Baby Boomers free essay sample

In the article Blue Collar Boomers Take Work Ethic to College Sander’s makes that argument that the baby boomers of our time are still eligible to work, and are very willing to try new ways of achieving the education to start different forms of work. Most of the baby boomer generation had gone straight to hard labor jobs to help bring home money for their families, and now that they are older the labor is straining on their bodies (Sanders 3). While they may be older, they are still capable of learning how to use new technology and expanding their minds (Sanders 27). Sanders discusses that college is no longer a place for young adults to attend once out of high school, but rather a place for anyone to receive high education in order to attain a job. Some of the older Americans are choosing to go back to college. Mr Hill says, â€Å"I want a job sitting down, at the computer, in the cubicle†¦after being out in the field for so many years, I would like a sit-down job. We will write a custom essay sample on Baby Boomers or any similar topic specifically for you Do Not WasteYour Time HIRE WRITER Only 13.90 / page Mr. Hill had decided that after working in the cold for so long, he thought that he deserved to make good money while not doing much physical labor (Sanders 24). After being a part of a great things or helping their country, some of the baby boomers believed that they deserve to live a cushy life. To a different extent, older Americans have to continue college as a matter of necessity. In paragraph 30 Mr. Ronan states, â€Å"They do not have the luxury nor the interest in going back to college for two or three years, they need something quick † This statement tells readers that older Americans do not have the luxury to go back to college because unlike younger Americans, they have bills to pay. Some of the baby boomers are continuing college for a job because the hard labor of their old career has left their bodies withered (Sanders 3). However, just because their bodies are incapable of hard work, does not mean that their minds are. When these older students come to college, they bring their values with them. In today’s society, people believe that college is just something that mostly everyone must go to after high school as a part of their path in life; and some take it for granted. The older Americans, or baby boomers, did not have the opportunities to go to college like we do. To them, college is a wonderful experience to learn the things needed to go into their field of work or even just to further their own knowledge. Baby boomers realize the value of a good education and what it can bring for their careers (Sanders 31). They are simply merging their work ethic from hard labor jobs, to studying just as hard in the class room.

Pierre Trudeau, Former Prime Minister Of Canada, Was Once Described As Essay Example For Students

Pierre Trudeau, Former Prime Minister Of Canada, Was Once Described As Essay A French Canadian proud of his identity and culture, yet a biting critic of French-Canadian society, determined to destroy its mythology and illusions. He has also been identified as A staunch, upholder of provincial autonomy holding the justice portfolio in the federal government. Such cumulative appraisal and observation made by past fellow bureaucrat provides high testimonial for the ex-Democratic Socialist. This critique will establish and dispute the prime directives that Trudeau had advocated in his own book written during the years 1965 to 1967. The compilation of political essays featured in his book deal with the diverse complexities of social, cultural and economical issues that were predominant in Canadian politics during the mid 1960s. However, throughout my readings I was also able to discover the fundamental principles that Trudeau would advocate in order to establish a strong and productive influence in Canadian politics. Born in 1921, Trudeau entered the world in a bi lingual/bicultural homelocated in the heart of Montreal, Quebec. His acceptance into the University of Montreal would mark the beginning of his adventures into the Canadian political spectrum. Early in his life, Trudeau had become somewhat anti-clerical and possessed communist ideologies which were considered radical at the time. Graduating from prestigious institutions such as Harvard and The School of Economics in England, Turdeau returned to Canada in 1949 and resumed his social science endeavors. At this time in Quebec, the province was experiencing tremendous cultural and political differences with the rest of the country. The Union Nationale had taken possession of political matters in Quebec and was steadily dismantling the socialist essence imposed on the province by the Federal government. The current Prime Minister, Maurice Duplessis, found himself battling a religious nationalist movement that corrupted the very fabric of political stability in Quebec. The Duplessis facti on maintained their conservative approach towards political reform but failed to sway the majority of the population