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Jalua Volcano
The Jalua Volcano is a volcano located in the Northern Red Sea region of Eritrea. It is a stratovolcano, with no eruption ever recorded. See also *List of volcanoes in Eritrea *List of stratovolcanoes A list of stratovolcanoes follows below. Africa Cameroon * Mount Cameroon Democratic Republic of Congo * Mount Nyiragongo, Goma; designated as a Decade Volcano ** It contains an active lava lake inside its crater which overflowed due t ... References Mountains of Eritrea Stratovolcanoes of Eritrea Rift volcanoes {{Eritrea-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eritrea
Eritrea ( ; ti, ኤርትራ, Ertra, ; ar, إرتريا, ʾIritriyā), officially the State of Eritrea, is a country in the Horn of Africa region of Eastern Africa, with its capital and largest city at Asmara. It is bordered by Ethiopia in the south, Sudan in the west, and Djibouti in the southeast. The northeastern and eastern parts of Eritrea have an extensive coastline along the Red Sea. The nation has a total area of approximately , and includes the Dahlak Archipelago and several of the Hanish Islands. Human remains found in Eritrea have been dated to 1 million years old and anthropological research indicates that the area may contain significant records related to the evolution of humans. Contemporary Eritrea is a multi-ethnic country with nine recognised ethnic groups. Nine different languages are spoken by the nine recognised ethnic groups, the most widely spoken language being Tigrinya, the others being Tigre, Saho, Kunama, Nara, Afar, Beja, Bilen and Ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcano
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Red Sea Region
The Northern Red Sea Region (, it, Regione del Mar Rosso Settentrionale, ) is an administrative region of Eritrea. It lies along the northern three quarters of the Red Sea, and includes the Dahlak Archipelago and the coastal city of Massawa. As of 2005, the region had a population of 653,300 compared to a population of 576,200 in 2001. The net growth rate was 11.80 per cent. The total area of the province was 27800.00 km2 and the density was 23.50 persons per km2. Geography The Northern Red Sea Region borders the Anseba, Maekel (Central) and Debub (Southern) regions to the west, and the Southern Red Sea Region to the east. It has an area of around 27,800 km². The lowest point in Eritrea, Lake Kulul, is in this region. The topography of the region has coastal plains, which are hotter than the regions around the highland plateau. There are two rainy seasons, the heavier one during summer and the lighter one during spring. The climate and geography of the region al ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Regions Of Eritrea
The regions of Eritrea are the primary geographical divisions through which Eritrea is administered. Six in total, they include the Central, Anseba, Gash-Barka, Southern, Northern Red Sea and Southern Red Sea regions. At the time of independence in 1993 Eritrea was arranged into ten provinces. These provinces were similar to the nine provinces operating during the colonial period. In 1996, these were consolidated into six regions (''zobas''). Gash-Barka Region was the largest and the most densely populated region and is called the "bread-basket". The People's Front for Democracy and Justice or PFDJ (originally Eritrean People's Liberation Front) rules the country and its regions as a single-party totalitarian government. The regional and local elections are conducted on a periodic basis on a restricted framework. All men and women of any ethnic or religious background are eligible to vote. No parties or groups other than PFDJ are allowed to contest and the elections are presid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Volcanoes In Eritrea ...
This is a list of active and extinct volcanoes in Eritrea. References {{Global Volcanism Program Eritrea Volcanoes A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Stratovolcanoes
A list of stratovolcanoes follows below. Africa Cameroon * Mount Cameroon Democratic Republic of Congo * Mount Nyiragongo, Goma; designated as a Decade Volcano ** It contains an active lava lake inside its crater which overflowed due to cracks in 2002. * Mount Mikeno Eritrea * Alid Volcano * Dubbi Volcano * Nabro Volcano Ethiopia * Adwa * Borawli, Afar Region * Dabbahu Volcano * Mount Fentale * Mount Bryan Kenya * Mount Kenya, which contains several volcanic plugs on its peak. * Mount Longonot Rwanda * Mount Bisoke, on the border between Rwanda and the Democratic Republic of the Congo. * Mount Gahinga, on the border between Rwanda and Uganda. * Mount Karisimbi, on the border between Rwanda and the Democratic Republic of the Congo. * Mount Muhabura, on the border between Rwanda and Uganda. * Mount Sabyinyo, marks the border between Rwanda, Uganda, and the Democratic Republic of the Congo. Tanzania * Ol Doinyo Lengai, the Earth's only active carbonati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Eritrea
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratovolcanoes Of Eritrea
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 volcanoes. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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