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Effects of natural disasters on human lives
Effects of natural disasters on human lives
Effects of natural disasters on human lives
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Report on Earthquakes by Zeta Stevens
Why Do Earthquakes Occur?
The earth is split into four layers, inner and outer core, the mantle and crust. The top of the mantle and crust make up what is like the skin of our earth (see source 2). The skin is split up like a puzzle and we call these puzzle pieces’ tectonic plates (see source 1). These plates are constantly moving and the plate boundaries (edges of the plates) move and slide past one another. Sometimes as the plates move the plate boundaries become stuck. Pressure builds up in the stuck area over time and eventually breaks. This is why earthquakes occur due to the sudden movement of the plate sliding and breaking creating a fault line to go off. The fault line is the line on which the
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Source 4. A map of the Earth’s fault lines and plates with the direction of their movement.
Although there is no way of knowing exactly when an earthquake is going to occur. Scientists have been able to predict an earthquakes range for them to occur. For example, if a fault hasn’t gone off for around 20 years, then this fault is likely to go off in the next five years. This is as close as scientists can get to exactly knowing when an earthquake will occur, although this can still help people to be prepared to some extent. We know that an earthquake will occur with the tectonic plates movements and with them either colliding, sliding or doing both against each other. An earthquake will occur with the force of these movements, but depending on the strength of the movements depends how strong the earthquake is on the Richter Scale (see source 5) or on a Seismograph (see source 6).
Earthquakes are frequent but most of the time aren’t very big on the Richter Scale. Statistics and research show that there are earthquakes happening constantly, but most of the time are impossible to feel unless they are above a 3 on the Richter Scale (see source7).
Source 6. A diagram of how a seismograph works and the measurements Source 7. Statistics on the Earth’s earthquakes
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This is one of the most commonly asked questions around the world. Earthquakes are very common because the Earth’s tectonic plates are constantly moving, because they are constantly moving earthquakes are happening quite often across the globe. Statistics show that over 1 million occur each year worldwide (see source 9), but earthquakes don’t have to be felt for them to have occurred. Statistics prove that 1 100 000 earthquakes happen per year worldwide that can’t be felt by humans. Statistics show that about 11 670 earthquakes occur that can be felt in the area of occurrence and sometimes even further
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...
Massive Mega-Quakes happen at regular intervals in the Pacific Northwest. There have been mega-quakes in the beginning of time. In Japan, a mega-quake send a 600-foot wave of water.
Before examining the Northridge event, understanding the naturally occurring hazard that is an earthquake will help to better understand exactly what happened and why it was such an important geological event. With four distinct layers, two layers, the crust and upper portion of the mantle, compose the skin that is the surface layer of the Earth. The crust is not a single, continuous piece. It is actually several different pieces, or plates, that come together to form the puzzle that comprises the surface of the Earth. These plates are in constant motion rubbing against one another. These areas, known as fault lines, where the plates rub up against one another have spots where one plate ”gets stuck while the rest of the plate keeps moving. When the plate has moved far enough, the edges unstick and is how most of the earthquakes around the world occur” (Wald, 2012). The energy stored from the friction of the two plate...
