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.
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. Then the magma squirts into the crack and starts building pressure again. Every time the rock cracks it makes a small earthquake. These earthquakes are usually too weak to be felt but can be detected and recorded by sensitive instruments. Once the plumbing system of the volcano is open and magma is flowing through it, constant earthquake waves, called harmonic tremor, are recorded (but not felt).
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.
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. Then the magma squirts into the crack and starts building pressure again. Every time the rock cracks it makes a small earthquake. These earthquakes are usually too weak to be felt but can be detected and recorded by sensitive instruments. Once the plumbing system of the volcano is open and magma is flowing through it, constant earthquake waves, called harmonic tremor, are recorded (but not felt).
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.
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. Then the magma squirts into the crack and starts building pressure again. Every time the rock cracks it makes a small earthquake. These earthquakes are usually too weak to be felt but can be detected and recorded by sensitive instruments. Once the plumbing system of the volcano is open and magma is flowing through it, constant earthquake waves, called harmonic tremor, are recorded (but not felt).
Volcanoes and earthquakes are seemingly very different geological events, yet they are actually closely related - both result from movements of Earth's crust.
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.
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. Then the magma squirts into the crack and starts building pressure again. Every time the rock cracks it makes a small earthquake. These earthquakes are usually too weak to be felt but can be detected and recorded by sensitive instruments. Once the plumbing system of the volcano is open and magma is flowing through it, constant earthquake waves, called harmonic tremor, are recorded (but not felt).
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.
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. Then the magma squirts into the crack and starts building pressure again. Every time the rock cracks it makes a small earthquake. These earthquakes are usually too weak to be felt but can be detected and recorded by sensitive instruments. Once the plumbing system of the volcano is open and magma is flowing through it, constant earthquake waves, called harmonic tremor, are recorded (but not felt).
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.
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. Then the magma squirts into the crack and starts building pressure again. Every time the rock cracks it makes a small earthquake. These earthquakes are usually too weak to be felt but can be detected and recorded by sensitive instruments. Once the plumbing system of the volcano is open and magma is flowing through it, constant earthquake waves, called harmonic tremor, are recorded (but not felt).
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.
Volcanoes and earthquakes are seemingly very different geological events, yet they are actually closely related - both result from movements of Earth's crust. Earth's crust - the lithosphere - is composed of several major plates and many minor plates that change shape and position. Over time, these tectonic plates move, interact with each other, and are responsible for the formation of ocean basins, mountain ranges, islands, volcanoes, and earthquakes.
Volcanoes and earthquakes are seemingly very different geological events, yet they are actually closely related - both result from movements of Earth's crust.
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.
Volcanoes shake and spew out lava. Earthquakes shake and bring down buildings. Both volcanoes and earthquakes change the atmosphere around them in sometimes fatal ways.
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.
ReplyDeleteMost earthquakes directly beneath a volcano are caused by the movement of magma. The magma exerts pressure on the rocks until it cracks the rock. Then the magma squirts into the crack and starts building pressure again. Every time the rock cracks it makes a small earthquake. These earthquakes are usually too weak to be felt but can be detected and recorded by sensitive instruments. Once the plumbing system of the volcano is open and magma is flowing through it, constant earthquake waves, called harmonic tremor, are recorded (but not felt).
http://volcano.oregonstate.edu/how-are-volcanoes-and-earthquakes-related
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.
ReplyDeleteMost earthquakes directly beneath a volcano are caused by the movement of magma. The magma exerts pressure on the rocks until it cracks the rock. Then the magma squirts into the crack and starts building pressure again. Every time the rock cracks it makes a small earthquake. These earthquakes are usually too weak to be felt but can be detected and recorded by sensitive instruments. Once the plumbing system of the volcano is open and magma is flowing through it, constant earthquake waves, called harmonic tremor, are recorded (but not felt).
http://volcano.oregonstate.edu/how-are-volcanoes-and-earthquakes-related
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.
ReplyDeleteMost earthquakes directly beneath a volcano are caused by the movement of magma. The magma exerts pressure on the rocks until it cracks the rock. Then the magma squirts into the crack and starts building pressure again. Every time the rock cracks it makes a small earthquake. These earthquakes are usually too weak to be felt but can be detected and recorded by sensitive instruments. Once the plumbing system of the volcano is open and magma is flowing through it, constant earthquake waves, called harmonic tremor, are recorded (but not felt).
Volcanoes and earthquakes are seemingly very different geological events, yet they are actually closely related - both result from movements of Earth's crust.
ReplyDeletethey both involve shaking the earth
ReplyDeleteSome, 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.
