Ale Bagu
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Ale Bagu
Ale Bagu is a stratovolcano located in the Afar Region, Ethiopia. It is the highest volcano of Erta Ale Range. The village of El Dom sits at the base of Ale Bagu.Philip Briggs, ''Ethiopia: the Bradt Travel Guide'', fifth edition, updated by Brian Blatt (Chalfont St Peter: Bradt Travel Guides, 2009), p. 314 See also *Afar Depression *Geography of Ethiopia *List of volcanoes in Ethiopia This is a list of volcanoes in Ethiopia. It includes both active and extinct vents. See also * Geography of Ethiopia * Lists of volcanoes References {{Global Volcanism Program Volcanoes Ethiopia Ethiopia, , om, Itiyoophiyaa, so ... References Mountains of Ethiopia Stratovolcanoes of Ethiopia Afar Region {{Afar-geo-stub ...
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Erta Ale
Erta Ale (or Ertale or Irta'ale; Amharic: ኤርታሌ) is a continuously active basaltic shield volcano in the Afar Region of northeastern Ethiopia. It is situated in the Afar Depression, a barren desert area. Erta Ale is the most active volcano in Ethiopia. Geology Erta Ale is high, with one or sometimes two active lava lakes at the summit which occasionally overflow on the south side of the volcano. It is notable for holding the longest-existing lava lake, present since the early years of the twentieth century (1906). Volcanoes with lava lakes are very rare: there are only eight in the world. ''Erta Ale'' means "smoking mountain" in the local Afar language and its southernmost pit is known locally as "the gateway to Hell". In 2009, it was mapped by a team from the BBC using three-dimensional laser techniques, in order for the mapping team to maintain a distance and avoid the lakes' searingly hot temperatures. Erta Ale is centered over the East African Rift system, which is ...
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List Of Volcanoes In Ethiopia
This is a list of volcanoes in Ethiopia. It includes both active and extinct vents. See also * Geography of Ethiopia * Lists of volcanoes References {{Global Volcanism Program Volcanoes Ethiopia Ethiopia, , om, Itiyoophiyaa, so, Itoobiya, ti, ኢትዮጵያ, Ítiyop'iya, aa, Itiyoppiya officially the Federal Democratic Republic of Ethiopia, is a landlocked country in the Horn of Africa. It shares borders with Eritrea to the ... ...
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Afar Depression
The Afar Triangle (also called the Afar Depression) is a geological depression caused by the Afar Triple Junction, which is part of the Great Rift Valley in East Africa. The region has disclosed fossil specimens of the very earliest hominins; that is, the earliest of the human clade, and it is thought by some paleontologists to be the cradle of the evolution of humans. The Depression overlaps the borders of Eritrea, Djibouti and the entire Afar Region of Ethiopia; and it contains the lowest point in Africa, Lake Assal, Djibouti, at below sea level. The Awash River is the main waterflow into the region, but it runs dry during the annual dry season, and ends as a chain of saline lakes. The northern part of the Afar Depression is also known as the Danakil Depression. The lowlands are affected by heat, drought, and minimal air circulation, and contain the hottest places (year-round average temperatures) of anywhere on Earth. The Afar Triangle is bordered as follows (see the topogr ...
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Afar Region
The Afar Region (; aa, Qafar Rakaakayak; am, አፋር ክልል), formerly known as Region 2, is a regional state in northeastern Ethiopia and the homeland of the Afar people. Its capital is the planned city of Semera, which lies on the paved Awash– Assab highway. The Afar Triangle, the northern part of which is the Danakil Depression, is part of the Great Rift Valley of Ethiopia, and is located in the north of the region. It has the lowest point in Ethiopia and one of the lowest in Africa. The southern part of the region consists of the valley of the Awash River, which empties into a string of lakes along the Ethiopian–Djibouti border. Other notable landmarks include the Awash National Park. Demographics Based on the 2017 projections by the Central Statistical Agency of Ethiopia (CSA), the Afar Regional State has a population of 1,812,002, consisting of 991,000 men and 821,002 women; urban inhabitants number 346,000 of the population, a further 1,466,000 were pastora ...
