Bara Ale
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Bara Ale
Asavyo also known as Bara Ale is a large silicic stratovolcano in Ethiopia, which forms part of the Bidu Volcanic complex. It lies about 20 km southwest from the Nabro and Mallahle volcanoes. Asavyo has a 12 km wide caldera A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is .... References {{Volcano-stub Mountains of Ethiopia Stratovolcanoes of Ethiopia Calderas of Ethiopia ...
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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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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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Bidu Volcanic Complex
BIDU or Bidu may refer to: Places * Bidu, Dashtestan, Bushehr, Iran * Bidu, Deylam, Bushehr, Iran * Bidu, Jam, Bushehr, Iran * Bidu, Anarestan, Jam, Bushehr, Iran * Bidu, Shahr-e Babak, Kerman, Iran * Bidu, Yazd, Iran * Bidu (woreda), Ethiopia Other uses * Bidu (god), gatekeeper of the underworld in Mesopotamian mythology * Bidu Cola, Argentinian cola soft drink, also marketed in other countries, including Curaçao (Netherlands Antilles) * Bidu Sayão (1902–1999), Brazilian opera soprano * BIDU, the NASDAQ ticker symbol for Baidu * Blu (Monica's Gang) ''Blu'' (''Bidu'') is a character in the Brazilian comic strip ''Monica's Gang'', created in 1959. He was the first character created by Maurício de Sousa, along with his owner Franklin (''Franjinha''). The character appears in the logo and is t ... (known as Bidu in Brazil), a character in ''Monica's Gang'' media * Matheus Lima Beltrão Oliveira, Brazilian footballer See also * Biddu Appaiah (born 1944), Anglo-Indian music ...
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Nabro Volcano
The Nabro Volcano is an active stratovolcano in the Southern Red Sea Region of Eritrea. It is located at the south-east end of the Danakil Alps in the Danakil Depression. Before its 2011 eruption, the volcano was widely believed to be extinct. Geology Part of the Afar Triangle, the Nabro Volcano is one of many volcanic caldera complexes in the northeasternmost part of the East African Rift valley region. The twin calderas likely formed during an eruption of about 20 to 100 cubic kilometres consisting of ignimbrite, although the date of their formation is unknown. The subaerial volume of volcanic material within the Nabro Volcanic Range is likely on the order of . 2011 eruption Although it had undergone no historically reported eruptions,"Eruption at Nabro Volcano, Eritrea"
NASA Earth ...
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Mallahle
Mallahle (also Mallali or Aruku) is a stratovolcano on the border of Ethiopia and Eritrea, with a 6 km wide caldera. Mallahle is the highest peak in the Afdera region of Ethiopia. It is located in the Danakil Horst at the southern end of the Danakil Alps. It makes up part of the Bidu volcanic complex (with the Nabro Volcano The Nabro Volcano is an active stratovolcano in the Southern Red Sea Region of Eritrea. It is located at the south-east end of the Danakil Alps in the Danakil Depression. Before its 2011 eruption, the volcano was widely believed to be extinct. G ..., Bara Ale and Sork Ale). References Stratovolcanoes of Ethiopia Calderas of Ethiopia Calderas of Eritrea {{Ethiopia-geo-stub ...
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Caldera
A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface (from one to dozens of kilometers in diameter). Although sometimes described as a Volcanic crater, crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018. Etymology The term ''caldera'' comes from Spanish language, S ...
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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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