into alleviating with the demands of the Canadian government. The citizens of Quebec revered their clerical sector as holding utmost importance towards preserving French cultural values and this did not correlate with the Federal governments policies and ideals. Francophones were under the impression that their own Federal government had set out to crush and assimilate what had remained of their illustrious heritage in order to accommodate economic and political tranquility. Trudeau himself had decided to join the nationalist uprising with his advocation of provincial autonomy. Ultimately, he and other skilled social scientists attempted to bring down the Duplessis party in 1949, but failed miserably in their efforts. Duplessis buckled underneath the continuous pressure of French patriotism and was rewarded for his inept idleness by winning his fourth consecutive elec tion in 1956. Although nothing of significance had been accomplished, Quebec has solidified its temporary presence in confederation at such a time. This prompted Trudeau to involve himself in provincial diplomacy as he would engage in several media projects that would voice his displeasure and disapproval with the ongoing cultural predicament in Canada (this included a syndicated newspaper firm, live radio programs). If, in the last analysis, we continually identify Catholicism with conservatism and patriotism with immobility, we will lose by default that which is in play between all cultures. By literally encouraging a liberal, left-wing revolution in his province, Trudeau believed that Democracy must come before Ideology. Gradually, his disposition would attract many politicians and advocates of Socialism, and thus it allowed him to radiate his ideology onto the populace of Quebec. Trudeau makes it clear in his book that during the early years of the Duplessis government, he was a staunch admirer of provincial autonomy, but with the archaic sequence of events following the conflicts that arouse between Federal and Provincial matters in Quebec, he had taken a stance on Federalism that involved security, economic prosperity and centralized authority. It wasnt until 1963 when the newly appointed Premier of Quebec, Rene Levesque, warned that there must be a new Canada within five years or Quebec will quit confederation. It was not until 1965 that a man named Pierre Trudeau entered politics. It is at this point in his anthology that I was able to surmise the radical and unorthodox political convictions that the soon-to-be Prime Minister would incorporate into Canada. His thesis is focused around pertinent issues which demanded attention at the time. After he elaborates on the importance of Federalism and how it is associated with Quebec, the reader begins to interpret the resolutions he offers and then finds himself comprehending the dilemma that French Canadians face in Canada. In the wake of a constitutional referendum, such knowledge can be viewed as ironically significant. A defender of civil rights and freedoms, Trudeau, even as a teenager, was adamantly opposed to supporting any political theory based on ethnic tendencies; he makes this clear on an essay in the book entitled: Quebec and the Constitutional Problem. He was convinced that not only the divided jurisdiction of a federal state helped protect the liberty of its citizens but also that in fact the economic, social and cultural goods of Quebec can best be achieved with a Canadian federal state. It seemed that an archetypal Trudeau Federal infrastructure would be one where each level of government would function on its own jurisdiction. In doing so, Trudeau would voice his admiration for the Bill of Rights and how he would concentrate on developing a Federal government for the individual. It was not until 1962 that Trudeau actually began defending Federalism for what it represen ted to the average labourer, but the fact that Quebec seemed to convert provincial autonomy into an absolute forced him to reconsider his political stance. Joining the struggling Liberal party in 1965, his only coinciding proposition with that of his party was the advocation of an open Federal system. Nonetheless, it marked the beginning of a political career that would take him to the heights of power in his dominion. .u689772dcc031d4bd2a8f4c1601c7b7c0 , .u689772dcc031d4bd2a8f4c1601c7b7c0 .postImageUrl , .u689772dcc031d4bd2a8f4c1601c7b7c0 .centered-text-area { min-height: 80px; position: relative; } .u689772dcc031d4bd2a8f4c1601c7b7c0 , .u689772dcc031d4bd2a8f4c1601c7b7c0:hover , .u689772dcc031d4bd2a8f4c1601c7b7c0:visited , .u689772dcc031d4bd2a8f4c1601c7b7c0:active { border:0!important; } .u689772dcc031d4bd2a8f4c1601c7b7c0 .clearfix:after { content: ""; display: table; clear: both; } .u689772dcc031d4bd2a8f4c1601c7b7c0 { display: block; transition: background-color 250ms; webkit-transition: background-color 250ms; width: 100%; opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #95A5A6; } .u689772dcc031d4bd2a8f4c1601c7b7c0:active , .u689772dcc031d4bd2a8f4c1601c7b7c0:hover { opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #2C3E50; } .u689772dcc031d4bd2a8f4c1601c7b7c0 .centered-text-area { width: 100%; position: relative ; } .u689772dcc031d4bd2a8f4c1601c7b7c0 .ctaText { border-bottom: 0 solid #fff; color: #2980B9; font-size: 16px; font-weight: bold; margin: 0; padding: 0; text-decoration: underline; } .u689772dcc031d4bd2a8f4c1601c7b7c0 .postTitle { color: #FFFFFF; font-size: 16px; font-weight: 600; margin: 0; padding: 0; width: 100%; } .u689772dcc031d4bd2a8f4c1601c7b7c0 .ctaButton { background-color: #7F8C8D!important; color: #2980B9; border: none; border-radius: 3px; box-shadow: none; font-size: 14px; font-weight: bold; line-height: 26px; moz-border-radius: 3px; text-align: center; text-decoration: none; text-shadow: none; width: 80px; min-height: 80px; background: url(https://artscolumbia.org/wp-content/plugins/intelly-related-posts/assets/images/simple-arrow.png)no-repeat; position: absolute; right: 0; top: 0; } .u689772dcc031d4bd2a8f4c1601c7b7c0:hover .ctaButton { background-color: #34495E!important; } .u689772dcc031d4bd2a8f4c1601c7b7c0 .centered-text { display: table; height: 80px; padding-left : 18px; top: 0; } .u689772dcc031d4bd2a8f4c1601c7b7c0 .u689772dcc031d4bd2a8f4c1601c7b7c0-content { display: table-cell; margin: 0; padding: 0; padding-right: 108px; position: relative; vertical-align: middle; width: 100%; } .u689772dcc031d4bd2a8f4c1601c7b7c0:after { content: ""; display: block; clear: both; } READ: A Turning Point in My Life Essay My political action, or my theory insomuch as I can be said to have one can be expressed very simply: create counter-weights. The measure of a man can be traced to his ideological convictions, and in doing so, I have only started to realize the prominent role that Trudeau has played in Canadian politics. He was heralded as a radical, somewhat of a usurper and definitely a socialist mogul, but what was clear about Trudeau was his respect and admiration for liberties of the common man and how they were preserved from the clutches of Federal policies. This respect would not be replaced at any cost during his tenure and as he forecasted the ensuing constitutional dilemma with a very impartial, non-partisan outlook, he would primarily concentrate on two factors (economic and linguistic) which offered practical conclusions without chaotic implications. Trudeau envisioned himself in power, speculating two choices he would offer to Quebec; full sovereignty or maximized integration into the American continent. But what Trudeau avoided treading upon was the infringement of state policies on the individuals rights and freedoms. Many members of the Federal government believed that Trudeau did not speak on behalf of French Canadians but that he substituted their cultural plight with his own theories. This generated the following response: If the party does not agree with my opponents, it can repudiate me; if my constituents do not, they can elect someone else. Trudeau maintains that he dedicated his anthology in order for others to understand the problems that French Canadians faced in terms of cultural progress, and I am compelled to conclude that his involvement with the Federal regime may have saved the country for twenty yearsunfortunately, he was unable to complete the affirmation of his ideology into the French Canadian scope and thus Canada today is contemplating the outcome of another constitutional referendum. His failure to absolve the constitution of any future repercussions with the masses should not be viewed as a political error, but as an ideological truth which he exhibited since 1965 (the addition of the notwithstanding clause). Trudeaus book covers an immense amount of historical and idealistic content. Published in 1965, it is fascinating to read and discover how intently and closely he would follow his ideologies as he would eventually ascend to the position of Prime Minister. His reliability would be questionable at the time (based on limited experience as a politician) but the fact that he had submerged himself into a field which required innovative and pragmatic thought led me to believe that his Federalist stance would eventually be justified in Canadian history. With a superlative writing style, his use of vocabulary and terminology aided the reader in understanding his convictions. Not even this reader expected such a barrage of political jargon. Recent events in Canada have somewhat curtailed the ambience dealing with this critique in respects to the opinions exhibited on behalf of the author and reviewer. Trudeau takes obvious pride in his ideological perspective of multicultural Canada, and in doing so one might expect a partisan, biased array of resolutions. This, however, is not the case. This book leaves room for educational prowess without any noticeable weaknesses. Federalism and the French Canadians is an insightful, ideological anthology that could be found especially useful to other politics students who wish to examine the importance of cultural and social values in a country missing a stable political doctrine (and perhaps a leader, no less).