ReplyDeleteMost earthquakes directly beneath a volcano are caused by the movement of magma. The magma exerts pressure on the rocks until it cracks the rock. Then the magma squirts into the crack and starts building pressure again. Every time the rock cracks it makes a small earthquake. These earthquakes are usually too weak to be felt but can be detected and recorded by sensitive instruments. Once the plumbing system of the volcano is open and magma is flowing through it, constant earthquake waves, called harmonic tremor, are recorded (but not felt).
http://volcano.oregonstate.edu/how-are-volcanoes-and-earthquakes-related
Earthquakes are like volcanos because they're both destructive. (Most of the time)
ReplyDeleteSome, 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.
ReplyDeleteMost earthquakes directly beneath a volcano are caused by the movement of magma. The magma exerts pressure on the rocks until it cracks the rock. Then the magma squirts into the crack and starts building pressure again. Every time the rock cracks it makes a small earthquake. These earthquakes are usually too weak to be felt but can be detected and recorded by sensitive instruments. Once the plumbing system of the volcano is open and magma is flowing through it, constant earthquake waves, called harmonic tremor, are recorded (but not felt).
http://volcano.oregonstate.edu/how-are-volcanoes-and-earthquakes-related
Volcanos and earthquakes are alike because they occur in the same area and they are both are natural distaters
ReplyDeleteEarthquakes are like volcanoes because they both destroy anything in its path.
ReplyDeleteThey are both somewhat alike because they both have the power to cause mass destruction.
ReplyDeleteBoth shake the earth.
ReplyDeletehttp://volcano.oregonstate.edu/how-are-volcanoes-and-earthquakes-related
ReplyDeleteVolcanos and Earthquakes are both alike by where they take place and how destructive they both are.
ReplyDeleteEarthquakes are like volcanoes because they both damage the Earth.
ReplyDeleteaustine dasiy snell
ReplyDeletehi
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ReplyDeleteEarthquakes can be like volcanoes because they can both destroy Earth's surface.
ReplyDeleteSome, 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.
ReplyDeleteMost earthquakes directly beneath a volcano are caused by the movement of magma. The magma exerts pressure on the rocks until it cracks the rock. Then the magma squirts into the crack and starts building pressure again. Every time the rock cracks it makes a small earthquake. These earthquakes are usually too weak to be felt but can be detected and recorded by sensitive instruments. Once the plumbing system of the volcano is open and magma is flowing through it, constant earthquake waves, called harmonic tremor, are recorded (but not felt).
I forgot my source
Deletehttp://volcano.oregonstate.edu/how-are-volcanoes-and-earthquakes-related this is the site she got it form mr ruby...
DeleteThey both shake the ground and make loud noises when they happen.
ReplyDeletethey both do damage so they are like the same
ReplyDeleteSome earthquakes occur along the earth's tectonic plates, then, sometimes, volcanoes are made along tectonic plates.
ReplyDeleteThey both have to do with rocks and make loud noises.
ReplyDeleteVolcanoes and Earthquakes are similar because they both have an affect on the Earth.
ReplyDeleteEarthquakes and volcanoes are alike because they both cause damage.
ReplyDeleteEarthquakes and volcanoes are similar, because they both involve plates in the earth.
ReplyDeleteThey both are involved in the plates under the earth and they cause great destruction.
ReplyDeleteNNOAH L Earthquakes are like volcanoes because they both damage the Earth.
ReplyDeletethey both explode.
ReplyDeleteEarthquakes and volcanoes are similar, because they both involve plates in the earth and rocks.
ReplyDeleteSome, 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.
ReplyDeleteVolcanoes and earthquakes are seemingly very different geological events, yet they are actually closely related - both result from movements of Earth's crust. Earth's crust - the lithosphere - is composed of several major plates and many minor plates that change shape and position. Over time, these tectonic plates move, interact with each other, and are responsible for the formation of ocean basins, mountain ranges, islands, volcanoes, and earthquakes.
ReplyDeleteSource: Wiki Answers
they both happen when earths plates move
ReplyDeleteThey both shake the earth around it breaking things in there way.
ReplyDeletethey both are formed from earth
ReplyDeleteVolcanoes and earthquakes are seemingly very different geological events, yet they are actually closely related - both result from movements of Earth's crust.
ReplyDeleteEarthquakes and volcanos are similar because they are both started under ground. Magma builds up under the ground and plates shift under the ground.
ReplyDeleteVolcanos and Earthquakes are both alike by where they take place and how destructive they both are.
ReplyDeleteSome, 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.
ReplyDeleteVolcanoes shake and spew out lava. Earthquakes shake and bring down buildings. Both volcanoes and earthquakes change the atmosphere around them in sometimes fatal ways.
ReplyDeleteEarthquakes and volcanoes are similar because they both cause damage to the surface of earth.
ReplyDelete