Geology 2400 is a course where students are taught different examination of the earth such as the solar system, interior surface of the earth, atmosphere, and relationships of earth systems such as natural disasters. Three essential concepts I mastered was: earthquake’s wave, the planets, and minerals. First, one scheme of a natural disaster is an earthquake. An earthquake is the violent shaking of the ground which sometimes causes great destructions. Earthquakes happened due to seismic waves. A seismic wave is a wave in the earth that is produced by an earthquake. In addition, body waves play a big role in earthquakes. Primary wave (P), is the fastest and it is compressional meaning it can pass through liquids gasses and solids. A secondary wave(S) is the second fastest wave that is shearing, meaning it can only go through solids. Nest, the surface waves also known as the L waves, travel along the surface. For example, these types of waves look like “ripples” moving vertically up and down in motion. On the contrary, love waves (LQ) are horizontal waves and
Chapter 3 is about Earth’s structure and plate tectonics. Earth’s interior is consists of four layers inner and outer core, mantle, and Earth’s crust. Each layer is thicker than the layer above. Millions of years ago Earth was as one continent, but eventually the continents have spread out from each other. Continents are floating in the ocean and constantly moving towards or away from one another. The movement of continents is due to plate tectonics about 1-15 centimeters a year. Different plates move at a different rate. There are about a dozen of tectonic plates on the Earth. The plates have converged, diverged, and slipped past one another since Earth’s crust first solidified and cooled, driven by slow, heat-generated currents rising and
Beno Gutenberg was the foremost observational seismologist of the twentieth century. He combined exquisite analysis of seismic records with powerful analytical, interpretive, and modeling skills to contribute many important discoveries of the structure of the solid Earth and its atmosphere. Perhaps his best known contribution was the precise location of the core of the Earth and the identification of its elastic properties. Other major contributions include the travel-time curves; the discovery of very long-period seismic waves with large amplitudes that circle the Earth; the identification of differences in crustal structure between continents and oceans, including the discovery of a significantly thin crust in the Pacific; the discovery of a low-velocity layer in the mantle (which he interpreted as the zone of decoupling of horizontal motions of the surficial parts from the deeper parts of the Earth); the creation of the magnitude scale for earthquakes; the relation between magnitudes and energies for earthquakes; the famous universal magnitude-frequency relation for earthquake distributions; the first density distribution for the mantle; the study of the temperature distribution in the Earth; the understanding of microseisms; and the structure of the atmosphere.
Simkin,T., Unger, J., Tilling, R., Vogt, P. and Spall, H. (1994) This dynamic planet : world map of volcanoes, earthquakes, impact craters, and plate tectonics. U.S. Geological Survey, Map Distribution
The basic science is pretty straightforward. The earth lurches from time to time because its outer shell is broken into huge, solid plates floating on a layer of molten rock that has the consistency of Silly Putty. These tectonic plates are constantly jostling each other, like rafts crowded into a small pond, and its along the boundaries where they meet that most quakes are born.
Richer Scales Measures in Earthquakes (2011), Weegy [online] Available at: http://www.weegy.com/home.aspx?ConversationId=E0B052FE [Accessed September 9, 2011]
Earth's floor then is sucked into deep ocean trenches creating a force, this called subduction. As two rock plates slide past one another a crack or fault develops, which prevents energy to form an earthquake. One of these plates are called Tectonic Plates. Tectonic Plates are pieces of crust moving around earth, pushing together, pulling apart and sliding past each other. The second plate is Plate Tectonics. This is when earth's crust is made up of rigid plate that "float" on molten layer of the mantle beneath earth's crust. Oceanic- oceanic plate is a similar plate that sinks under the other when the two plates converge. With these plates in motion, causes movement and the split of continents. As one plate moves, it cause other plates to move. The split between supercontinent led to divergent evolution, unique species formed in response to different environment conditions, this was the height of the age of
An earthquake is caused by two tectonic plates suddenly slip past each other and cause the shaking of the ground. The spot at which the two plates slip past each other is called a fault or fault plate. The area below the earth’s surface where the earthquake starts is called the hypocenter. The spot directly above the hypocenter, and on the surface, is called the epicenter. An earthquake can also have foreshocks. Foreshocks are smaller earthquakes that are in the same place as the larger earthquake which follows
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...
Keller E A and Pinter N (1996) “Active tectonics: Earthquakes Uplift and Landscapes”; Prentice Hall, New Jersey.
Earthquakes are natural disasters that are also referred to as a ‘quake’ or ‘tremor’. It is classified as a geomorphic hazard, which are elements of the physical environment that can cause damage, (economically and environmentally) such as Volcanoes, Tsunamis, Landslides etc. Earthquakes have been around for thousands of years but no one had properly understood the concept. Not one person, but a crowd of geologists and scientists had discussed this hazard and identified what it actually. There have been some weird beliefs about earthquakes such as earthquakes were caused by air rushing out from caverns underground.
Earthquakes belong to the class of most disastrous natural hazards. They result in unexpected and tremendous earth movements. These movements results from dissemination of an enormous amount of intense energy in form of seismic waves which are detected by use of seismograms. The impact of earthquakes leaves behind several landmarks including: destruction of property, extensive disruption of services like sewer and water lines, loss of life, and causes instability in both economic and social components of the affected nation (Webcache 2).