Plate tectonics is a sub domain of geography that explains the motion of the surface of the earth. Basically, it is the theory which is based on the concept of continental drift. The lithosphere, which is the outermost shell of the Earth, is divided unevenly into land masses, known as tectonic plates. These plates are composed of the lithosphere, both at the continent and ocean, each topped by its own kind of crust. They vary in size and composition, depending on the composition of the earth’s crust. When two of such plates meet, collide or divulge from one another, it leads to tremors in the earth’s surface. Plate tectonics tend to bring some severe activities such as earthquakes, volcanoes, mountain buildings, the creation of oceanic trench, etc.
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Students pursuing the geology and geography course are often assigned with the assignments from several aspects of plate tectonics which creates a lot of difficulties for them. The topic of plate tectonics is not an easy task as it requires a professional approach as students are still in the learning phase and thus they are not proficient enough in acquiring a deeper understanding of the topic. Moreover, the theory of plate tectonics is provided in geology and geography; it may confuse the student’s mind as they don’t know which domain to look for the exact information. The topic of plate tectonics is vast and requires an extensive research of its concepts, thus it creates a difficulty for the students as they confined their research to the textbooks only. There are many other important topics in plate tectonics like ocean basins, earthquakes, volcanism, rift basins, and much more. Getting information on the topics is a really time-consuming task as they are also involved in some other courses too.
There are three types of plate tectonics boundaries mentioned below:
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