The development and history of plate tectonics

Plate tectonics comes from two terms; plate and tectonic. Plate in geological phrases means that a large slab of tricky rock even as tectonics in Greek implies’ to build’. Therefore’ plate tectonic may very well be outlined as how the earth’s builds on shifting the plate. It could actually even be well-defined like a segment of the Earth’s lithosphere that is certainly rigid moves distinctively from all those bordering it (Rodger, 1993).

Theory of plate tectonics states the lithosphere on the earth is designed up of individual plates that fragmented into a number of sizeable and smaller pieces of good rock. The plates shift following to each other in addition to the decreased mantle to produce diverse sorts of plate borders which have shaped the Earth’s landscape greater than quite a few yrs. (Oreske & Legrand, 2001).

Alfred Wegener, a populous meteorologist, is known to be the founder from the plate tectonic theory. He noticed which the coastline of East South America and that of your 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) connected to a single considerable plate called Pangaea which gradually began to drift apart around 300 million several years ago (Rodger, 1993).

More scientific research on the plates’ coastline revealed that all the plate of earth’s continent somehow fit together. The principle, commonly known as continental drift principle, and Wegener became the founder from the theory on which scientist have based on their research.he said

However, Alfred Wegener plate tectonics concept could not ascertain how exactly the continents drifted away from each and every other. He proposed the earth’s rotations and the centrifugal forces towards the equator as one belonging to the possible 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 within the Earth’s continents. He based on heating and cooling cycle within the Earth’s mantle that caused the continents to go. The Wegner’s idea being borrowed by scientist community in their quest for earth’s shape.

Today scientist have researched and analyzed past parts of evidence and findings by geologist and scientist to expound and come up with a better ways of explaining plate tectonic concept and forces that were behind the drifting on the plates. It is believed and proofed using geological evidence that earth’s plate at one time was one big supercontinent called Pangaea. Due to three main driving forces namely, mantle convection, gravity, and the Earth’s rotation led to the drifting away within the numerous plate from the main one. A variety of major plates (continents) formed which include North America, South America, Eurasia, Africa, Indo-Australian, Pacific, and Antarctica.

Expounding on the three main driving forces for the movement belonging to 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 colossal convection current of molten material in the Earth’s upper mantle produces a lot of energies which is transferred to decrease mantle. The reduced mantle material finds their way to the crust causing the embedded rock to transfer away and out from the ridge thus transferring the plate. Evident of this is present in mid-ocean ridges.

Gravity evidenced by the mid-ocean ridges where the elevation is higher than the bordering ocean floor. Convection currents within the Earth cause decrease 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 within the plates. Then lastly earth rotation is caused by centrifugal forces as the earth rotates (Oreskes $ Legrand, 2001).

Plates design different forms for the boundaries as they interact with their movement. Some belonging to the boundaries established include the Divergent boundaries form when a plate breaks along certain lines of weakness and shift away from each and every other forming a new crust, for instance, Mid-ocean ridges. The other boundary is called Convergent boundaries and created when two plates collide with one another causing the sinking of one plate below the other. Transform boundaries forms at the location where new crust created and without destroying it.

Today, through research, scientists have come up with shreds of evidence proving that earth plates were once super plate that split into the current Continent. One for the evidence is the jig-saw fitting for the East coast of South America, west coast of Africa appear to fit into one another. Also, Fossils remains of plants and animals collected by scientist around the world showed similarities that were cumbersome to explain unless continents had once joined. For instance, Cynognathus was a land reptile; its Fossils remain present both Africa and South America. Thus proving that the two continents joined as one, millions of many years ago, (Oreskes $ Legrand, 2001). Scientists 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 form the basis why the landscape belonging to the earth is the way it is, scientist community has advanced the methodology of studying the plate tectonic principle currently. They use the satellite to study evidences of plate tectonic where they position it scores of kilometers away from the earth surface. From the satellite statistics, it is evidenced which the plates transfer linearly and away from just about every other at the speed of 10mm to 100mm per year. Thus proving that plate tectonic concept that may be earth was once one plate that gradually drifted apart over millions of a long time back to form the current continents.