8,510 ft³/s). Course The Baro/Openo 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/Openo include the Alwero and Jikawo Rivers. The Baro meets the Pibor river to the west of Jikawo. During the rainy season the river floods to form the huge inundated area to the east and ...
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Gibe River
The Gibe River (also Great Gibe River) is by far the largest tributary of the Omo River in Ethiopia and typically flowing south-southeast. The confluence of the large Gibe River at with the smaller Wabe River forms the even larger Omo River. Consequently, the whole drainage basin is sometimes called the ''Omo-Gibe River Basin'' with the Gibe and the Omo draining the upper and lower reaches, respectively. Located in southwest Ethiopia, the Gibe River is not navigable, like almost all rivers in the country. Overview The Gibe rises at an elevation of more than 2,000 m north of Bila town and west of the Chomen swamp (specifically, from Gudeya Bila woreda, which is located in the East Welega Zone, Oromia Region). The river is then flowing generally to the southeast to its confluence with the Wabe River. Its tributaries include the Amara, Alanga and Gilgel Gibe rivers. The southern drainage area of the Gibe includes the historic Gibe region, where a number of the former kingdoms o ...
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Genale
Genale is a town founded by Italian colonists in the southeastern Lower Shebelle (Shabeellaha Hoose) region of Italian Somalia. Currently it is called Janaale. History Genale was created in 1924 by a group of settlers from the Italian city of Torino, with the supervision of the Italian governor of the colony. Near the Genale of the colonists and separated by the Shebelle river, soon grew a bigger city populated by Somalis (working as cheap labor force in the plantations): the actual Janaale. After WW2 remained only Janaale, while Genale disappeared when the defeated Italians moved away from Somalia. In 1924 indeed it was started the Italian colonization of the area of Genale, in southern Somalia, forming a group of small and medium-sized farms. Most settlers consisted of old fascist militants of Turin who had followed in this Italian colony the new governor of Somalia, Cesare Maria De Vecchi. The first informal association between farmers, however, arose only in 1928. The main c ...
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Awash River
The Awash (sometimes spelled Awaash; Oromo: ''Awaash'', Amharic: አዋሽ, Afar: ''We'ayot'', Somali: ''Webiga Dir'') 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 kilometres (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 Valley (and especially the Middle Awash) is internationally famous for its high density of hominin fossils, offering unparalleled insight into the early evolution of humans. "Lucy", one of the most famous early hominin fossils, was discovered in the lower Awash Valley. For its paleontological and anthropological importance, the lower valley of the Awash was inscribed on the UN ...
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The Awash River
''The'' () is a grammatical article in English, denoting persons or things already mentioned, under discussion, implied or otherwise presumed familiar to listeners, readers, or speakers. It is the definite article in English. ''The'' is the most frequently used word in the English language; studies and analyses of texts have found it to account for seven percent of all printed English-language words. It is derived from gendered articles in Old English which combined in Middle English and now has a single form used with pronouns of any gender. The word can be used with both singular and plural nouns, and with a noun that starts with any letter. This is different from many other languages, which have different forms of the definite article for different genders or numbers. Pronunciation In most dialects, "the" is pronounced as (with the voiced dental fricative followed by a schwa) when followed by a consonant sound, and as (homophone of pronoun ''thee'') when followed by a v ...
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Great Rift Valley, Ethiopia (2059080512)
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. Description 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 Somali 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 rift is extending in an ESE-WNW direction at about annually. The Ethiopian rift valley is about wide and bordered on both margins by large, discontinuous normal faults that give rise to ...
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Mount Batu
Mount Batu is one of the highest of the Bale Mountains of Ethiopia, as well as of the Oromia Region. Part of the Bale National Park Bale Mountains National Park (BMNP) is a national park in Ethiopia. The park encompasses an area of approximately in the Bale Mountains and Sanetti Plateau of the Ethiopian Highlands. The park's Afromontane habitats have one of the highest inci ..., and located at , it reaches an elevation of 4,307 meters. It consists of two peaks, Tinnish Batu ("Little Batu"), which is actually higher than Tilliq Batu ("Big Batu") to the south. The reason for these deceptive names is explained by Paul Henze, who reports that upon viewing them, "it appeared that the peak behind Tinnish Batu was definitely higher.""Local History in Ethiopia"
The Nordic Africa Institute ...
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Great Rift Valley, Ethiopia
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. Description 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 Somali 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 rift is extending in an ESE-WNW direction at about annually. The Ethiopian rift valley is about wide and bordered on both margins by large, discontinuous normal faults that give rise to ...
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