Continental Drift and Plate Tectonics Essay

Introduction The Beginning of the Continental grade possible action In the middle of the eighteenth century, James Hutton proposed a possibleness, uniformitarianism the present is the key to the late(prenominal). It held that processes much(prenominal) as geologic forces- gradual and catastrophic-occurring in the present were the resembling that op eonted in the past. (Matt Rosenberg, 2004) This possibleness coincides with the theory of Continental Drift that was first proposed by Abraham Ortelius in December 1596, who suggested that North, S come forthh the States, Africa and Eurasia were once connected but had been bust a straggle by footingquakes and floods.He also disc all overed that the coasts of the eastern part of South America and the western coasts of Africa fit together like a jigsaw puzzle and this fit becomes especi altogethery prominent as the edges of the Continental shelves switch similar shapes and thus, appear to be once fitted together. (Figure 1.1 and Figure 1.2) The likeness of southern continents geological formations had led Roberto Mantovani to speculate that all continents had once been a supercontinent and was little in its volume than it is immediately. Through volcanic act, fissures be created in the pertness create this continent to break apart. However, this theory, cognize as the Expanding solid ground Theory has since been turn up incorrect.The Theory of Continental DriftIn 1912, The Theory of Continental Drift was intensively developed by Alfred Wegener, who claimed that the world was make up of a single gigantic supercontinent named Pangea since the Permian period, 250 million darkened age ago. It began forming at the mystifyning of the Carboniferous period, 365 million years ago, when Gondwana collided into Laurussia producing the Appalachian mountain pat in eastern North America and closing in Paleo-Tethys naval and modern landmass became exposed to air. Alexander Du Toit then suggested that 145-2 00 million years ago, in the middle Jurassic Period, Pangea started breaking up into two eleganter supercontinents, Laurasia in the northern hemisphere and Gondwana in the southern hemisphere, with Tethys ocean and North Atlantic naval separating the two supercontinents.The late Jurassic era began the formation of the Rocky Mountains and Sierra Nevada mountains. In the Cretaceous Period, 65 million years ago, the two supercontinents then began fragmenting into the present seven continents. (USGS, 2012) The Tethys ocean that lay between the two landmasses was subducted beneath Eurasia, forming the lower Atlantic Ocean. Eventually, it disappe bed. (Nelson Thomas, 2007) (Figure 2) Wegener proposed that continents were go at about one yard per century and supported this theory with several points of evidence.Evidence supporting the Theory of Continental Drift (Alfred Wegener and Du Toit) Alfred Wegener matched up coastlines, and he realized that by fitting the continental shelves tog ether, cratons form a contiguous pattern across the boundary of South America and Africa. (Lois caravan Wagner, 2013) He realized that mountain ranges that ended at one coastline seemed to begin again on an opposite much(prenominal)(prenominal) as ancient mountains in South Africa that align with the mountains in near Buenos Aires in Argentina. (Sant, Joseph, 2012) He discovered earthworms of the family Megascolecina, who are unlikely to be long-distance migrators, were instal in soils of all the Gondwanaland continents. (kangarooistan, 2009) This identical species could not have a fancy upn on different continents without some variations. (WiseGeek, 2010) dodo remains of a prehistoric reptile known as the Mesosaurus had been exposed on both(prenominal) sides of the South Atlantic coasts, hitherto the creature was otiose to swim across the Atlantic Ocean. (Lois Van Wagner, 2013) Fossils of the land reptile, Lystrosaurus were discovered in South America, Africa and Antarctic a. (Sant, Joseph, 2012).He also discovered the fossil plant Glossopteris was distributed end-to-end India, South America, Southern Africa, Australia and Antarctica. (USGS, 2012)(Figure 3) Alexander Du Toit traveled to Brazil and Argentina where he found similarities in the fossils and jar strata to those found in South Africa such as the fossilized remains of Mesosaurus in fresh water deposits, sand dune deposits capped by basalt flows, tillite and coal beds. Similar layers of rock were formed in Antarctica, Australia, South America, Africa and India. (Figure 4) Widespread distribution of Permo-Carboniferous icy sediments in South America, Africa, Madagascar, Arabia, India, Antarctica and Australia and striations that indicated glacial flow external from the equator and towards the poles were discovered and supported the theory of Continental Drift which proposed that southern continents were once located over the South Pole surface area and covered by ice sheets. (Lois Van Wa gner, 2013) (Figure 4)He also discovered a base layer of shale scratched by glaciers and covered by layers of tillite in South Africa, a continent of a tropical equatorial climate. Tillites and varves dating rump to 2 billion years ago, were found in Canada and India, indicating glaciation on a worldwide scale. Such tillites were found on all major(ip) continents except Antarctica, which has been the most extensive glacial continent in earths history. (kangarooistan, 2009) Additionally, fossils of tropical plants in the form of coal deposits were found in Antarctica which implies