Plate Tectonics
A. The theory of plate tectonics states that the outer layer of the Earth is divided into several sections or plates that slide over the Earth’s mantle, the rocky layer surrounding the core. As compared to the Earth’s mantle, the plates are hard and unyielding and constitute the lithosphere. A modern version of the continental drift, the theory of Plate Tectonics was first put forward by scientist Alfred Wegener in 1912. Though at the time Wegener had no rationalization about the movements of continents, researchers today do. Nicholas Van der Elst, a seismologist at Columbia University’s Lamont-Doherty Earth Observatory in Palisades, New York, says that plate tectonics is a unifying theory of geology.
B. The plate tectonic theory, in essence, says that the plates glide across over the Earth’s mantle interacting at their boundaries as they move. Using information and clues from rocks and fossils, geoscientists can demonstrate the development of the earth’s continents. It is believed by most researchers that plate tectonic movements began about 3 billion years ago, as seen from ancient magma and minerals that have been preserved in rocks from that period. “We don’t really know when plate tectonics as it looks today got started, but we do know that we have a continental crust that was likely scraped off a downgoing slab (a tectonic plate in subduction zone) that is 3.8 billion years old,” said Van der Elst. “We could guess that plate tectonics was operating, but it might have looked very different from today.”
C. Supercontinents are giant landmasses that come together occasionally when continents move. Rodinia is one of the earliest supercontinents to have taken shape around 1 billion years ago. By the Snowball Earth theory, extreme cooling of the earth occurred at least once around 600-700 million years ago. The breakup of the supercontinent is believed to have triggered extreme cooling. There are a few major plates and around a dozen minor plates. The major plates such as the North American, the African and the Antarctic plates are named after the continents embedded in them. Though smaller in size, minor plates are just as important in shaping the earth. The tiny Juan de Fuca plate accounts for most of the volcanic activity around the Pacific Northwest of the United States.
D. Three types of tectonic boundaries are created by the movement of the plates. Convergent refers to the movement of the plates into one another resulting in a collision between continents. When plates move apart, it is called divergent, and plate movement sideways in relation to each other is called a transform boundary. The movement is not noticeable as it measures only around one to two inches per year. Mountain ranges are formed due to the collision of landmasses where the crust buckles. Fifty-five million years ago, India and Eurasia collided, resulting in the formation of the Himalaya. The mountains get higher due to constant pressure and buckling. Mt Everest, which is the highest mountain in the world, may become just a little bit taller in the future. Usually, one plate dives beneath another in ocean-ocean convergences, forming deep trenches. The Mariana Trench, the deepest point on earth, situated in the North Pacific Ocean, is a good example. These types of collisions result in underwater volcanoes that ultimately develop into islands such as Japan.
E. In a report published in Nature Magazine, a team of Australian and American scientists asserts, however, that plate tectonics was not required in ancient times to form rocks much like the ones associated with the tectonic processes of today. “The issue of when the process began is highly debatable, but many geophysicists believe that about 3.0 to 2.8 billion years ago, the Earth went through a prolonged period in which its crust was a single solid shell, punctuated here and there by volcanoes, but without today’s moving plates,” says Michael Brown, applied metamorphic petrologist at the University of Maryland, College Park, Maryland. Undoubtedly, further research into plate tectonics is necessary to throw light on the subject.