Try about the progress and history of plate tectonics

Try about the progress and history of plate tectonics

Plate tectonics comes from two words plate and tectonic. Plate in geological conditions usually means a large slab of tricky rock whilst tectonics in Greek implies’ to build’. Therefore’ plate tectonic could be outlined as how the earth’s is designed on moving the plate. It can even be well-defined to be a rigid phase in the Earth’s lithosphere that moves individually from those bordering it (Rodger, 1993). Theory of plate tectonics states which the lithosphere with the earth is produced up of personal plates which are fragmented into various huge and small pieces of strong rock. The plates go subsequent to each other on top of the reduced mantle to build various types of plate borders which have formed the Earth’s landscape above a lot of yrs.(Oreskes & Legrand, 2001). Alfred Wegener, a popular meteorologist, is known to be the founder in the plate tectonic idea; He noticed which the coastline of East South America and that of west coast of Africa seemed to fit together in a jigsaw manner like to form a bigger plate. He then proposed an idea that all plates (continents) were connected to a single significant plate called Pangaea which gradually began to drift apart in excess of 300 million a long time ago (Rodger, 1993). More scientific research over the plates’ coastline revealed that all the plate of earth’s continent somehow fit together. The concept was commonly known as continental drift concept, and Wegener became the founder of the concept on which scientist have based their research on. However, Alfred Wegener plate tectonics principle could not ascertain how exactly the continents drifted away from each other. He proposed the earth’s rotations and the centrifugal forces towards the equator as the mechanism for continental drift. He said that Pangaea started at South Pole and earth’s rotation finally caused it to break up, sending continents toward the equator. His theories were discarded by the scientific community (Rodger, 1993). Arthur Holmes, (1929), a British geologist, came up with the theory of thermal convection to explain the gradual drift of your Earth’s continents. He based on heating and cooling cycle in the Earth’s mantle that caused the continents to go. The idea has been borrowed by scientist community in their quest for earth’s shape. Today scientist have researched and analyzed past evidences and findings by geologist and scientist to expound and come up with a better ways of explaining plate tectonic principle and forces that were behind the drifting from the plates. It is believed and proofed using geological evidence that earth’s plate at one time was one super plate called Pangaea. Due to three main driving forces namely, mantle convection, gravity, and the Earth’s rotation led to the drifting away of several plate from the main one. A number of major plates (continents) were formed which include North America, South America, Eurasia, Africa, Indo-Australian, Pacific, and Antarctica. Expounding about the three main driving forces for the movement with the Earth’s tectonic plates; Mantle convection is the most extensively studied technique of tectonic plate movement. It was widely discussed by Holmes in 1929, in his idea. The significant convection current of molten material in the Earth’s upper mantle produces a lot of energies which is transferred to decreased mantle. The lower mantle material finds their way to the crust causing the embedded rock to shift out and away from the ridge thus moving the plate. Evidence of this is shown at mid-ocean ridges. Gravity is evidenced by the mid-ocean ridges where the elevation is higher than the bordering ocean floor. Convection currents within the Earth cause reduce mantle material to rise and spread away from the ridge, causing the older material to flow toward the ocean floor due to gravity and aid in the movement of your plates. Then lastly earth rotation is caused by centrifugal forces as earth rotates (Oreskes $ Legrand, 2001). Plates form different types of boundary as they interact with their movement. Some of the boundaries formed include Divergent boundaries form when a plate breaks along certain lines of weakness and move college essays writing away from each individual other forming a new crust, for instance, Mid-ocean ridges. The other boundary is called Convergent boundaries and is created when two plates collide with one another causing the sinking of one plate below the other. Transform boundaries forms at location where new crust created and without destroying it. Today, through research, scientists have come up with numerous evidences proving that earth plates were once super plate which split into the current Continents. Some of your evidences include: the jig-saw fitting with the East coast of South America and west coast of Africa appear to fit into one another; Fossils remains of plants and animals collected by scientist around the world showed similarities that were hard to explain unless continents had once been joined. For instance, Cynognathus was a land reptile. Its Fossils remains have been found in both Africa and South America, thus proving the two continents were once joined (Oreskes $ Legrand., 2001). Scientist have also found out from the evidence of earthquakes happened continually and occurred along certain lines, near the boundaries between tectonic plates. As Wegener’s ideas forms the basis why the landscape of the earth is the way it is, scientist community currently advanced methodology of studying the plate tectonic idea. They use satellite to study evidences of plate tectonic where they position it a lot of kilometers away from the earth surface. From the satellite statistics, it is evidenced which the plates shift linearly and away from just about every other at the speed of 10mm to 100mm per year.

References

Oreskes, N., & LeGrand, H. E. (2001). Plate tectonics: An insider’s historical past in the modern principle of the Earth. Boulder, Colo: Westview Press. Rogers, J. J. W. (1993). A record of your earth. New York, NY, USA: Cambridge University Press.

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