Volcanoes are a result of the Earth trying to lose its internal heat. If the Earth's interior was cold, there would be no volcanoes. So how does a volcano form hey.
Well, deep inside Earth, between the molten iron core and the thin crust at the surface, there is the mantle, a large layer of rock that is largely solid, but flows like plastic. When, for various reasons, rock from the mantle melts, it sometimes moves to the Earth’s surface through weak spots in the crust, releasing heat, gasses, and rock, what do you get when you put all this together..... you got it, a volcanic eruption.
Volcanoes erupt because magma is less dense than the solid rocks surrounding it in the mantle of the earth. As it nears the surface, gases expand and boil out of the rock, and this force of explosion propels lava from the vent.
Volcanoes can occur by themselves or in belts and chains. The location of these volcanoes splits them into three groups. Rift volcanoes, subduction volcanoes, and hot spot volcanoes. This has a lot to do with plate tectonics, or moving of the segments of the earth's lithosphere.
· Rift volcanoes occur where the plates are moving away from each other. They fill the separations with lava flows, creating new sea floor and mountain ridges beneath the waves.
· Subduction volcanoes form where the plates collide and slide over each other. They create ridges and peaks. The Ring of Fire is a famous chain of volcanoes that rim the Pacific Ocean. About 1,000 live subduction volcanoes occur in this ring, and in any one-year, approximately 40 will be in some state of eruption. The Ring of Fire is composed of stratovolcanoes, which normally occur in chains, and account for over 95% of the world's active volcanoes.
Hot spot volcanoes are the exception to the rule of volcanoes occurring along plate margins. There are constant zones of magma within the earth in some places beneath the plates. The magma pierces through the plate. As time passes and the plates move, new volcanoes appear, and the extinct volcanoes are carried away with the drift of the plates. The common forms of hot spot volcanoes are shield volcanoes, like Mauna Loa of the Hawaiian Islands.
Many factors determine the location, appearance, and amount of activity of each volcano. The location and consistency of magma determine the type of explosion, which determine the type of volcano that is formed.
Volcanoes are both facinating and deadly examples of natures power. They are natural wonders that should be not just appreciated, but studied aswell.
Sorry this is long its just I studied volcanoes at uni and just find them fascinating.
2006-11-26 21:03:32
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answer #1
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answered by Pete 2
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There are four answer for it.
1.A volcano is formed when plates hit each other. One of the plates goes under the other. This is where the earth heats and melts the rock into magma and gases. This can happen as deep as 100 miles below the earth. Magma settles in pools or chambers near the surface. This is where eruptions take place.
2.Volcanoes can also be formed when the plates go away from each other. The magma pushes up and lava forms. These types of volcanoes are found on the ocean floor.
3.A volcano forms when hot molten rock (called magma while it's still underground) erupts at the surface. Molten rock on the surface is called lava and it will build up around the vent where it comes out, forming a volcano. There is also almost always a lot of gas within the magma. When it gets to the surface it expands rapidly and sometimes explosively (like releasing the pressure on a soda). This produces pyroclastic material (material that is thrown into the air from the vent). Pyroclastic material can be fine or coarse, but either way it will also pile up around the vent, helping to build the volcano. Most volcanoes, therefore are composed of layers of lava and pyroclastic material. Some are more of one or the other, and some are about even.
4.Volcanoes are formed when magma from within the Earth's upper mantle works its way to the surface. At the surface it erupts to form lava flows and ash deposits. Ash deposits result from more explosive activity and lava flows usually are associated with quieter activity. Anyway, once you have piled up lava and/or ash around the vent, you have a young volcano. After many many more eruptions you have a big volcano that is constructed of the ash and lava products of these eruptions.
2006-11-26 23:03:23
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answer #2
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answered by aaki 2
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A volcano is an opening (or rupture) in the Earth's surface or crust, which allows hot, usually molten rock, ash, and gases to escape from deep below the surface. Volcanic activity involving the extrusion of rock tends to form mountains or features like mountains over a period of time.
Volcanoes are generally found where two to three tectonic plates pull apart or are coming together. A mid-oceanic ridge, like the Mid-Atlantic Ridge, has examples of volcanoes caused by "divergent tectonic plates" pulling apart; the Pacific Ring of Fire has examples of volcanoes caused by "convergent tectonic plates" coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another (like the San Andreas fault). Volcanoes can also form where there is stretching of the Earth's crust and where the crust grows thin (called "non-hotspot intraplate volcanism"), such as in the African Rift Valley or the European Rhine Graben with its Eifel volcanoes).
Finally, volcanoes can be caused by "mantle plumes," so-called "hotspots;" these hotspots can occur far from plate boundaries, such as the Hawaiian Islands. Interestingly, hotspot volcanoes are also found elsewhere in the solar system, especially on rocky planets and moons.
2006-11-26 21:40:02
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answer #3
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answered by Anonymous
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Volcanoes are generally found where two to three tectonic plates pull apart or are coming together. A mid-oceanic ridge, like the Mid-Atlantic Ridge, has examples of volcanoes caused by "divergent tectonic plates" pulling apart; the Pacific Ring of Fire has examples of volcanoes caused by "convergent tectonic plates" coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another (like the San Andreas fault). Volcanoes can also form where there is stretching of the Earth's crust and where the crust grows thin (called "non-hotspot intraplate volcanism"), such as in the African Rift Valley or the European Rhine Graben with its Eifel volcanoes).
Finally, volcanoes can be caused by "mantle plumes," so-called "hotspots;" these hotspots can occur far from plate boundaries, such as the Hawaiian Islands. Interestingly, hotspot volcanoes are also found elsewhere in the solar system, especially on rocky planets and moons.
You could get more information from the link below...
2006-11-26 21:28:49
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answer #4
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answered by catzpaw 6
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Like mountains, volcanoes form when plates collide. Sometimes, one plate pushes over the top of another plate. As the bottom plate slides downward into the mantle, it begins to melt. There is a great deal of pressure in the mantle. A volcano is a kind of giant safety valve that releases pressure. A volcano erupts when melted, or molten, rock pushes up through cracks in the crust. After the molten rock, or magma, hardens it just keeps on building up until it forms a huge mountain which is then a volcano.
2016-05-23 08:36:08
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answer #5
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answered by Anonymous
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A volcano is formed by pressure building up below the Earth’s crust. Magma forces it way through weaknesses in the earth's crust. When the magma emerges it is called lava. When it cools, it solidifies into rock,or it may emerge though thin cracks,which are called fissure.Or it may be forced though wider pipes,that starts to build up, to a volcano.
2006-11-26 20:16:11
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answer #6
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answered by Anonymous
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The gravity was weak in the early days so when rocks and lava flowed from the ground they tended to form cone shapes with open tops witch started a flow of lava inside of them.
2006-11-26 20:17:30
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answer #7
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answered by D H 1
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Umm...A a turd is a turd ok. bye.
2016-02-16 10:29:58
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answer #8
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answered by rherum 3
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