are all the volcanoes found in the same location answers?
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All the volcanoes are not found in the same location. The volcanoes can be seen along the destructive or subducting plate boundaries, constructive or divergent plate boundaries, and at hot spots in the earth's surface. More than half of the active volcanoes in the world above sea level form part of the Ring of Fire.
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Cinder cones are commonly found on the flanks of shield volcanoes, stratovolcanoes, and calderas. For example, geologists have identified nearly 100 cinder cones on the flanks of Mauna Kea, a shield volcano located on the island of Hawaii.
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Although there are no active volcanoes located in the Virgin Islands, the eastern edge of the Caribbean Plate is a subduction zone with seventeen active volcanoes along its boundary. The notable volcanoes are found on Montserrat, Martinique, Guadeloupe and Saint Vincent.
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Hotspot volcanoes are considered to have a fundamentally different origin from island arc volcanoes. The latter form over subduction zones, at converging plate boundaries. ... It is this that fuels a chain of volcanoes, such as the Aleutian Islands, near Alaska.
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Shield volcanoes. Shield volcanoes are found on divergent plate boundaries , where two plates move away from one another. Shield volcanoes have the following characteristics: Basaltic magma, which is high in temperature, very low on silica and with low gas content.
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Most are located around the Pacific Ocean in what is commonly called the Ring of Fire. A volcano is defined as an opening in the Earth's crust through which lava, ash, and gases erupt. The term also includes the cone-shaped landform built by repeated eruptions over time.
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NARRATOR: Scientists believe that 80 percent of the volcanic eruptions on Earth take place in the ocean. ... Nearly 4000 feet below the surface of the Pacific Ocean – in an area between Samoa, Fiji and Tonga - the West Mata volcano was discovered. The explosions of molten rock were spectacular.
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['A volcano is formed by eruptions of lava and ash.', 'Volcanoes are usually cone shaped mountains or hills.', "When magma reaches the Earth's surface it is called lava. ... ", 'Volcanic eruptions can happen at destructive and constructive boundaries , but not at conservative boundaries or collision zones .']
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Some, but not all, earthquakes are related to volcanoes. For example, most earthquakes are along the edges of tectonic plates. ... Most earthquakes directly beneath a volcano are caused by the movement of magma. The magma exerts pressure on the rocks until it cracks the rock.
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['Fissure Volcanoes. ... ', 'Shield Volcanoes. ... ', 'Stratovolcanoes. ... ', 'Cinder Cone. ... ', 'Caldera.']
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No! “Volcanoes are not, in any meaningful sense of the word, alive. Volcanoes are rocky structures formed by the ejection of molten rock through weak spots in the Earth's crust, according to Oregon State University. Apart from some of the gases they expel, they are primarily silicon-based, not carbon-based.”
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Pinatubo, Krakatoa, and Mt. Vesuvius are all famous explosive subduction zone volcanoes. ... The third way that volcanoes form occurs at a hot spot . Hot spots are usually found under oceanic crust , but can be located under continental crust .
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While most volcanoes form along tectonic plate boundaries, mantle plumes and hot spots lead to their development as well. ... Because the hot spot is caused by mantle plumes that exist below the tectonic plates, as the plates move, the hot spot does not, and may create a chain of volcanoes on the Earth's surface.
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Cinder cone volcanoes can form in a few different tectonic settings. Many of them form at convergent plate boundaries, where oceanic crust slips underneath continental crust or other oceanic crust. We call this slip "subduction", and at these boundaries the oceanic crust gets pulled down into the mantle.
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California has active and hazardous volcanoes. Map of moderate, high and very high threat volcanoes monitored by the California Volcano Observatory in California and Nevada. (Public domain.) California is host to all every type of volcano.
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For example, most earthquakes are along the edges of tectonic plates. This is where most volcanoes are too. However, most earthquakes are caused by the interaction of the plates not the movement of magma . Most earthquakes directly beneath a volcano are caused by the movement of magma.
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Some, but not all, earthquakes are related to volcanoes. For example, most earthquakes are along the edges of tectonic plates. This is where most volcanoes are too. However, most earthquakes are caused by the interaction of the plates not the movement of magma .