Plate tectonics is the theory that the exterior layer of the earth's (lithosphere) is separated into multiple plates that are continuously moving around the earths surface. (Fichter, 2000). The theory looks at the way plate tectonics have divided, clashed and been altered throughout human history. (Plate Tectonics, 2018). The theory of plate tectonics has been in the making for 400 years by multiple scientists and geologists. Plate tectonics started as a small idea, only having the slightest bit of evidence supporting the theory. However, throughout time the theory around plate tectonics later progressed into today's hypothesis. “The separating of continents” also including “the forming of many geographical features”. Plate tectonics also
He proposed that the continents were once connected, and that “America was torn away from Europe and Africa . . . by earthquakes and floods". (Hanks, 2012). This was the first suggestion that a supercontinent called Pangea existed long ago. Years later in 1638 a geologist named Nicolaus Steno introduced a new theory called the ‘Law of Superposition’. As Steno looked deeper into the theory and found out that in a sequence of sedimentary rock layers, each layer of rock is older than the layer above it. Hundreds of years later, this theory was continued on by Scottish geologist, James Hutton. In 1785 Hutton stated that erosion began the natural process of forming new land and surfaces. (James Hutton, 2018). This theory, then provided much more evidence to help scientists and geologists find what was really going on with our
Within the scientific community multiple ideas and concepts were improved and altered to confirm the plate tectonics theory. To achieve this confirmation scientists had to cover the research of convection currents within the mantle, layers of rocks, the supercontinent ‘Pangea’ and the moving of tectonic plates. From 320 million years ago and still to this day the earth is consistently moving and changing due to several geographical factors we now know about, because of the in-depth research that scientists
Earthquakes are a natural part of the Earth’s evolution. Scientific evidence leads many geologists to believe that all of the land on Earth was at one point in time connected. Because of plate tectonic movements or earthquakes, continental drift occurred separating the one massive piece of land in to the seven major continents today. Further evidence supports this theory, starting with the Mid-Atlantic ridge, a large mass of plate tectonics, which are increasing the size of the Atlantic Ocean while shrinking the Pacific. Some scientists believe that the major plate moveme...
could be used to explain and illustrate that previous theories were not entirely correct (Merali and Skinner, 2009, p.253). Through the analyzation of arrival times of these waves, Oldham had drawn an conclusion that p waves and s waves react differently in terms of being refracted, reflected or absorbed depending on the state of the material as shown in Figure 1.(Tarbuck, Lutgens, Tasa, 2013, p.143). Oldham had developed this theory of the Earth not being the same state due to these effects of seismic discontinuity which are shown in Figure 1., consisting of refraction, reflection and absorption. The changes that are displayed from this idea are; the speed of the waves due to a refraction occu...
Source 4. A map of the Earth’s fault lines and plates with the direction of their movement.
Back then, no one understood how or why the two rocks were next to each other until around 40 years ago when the theory of plate tectonics was introduced. The purpose of the tectonic theory was to explain the process of earthquakes, not just around the San Andreas Fault, but also on the others that ran concurrent to it.
The traditional theory about the Earth’s core suggest that the core of the Earth is a solid nickel and iron sphere surrounded by a fluid metallic magma. The rotation of the Earth is believed to create massive columns of magma to swirl in the core. These columns are believed to produce the Earth’s magnetic field. This theory is based on the assumption that the Earth’s core is cooling and will eventually cool completely and cease to produce energy and a magnetic field. However, this theory does not answer many ongoing mysteries about the Earth, such as why the Earth’s magnetic field periodically shuts down, and questions about the energy production of the Earth. It was apparent that a new theory was needed to explain the mystery of the Earth’s core.
...s from the Paleozoic, Mesozoic, and Cenozoic periods show proof of how animals have gone through evolution and why certain fossils look very similar. The Law of Original Horizontality and the Law of Superposition both express true when looking at modern rock layers today. The Law of Original Horizontality happens when sediments are constantly deposited over old layers of rock forming new layers over millions of years, while the Law of Superposition is the law that older rock layers lie beneath the newer layers. Also, Pangea and Panthalassa are now the seven continents and four oceans of the world today as a result of Continental Drift. All things considered, Rock layers are therefore evidence of Evolution for, rock layers holds proof of evolving animals seen through fossils, the plates in the earth separated Pangea, and the relation of evolution and rock layers.
