Essay on theory of plate tectonics

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The Earth's surface is broken into many different sections, called plates. When the plates force a high amount of pressure on each other, its causes earthquakes, volcanoes to erupt, and the formation of mountains. The area where two plates meet is called plate boundaries. Plate tectonics is a combination of two ideas, sea-floor spreading and continental drift. The creation of new oceanic crust at mid-ocean ridges is called sea-floor spreading. In , spreading plate margins became part of the theory of plate tectonics.
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Essay: Tectonic plate boundaries

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Plate Tectonics Essay on

The most reasonable way is the movements of the Earth 's crust. There are also many other plate tectonic related theories and studies that are connected with the earthquakes and volcanoes too. The Theory of the Continental Drift was made by Alfred Wegener and started to be more convincing when people heard about tectonic plates. Plate tectonics, plate tectonics are a theory explaining the structure of the earth and rarely resulting in the interaction of stiff lithospheric plates that move slowly over the lurking mantle below. Plate tectonics has been around for about 3.
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Plate Tectonics

Apple Pay is the easiest and most secure way to pay on Gradesfixer in Safari. The Earth had formed over 4. There are three pieces of evidence that help support the theory of plate tectonics, Shape of Continents, Locations of mountains and fossils, and earthquakes and volcanoes. The plate tectonics theory was started by Alfred Wegener, a brilliant geophysicist and meteorologist.
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Significant Earthquake Throughout its lifespan, earth has experienced some very extreme catastrophes. These disastrous events have the capability to totally alter the landscape as well as change the lives of the inhabitants of the area that they occur in. During this period of time some catastrophes were foreseeable such volcanos erupting, severe thunder and snow storms, however, catastrophes such as earthquake, tsunami and tornado were not predicable. Back in , the technology that we have today was not available; therefore there was no warning or indication when a possible earthquake might occur.
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