-The relationship between continental drift and the formation of the Earth’s Oceans stems from plate movement that occurred on Earth. There is a theory that all the continents were once all one big piece of land named Pangaea, and over millions and millions of years the land of Pangaea started to split apart into many different continents. It divided Panthalassa, the large global ocean that surrounded the supercontinent Pangaea, into many different oceans instead of just one big one and now we have many various oceans around the world.…
Plate tectonic theory is a widely excepted theory that the Earth’s lithosphere is made up of plates, both oceanic and continental, which slowly move due to convection currents in the mantle and the asthenosphere. However, it is very hard to be certain as we can’t see the structure of the Earth, so some people do not agree with it. This theory saw the introduction of what we know today to be tectonic plates. Tectonic plates occur where there is radioactive decay in the core and temperatures are extremely high. This decay can occur anywhere in the earth’s core. This results in a plume of magma rising through the mantle creating a thermal current. When this current reaches the surface it spreads through the asthenosphere, before cooling and sinking. These are the convection currents which move tectonic plates. Convection currents will only occur in liquid form and in warm conditions. Tectonic plate theory has evidence to prove that these currents do take place. We know that the mantle is liquid and has high temperatures as magma that originates in the mantle is molten. This means that convection currents can occur. This part of plate tectonic theory is supported by global seismic activity because if convection current did not exist and plates were not able to move, earthquakes would not occur at any plate boundaries, but particularly at collision plate boundaries as there would be no plate movement.…
Over the years proceeding the birth of the theory, increasingly convincing evidence has been gathered for proof of the theory of plate tectonics. In 1912, Alfred Wegner proposed the theory that continents are sat upon tectonic plates and that these plates are slowly drifting around the Earth (continental drift). Since then, volcanic and seismic events have made up a large proportion of the evidence towards the theory, including volcanic eruptions at both constructive and destructive boundaries, hotspots, sea floor spreading, paleomagnetism, and seismic earthquakes. However, not all of the evidence supporting plate tectonics comes from volcanic and seismic events; other evidence includes continental fit, geological evidence, biological evidence, climatological evidence and other activity at destructive plate margins.…
This theory was shown to be maybe correct when the mid-Atlantic ridge was discovered and a similar feature was discovered in the Pacific Ocean. After investigating it was suggested that sea floor spreading was occurring. Evidence for this was from alternating polarity of the rocks that form the ocean crust. Sea floor spreading implies that the Earth’s crust must be getting bigger. As we know this isn’t the case then the plates must be being destroyed somewhere to accommodate the increase in their size at mid oceanic ridges. Evidence was found with the discovery of huge oceanic trenches where large areas of ocean floor were being pulled downwards.…
The plate tectonic theory is the theory that describes large amounts of movements in the Earths lithosphere, whereby Continental and Oceanic crust is moved, destroyed and made from this. The idea of plate tectonics builds on other concepts such as continental drift, where continental plates over millions of years move, however the concept of continental drift was not accepted for some time, and there were many other theories to suggest that something else took place, as the idea of the earth moving was not accepted until it was clear from things such as maps and satellites which clearly show how continents such as south America and Africa used to fit together.…
1. Continental drift and the formation of the Earth’s Oceans are formed from plate tectonics. Plate tectonics occurred on Earth millions of years ago when Earth was known just to have one giant supercontinent known as Pangea. Pangea was made up of all our seven continents today and had one ginormous ocean called Panthalassa that surrounded the supercontinent. After millions of years plate tectonics did its job and split apart the supercontinent to what we have today with our seven continents. Therefore the relationship between the continental drift and the formation of the Earth’s oceans is plate tectonics.…
Movement of Earth’s Plates:The plates move due to the mantles CONVECTION CELLS: warm material rises toward surface, cools&descends back into the interior. Creating volcanoes, earthquakes, MTNS.…
The Continental drift was the process in which the Earth’s land surfaces ( at the time known as the pangea) started slowly breaking apart and drifting away. This has continued until the continents were in the places we know them to be today. This drift has caused the formation of separate oceans instead of one huge one. This drift still continues today.…
Earthquakes are an example of seismic activity caused by the build-up of tension at the three types of plate boundaries: destructive, constructive and conservative. The pressure is suddenly released as the plates jerk past each other, sending out seismic waves from the focus that travel through different parts of the earth. The movement of convection currents within the Earth’s mantle causing the crust to become mobile which creates the different types plate margins, makes the cause due to physical factors. However human activity is suggested to be the cause of some minor earthquakes, for instance the building of large reservoirs where the water stresses the surface rocks or the subsidence of deep mine workings.…
Plate tectonics theory, which is the modern theory of the motions of Earth’s layer, explains how geological features, such as mountain ranges, continents, and bodies of water move and form. An important aspect of plate tectonics theory is that the outer layer of the earth is divided into plates which move across the earth’s surface. “These plates move relative to each other, typically at rates of 2-4 inches per year. As the plates move, they interact along their boundaries” (Plate Tectonics). In other words, the formation of geological features occur at the plate boundaries which is where plates slide and interact. There are four types of plate boundaries: divergent boundaries, convergent boundaries, transform…
Over time plate movement or subduction causes increasing strain on "sticking points" within the crust. Similar to if you rub two pieces of sand paper together, they will initially resist sliding until enough strain is built up. At that point, the "sticking point" is weakened and releases the built up strain. Before this theory was developed, scientists were unsure whether earthquakes caused faulting (plate movement) of faulting caused earthquakes.…
The plate tectonics theory was put forward by Alfred Wegener suggesting that the continents were at one point all conjoined in one supercontinent known as Pangaea. He then said that Pangaea had drifted apart through the movement of plates to give us the current places of continents we have today. Wegener's theory was linked to a variety of evidence, however it took further research and evidence for this to become a leading theory. This means that although volcanic and seismic events help to prove the plate tectonics theory valid, there is also a range of other factors involved.…
All oceanic and continental plates move within the lithosphere, which is the outermost shell of the planet. The lithosphere has more strength than the underlying asthenosphere allowing the tectonic plates to move. Seafloor motion away from the spreading ridge and drag at the subduction zones is a theory for plate movement. The tidal forces of the sun and moon and the forces generated by the rotation of the globe is another idea for plate movement. There are other hypotheses on plate movement but these are the two main scientific theories. The relative importance of these factors are unclear and still on…
Earthquakes develop in the crust of the earth. The inner parts contains a lot of energy. Some of this energy can escape through cracks which can cause volcanic activity, but most of it is stored within the earth’s inner part, contained in the crust.The earth’s outer crust has rough edges and lines making it look a bit like a jigsaw puzzle.The energy stored here causes the pieces to slide, glide, knock and move around each piece. These pieces are also known as tectonic plates.…
Plate tectonics help us to explain the process of folding. According to the theory of plate tectonics, the earth’s crust is broken up into sections called plates. These plates float on the semi-molten mantle. Thermal convection currents in the mantle drag these plates in different directions resulting in tectonic activity.…