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Ethiopia
Ethiopia, , om, Itiyoophiyaa, so, Itoobiya, ti, ኢትዮጵያ, Ítiyop'iya, aa, Itiyoppiya officially the Federal Democratic Republic of Ethiopia, is a landlocked country in the Horn of Africa. It shares borders with Eritrea to the north, Djibouti to the northeast, Somalia to the east and northeast, Kenya to the south, South Sudan to the west, and Sudan to the northwest. Ethiopia has a total area of . As of 2022, it is home to around 113.5 million inhabitants, making it the 13th-most populous country in the world and the 2nd-most populous in Africa after Nigeria. The national capital and largest city, Addis Ababa, lies several kilometres west of the East African Rift that splits the country into the African and Somali tectonic plates. Anatomically modern humans emerged from modern-day Ethiopia and set out to the Near East and elsewhere in the Middle Paleolithic period. Southwestern Ethiopia has been proposed as a possible homeland of the Afroasiatic langua ...
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Erta Ale Range
Erta Ale Range is the most important axial volcanic chain of the Afar Depression, Afar Region, Ethiopia. It consists mostly of shield volcanoes. The active volcano Erta Ale is a prominent feature of the range. The highest volcano of the range is Ale Bagu, with an elevation of above sea level. Other named peaks (with their elevations) include Alu (), Dalaffilla () and Borale Ale (). Erta Ale This volcano of Erta Ale is the most active in Ethiopia and rises to at its highest point. It is one of many shield volcanoes in the area and is wide with a elliptical summit containing many steep pit craters. Its perpetually active pit craters are renowned for their churning lava lakes. See also *Geography of Ethiopia *List of volcanoes in Ethiopia This is a list of volcanoes in Ethiopia. It includes both active and extinct vents. See also * Geography of Ethiopia * Lists of volcanoes References {{Global Volcanism Program Volcanoes Ethiopia Ethiopia, , om, Iti ...
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Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ...
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Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ...
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Geography 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. Ethiopia has a high central plateau that varies from above sea level, with the highest mountain reaching . Elevation is generally highest just before the point of descent to the Great Rift Valley, which splits the plateau diagonally. A number of rivers cross the plateau; notably the Blue Nile rising from Lake Tana. The plateau gradually slopes to the lowlands of the Sudan on the west and the Somali-inhabited plains to the east. Ethiopia's westernmost locality is Pibor River opposite the Sudanese village of Denjok. Its easternmost locality lies along the eastern border of Dollo Zone opposite Puntland and Galmudug states. Physical features Geography Between the valley of the Upper Nile and Ethiopia's border with Sudan and South Sudan is a region of elevated plateaus from which rise the various tablelan ...
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Mountains Of Ethiopia
The following notable mountains and mountain ranges are completely or partially within the borders of Ethiopia: __NOTOC__ A Mount Abba Yared • Abul Kasim (mountain) • Mount Abuna Yosef • Mount Abuye Meda • Amba Alagi • Ale Bagu • Mount Amara • Amaro Mountains • Mount Ambaricho • Mount Amedamit • Amba Aradam • Mount Assimba • Mount Ayalu B Bale Mountains • Mount Bambasi • Mount Batu • Mount Belaya • Mount Biuat • Borale Ale • Borawli C Mount Chilalo • Mount Choqa • Choqa Mountains D Mount Damota Dangur range • Mount Dara Tiniro • Mount Darkeena • Debre Damo • Mount Delo • Mount Dendi E Entoto Mountains • Mount Entoto • Mount Erer • Erta Ale Range • Ethiopian Highlands F Mount Fentale • Mount Amba Ferit • Mount Fota • Mount Furi G Gada Ale • Mount Gara Muleta • Mount Gardolla • Mount Garochan • Mount Gaysay • Amba Geshen • Mount Gugu • Mount Guna • Mount Gurage H Mo ...
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Stratovolcanoes Of Ethiopia
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volc ...
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