Hutton thought that sedimentation takes place so slowly that the oldest of rocks are made of, in his words, “materials furnished from the ruins of former continents.” The opposite happens when rock is eroded or decayed from weather or conditions of the area. He called this destruction and renewal the “great geological cycle,” and then realized that it had been happening for many years. Another one of Hutton’s theories was the Theory of Uniformitarianism. That was the idea that geological forces still at works today, were not that noticeable to people but they have a great affect on us, meaning that those forces still work the same as they did in the past. He died March 26th, 1797 in Edinburgh.
First you might need to know definition of tectonics. It is a theory in geology. The lithosphere of the Earth is divided into a small number of plates which float on and travel independently over the mantle and much of the Earth’s seismic activity occurs at the boundaries of these plates. That is the official definition of Plate tectonics. secondly, this plate covers many parts of continents. plate boundaries don’t go according to Continents boundaries, they make their own boundaries. The North American plat...
The plate tectonic theory is a theory that geologists use to help explain the Earth’s surface processes and events. It explains that the sliding of these plates are either away from each other, sliding past each other, or sliding into each other and causing one of the plates to slide beneath the other. There are three kinds of plate tectonic boundaries: divergent, convergent, and transform plate boundaries. A divergent boundary occurs when two tectonic plates move away from each other. Magma then flows up from the mantle to fill in the space between the plates, forming a raised ridge called a mid-ocean ridge. The magma also spreads in the exterior, forming new ocean floor and new oceanic crust. A convergent boundary occurs when two plates
They are the earth’s crust; they move very slowly every year. As the tectonic plates slide over each other they cause earthquakes. Earthquakes produce various damaging effects this includes damage to structures of buildings, bridges and other standing formations which then...
Earth was formed 4.8 billion years ago (3) . It became the home for hazelnuts because it had an atmosphere and environment which allowed for life to prosper in later years. Earth’s surface was once composed of a single landmass, known as Pangaea (1).Over time it was broken up into seven different plates which were free to move as a result of movements in the hot, semi-liquid magma beneath the...
Thomas Kuhn, one of the most widely recognized contributors to the discipline of the philosophy of science, raises the argument within The Structure of Scientific Revolutions that advancement within the field of science occurs in a revolutionary manner as opposed to one more progressive or cumulative. Kuhn makes the observation that scientific research is conducted cumulatively where every piece of evidence contributes towards gradually understanding a specific scientific phenomenon (Kuhn, 96). However, lasting scientific advancement only transpires when previously accepted scientific theories are overturned with entirely different, more suitable theories. Kuhn makes reference to the Copernican Heliocentric model as an instance to validate his assertion (Forster). Applying Kuhn’s argument to this revolutionary theory will provide clarity and further understanding necessary to demonstrate how this philosophical approach can be applicable towards relatively modern scientific theories such as plate tectonics.
The field of geology has many different branches. Some of these areas have hardly anything in common. The one thing that they all include, though, is that each one concentrates on some part of the Earth, its makeup, or that of other planets. Mineralogy, the study of minerals above the Earth and in its crust, is different from Petrology, the st...
Plate tectonics is the theory that landmasses on tectonic plates are in slow constant movement due to convection currents in the mantle. Plate tectonics, or the movements of plates above the lithosphere (the most upper layer of earth's crust) can cause divergent, convergent,and transform boundaries.A boundary the way two tectonic plates collide. is Continental plates are plates that the continents are formed on. Oceanic plates are plates that the ocean covers, and the oceans form on top of these plates. Convergent boundaries and divergent boundaries are ways that these oceanic and continental plates interact with each other. Landforms are formed at boundaries. The landforms formed at boundaries depends on the type of plates that collide, and
Due to the fact that rocks are composed of high intensity of elastic and brittle material, they therefore store considerable amount of strain energy that results from elasticity, during the action of plate tectonic. The brittleness leads to development of concurrent cracks on the rocks as a result of plate’s action.