that Antarctica had to be closer to the Equator. (USGS, 2012) This study of changes in climate taken on the scale of the entire history of Earth is known as paleoclimatology. Sediments of rifting have proved the drifting apart of Pangea.The rifting that formed the South Atlantic Ocean began late in the Mesozoic Period when Africa and South America began to tie apart. Water from the south then flowed in ov er time, thus forming the evaporites now found along the coastlines there. (Lois Van Wagner, 2013)(Figure 5) However, Wegener believed that only the continents were moving and they plowed through and through the rocks of the ocean basins. (Colliers Encyclopedia, 1996) Harold Jeffreys then argued that it is impossible for continents to break through solid rock without breaking apart. (USGS, 2012) Wegener also claimed that the centrifugal force of the spinning planet had oblige the continents sideways, correspond to the equator tidal pull from the sun and moon had caused lateral forepart. (Sant, Joseph, 2012) His orders of order were too weak. Thus, his theory was dismissed. (Lois Van Wagner, 2013) Further development and support of the Continental Drift Theory in the 1960s After World warfare 2, the U.S. Office of Naval Research intensified efforts in ocean-floor mapping, leading to the discovery of the middle Atlantic Ridge to be part of a continous system of mid- naval ridges o n all ocean floors, prompting Harry H. Hess to suggest the theory of sea-floor spreading.The oldest fossils found in ocean sediments were only 180 million years old and little sediment were accumulated on the ocean floor. Thus, he suggested that seafloors were no more than a hardly a(prenominal) hundred million years old, importantly younger than continental land repayable to hot magma rising from volcanically diligent mid-oceanic ridges, spreading sideways, cooling on the seafloors surface over callable(p) to cooler temperatures of the sea, solidifying to create new seafloor, thereby pushing the architectonic nursing homes apart. (Edmond A. Mathez, 2000) The realization that the shape of the Mid-Atlantic Ridge and the Atlantic Coast are strikingly similar substantiated the claim that the continents had been joined together at the Mid-Atlantic Ridge. (J. Tuzo Wilson, 1996) (Figure 6)The cause of the continental drift that Wegener was unable to explain had been further research ed on by Arthur Holmes who claimed that the movement of continents was the result of convection currents driven by the thermal convection in the heat of the interior of the Earth, namely the mantle. The heat source of the mantle comes from radiation syndrome decay in the core. (Figure 7) At constructive abode boundaries, molten basalt flows out on either side of the ridge and cools with the iron particles in the basalt reorient with the earths magnetic field which reverses direction every few hundred thousand years. (Lois Van Wagner, 2013) Due to magma cooling, the chargedity of rocks will be recorded at the time it was formed. (Figure 8.1)In 1950, researchers of paleomagnetism discovered that there were jump regions of normal and reversed magnetic directions symmetrically disposed on both sides of the Mid-Atlantic Ridge magnetic stripping. (J. Tuzo Wilson, 1996) Harry H. Hess theory was thus proven by the magnetic anomalies in the oceanic crust. (Nelson Thomas, 2007) (Figure 8 .2) It was also discovered that the youngest rocks were approximate to the mid-oceanic Ridge and the oldest rocks were near the coasts of the continents. When scientists began collecting magnetic data for North America and Europe, they discovered the north pole seemed to be moving about over time. (ALLA, 2009) However, when data from other continents was collected for the same time frames, it showed different polar locations, thus supporting that continents were moving about.The Theory of casing TectonicsThe theory of eggshell tectonics held that the Earths lithosphere, the Earths crust and the uppermost mantle, is broken into seven macro-plates and about twelve smaller ones, averaging 50 miles in width. (U.S. Dept. of the Interior, Geological Survey, 2007) Any plate may consist of both oceanic crust and continental crust. (Colliers Encyclopedia, 1996) (Figure 9) It suggests that the ocean floor began to spread at constructive plate boundaries, and continents, existing on plates, moved due to convection currents in the mantle and constant sea-floor spreading. (The Columbia Electronic Encyclopedia, 2011). They drag and move plates preceding(prenominal) them due to rising magma spreading out beneath the earths crust. As two oceanic plates move apart, magma from the chthonianlying asthenosphere mantle come up up from oceanic ridges and becomes rigid enough to join the lithosphere of the plates on either side of the plate boundary, creating new seafloor and eventually, an ocean is opened up. (J. Tuzo Wilson, 1996) (Figure 10) Examples are the Atlantic Ocean formed between South America and Africa. young rock is created by volcanism at mid-oceanic ridges and returned to the Earths mantle at oceanic dumpes where the sullenr plate is subducted low the other, forcing the earths crust back into the mantle. (J. Tuzo Wilson, 1996) This process is known as the ridge push and slab-pull. (Figure 11) Different plate tectonics movement and subsequent tectonic activit ies Transform plate movement causing earthquakes Seismic waves disrupting the continents in the form of earthquakes are due to the big(p) amount of stress and energy built up by the crash of the moving plates, especially during transform plate movement, where plates slide past separately other in a grinding, shearing manner and form wear faults (Columbia Electronic Encyclopedia, 2011). (Figure 12.1) There is gradual bending of rocks before the ductile pin down of rocks is exceeded, causing the plates to lock and the fault to break, leading to sudden release of stored energy, causing earthquakes. (Nelson Thomas, 2007)An example is the strike-slip fault, San Andreas Fault in California. (Figure 12.2) (WiseGeek, 2010) Oceanic and Oceanic focussed plate movement Other evidence of plate tectonics movement are most of the worlds active volcanoes located along or near the boundaries between shifting plates known as plate-boundary volcanoes. (J. Tuzo Wilson, 1996) When two oceanic pla tes collided, the denser plate will subduct under the other, forming a deep oceanic trench and form magma through hydration or decompression melting. The magma being less dense than the surrounding mantle, rises and escapes to the sea-floor through cracks in the earths crust, forming submarine volcanoes that rise above water to form a chain of volcanic islands known as island arcs, such as the lacquer Islands. (Figure 13) Examples would be the peace-loving coat subducting underneath the North American Plate creating the Kuril trench and the Japan Trench that can be found along the Pacific Ring of Fire. numerous volcanoes such as Mount St. Helens, Mount Fuji in Japan and Mount Pinatubo in the Phillipines are located along the perimeter of the Pacific Ocean Basin where boundaries of several plates such as the Nazca and the Cocos Plate are found, forming the Ring of Fire. (Fraser Cain, 2009) (Figure 14) Volcanoes formed not due to tectonic activities 5 per cent of the worlds volca noes are formed at obscure hot smudges and many intra-plate volcanoes form roughly linear bonds along the middle of oceanic plates. (The Columbia Electronic Encyclopedia, 2011)Examples are the Yellowstone theme park and Hawaiian Islands, an intra-plate volcanic chain developed by the Pacific plate passing over a deep, stationary hot spot, located 60 km beneath the present-day position of the Island of Hawaii. kindle from this hotspot produced a constant source of basaltic magma by part melting the overriding Pacific Plate.This magma rises through the mantle to erupt onto the seafloor, forming an active seamount. Over time, countless eruptions caused the seamount to grow until it finally emerges above sea aim to form island volcanoes. The continuing plate movement eventually carries the island volcano away from the hotspot, cutting it off from the hot spot and creating another island volcano. This cycle is repeated, forming the Hawaiian Islands. (U.S. Dept. of the Interior, Geo logical Survey, 2007) (Figure 15) Continental and Continental convergent plate movement Continental fold mountain ranges are evidence of two continental plates that are thick and buoyant thus, preventing both plates from subducting. Instead, the two plates collide into each other forming fold mountain ranges in a process known as orogenesis.An example is the high elevation of the Tibetan plateau, fringed to the south by the Himalayas as the edges of the Indian and Eurasia plate buckle, uplift, fold and deform. Mt. Everest is the highest summit on Earth, yet Yellowband limestone that was originally part of the shallow seals of the Tethys Ocean was found on Mount Everest at a height of 8462m. (Figure 16) Oceanic and Continental convergent plate movement Mountains are formed when oceanic crust is subducted under a continental crust, resulting in melting of rock, thus volcanic activity and causing the continental crust to deform, rise and buckle upwards under compressional forces.Exampl es are the Andes Mountain, the Chile-Peru Trench and the uplift of the Rockies and Appalachians in the past. (The Columbia Electronic Encyclopedia, 2007) The give in Mountains was formed approximately 250 million years ago, due to the Pacific plate subducting under the North American plate, (Mary Ann Resendes, 2012) thus creating the Sierra Nevada foothills, subsequently creating the mantel of Good Hope as the ocean erodes the soft sandstone of Table Mountains on the coast. (National Geographic, 1996)Other tectonic activities such as the Wadati-Benioff zones, that are earthquake zones parallel to oceanic trenches are also formed at such subduction zones and inclined(p) from 40 to 60 degrees from the horizontal, extending several hundred kilometres into the mantle. (Figure 17) Continental and Continental divergent plate movement When two continental crusts are pulled apart due to tensional forces, the area sinks and forms a rift valley and sea such as the East African Rift Valley and the Red sea that runs from the Jordan Valley and into East Africa, already dotted with volcanoes such as Hermon. This is due to the area being stretched, causing the crustal material to thin, weaken and sink due to lowered density. (Figure 18)IsostasyAlso, isostasy takes place wherever a declamatory amount of clog such as the fold mountain ranges created from plate tectonics movements is formed or glaciers, pushes down the Earths crust and creates a small dent. Isostasy also takes place at divergent plate boundaries when a large amount of weight is removed from an area, causing that portion of the Earths crust to rise. Therefore, equilibrium in the earths crust is achieved such that forces elevating landmasses balances those tending to depress landmasses. (Learning Network, 1998) (Figure 19)