Scoping report for the earthquakes in New Madrid, and Fulton City, Missouri

Introduction Earthquakes are not a new phenomenon in the U.S.: numerous parts of the country experience them. They are cause stress accumulation in the underground rocks. The accumulation of this stress is a clear indication of the slow but constant movement of the earth’s outermost rocky layers.Advertising We will write a custom report sample on Scoping report for the earthquakes in New Madrid, and Fulton City, Missouri specifically for you for only $16.05 $11/page Learn More These are large sections of which move about earth as tectonic plates. The collision or grinding of adjacent plates leads to stressing of rocks. This stress is then released to the earth’s surface in the form of sudden shifts. Consequently, plate boundaries are the primary breeding ground for earthquakes. Earthquakes have many effects. They can cause deaths, injuries, and damages to buildings and other structures. They may lead to a wide range of long term economic or social impacts. As such, they should be addressed with a proportionate measure of seriousness and concern. Governments should use the past as a lesson on addressing any future occurrences of these disasters. This report examines the scope of the earthquake phenomenon in New Madrid and Fulton city, Missouri. Earthquakes in New Madrid: When did it all begin? The winter of 1811-12 was not an average humdrum winter to the residents of New Madrid. If anyone had been keen to record the events of that season, the manuscript would probably have been rejected as being just too fanciful for compelling fiction. In deed, seismologists call it the greatest release of seismic energy is so short a time ever witnessed and recorded by human beings. A few individual earthquakes have been bigger. In a few instances perhaps they have been more numerous within a short span. However, never so many were so big in so short a time (Braile et al., 1982). The drastic events that took place on December 16, 18 16 indicate that catastrophic earthquakes do not occur in the western [parts of the United States alone. In the last two and half decades, seismologists have come to learn that strong earth quakes that occur in the central Mississippi Valley are not mere events but have occurred repeatedly throughout the geologic past.Advertising Looking for report on geology? Let's see if we can help you! Get your first paper with 15% OFF Learn More This area has come to be known as the New Madrid Seismic Zone (NMSZ) (Pratt, 2009). The zone occupies the southeastern part of Missouri and the southern part of Illinois. The NMSZ consists of a number of thrust faults stretching from Marked Tree in Arkansas, to Cairo in Illinois. Earthquakes that occur in the eastern or central parts of the United States are worse than those of similar magnitude in the western parts. For instance, an earth quake that occurred in San Francisco, California in 1906 had some magnitude of 7.8 measured on the Ri chter scale. It was experienced some 350 miles away in the center of Nevada. However, an earthquake of almost a similar magnitude that occurred in New Madrid on December of 1811 went to the extent of ringing bells in Boston, a city that is 1000 miles away from the epicenter. Such geographical disparities in the east and west are caused by the Rocky Mountains. The large earthquakes, which occur in the region notably, affect the New Madrid Seismic Zone. The closest areas that are also affected by the zone earthquakes are Arkansas, Tennessee, Kentucky, and Illinois (Weznger 213). The southwestern parts of Indiana and the northwestern Mississippi have also declared to receive extraordinary shaking from the region’s strong earthquakes. The latest New Madrid fault system covers an area of 120 miles, cutting across the Mississippi River, as well as Ohio River (Braile et al., 1982). Geology of New Madrid Seismic Zone The New Madrid Seismic Zone is found in the northern region of Miss issippi embayment. The latter is a broad trough full of marine sedimentary rocks that are dated 50-100 million years ago. The top 30 meters of sediment that is in the embayment comprise of sand, silt, and clay. They were deposited by Rivers Mississippi, White, Ohio, and St. Francis. The NMSZ is composed of faults that were experienced when the area currently referred to as North America broke up. This occurrence occurred approximately 750 million years ago (Penick, 2001).Advertising We will write a custom report sample on Scoping report for the earthquakes in New Madrid, and Fulton City, Missouri specifically for you for only $16.05 $11/page Learn More The main cracks formed resulted to the present faults that are found in the zone. The magma that was pushed from inside the rocks came at the surface and formed themselves into igneous rocks. The rift that was formed when the earth was splitting off remained as a region of weakness underneath the earth su rface. Later, yet another unsuccessful rifting trial left the area weaker than before, hence, creating more faults. The second occurrence of unsuccessful rifting occurred approximately 200 million years ago (Pratt, 2009). The reel foot rift was realized because of geological structures that emerged after every rifting attempt. The large rocks that are found underneath the earths surface in New Madrid are feared to be mechanically weaker than most of other parts of North America, due to the past fault that were created. Chart 1. The geology of New Madrid Seismic Zone Source: Tuttle, M., Associates. (2011). ‘The geology of NMSZ’. The underneath weaknesses, together with the effects of stronger rocks, allow the east west condensed forces to reinforce the old faults. Although there are several rifts that are experienced in most parts of North America, not all of them are associated with the modern types of earthquakes that occur in the area.Advertising Looking for report on geology? Let's see if we can help you! Get your first paper with 15% OFF Learn More For instance, the mid-continent rift system that starts from Minnesota and ends in Kansas may not be associated with any earthquake, as other processes may add to mechanical stress on the already existing faults (Braile et al., 1982). Some of the local processes that are suspected to cause earthquakes are downward pulling from underneath rocks that are below the fault. Other incidences include bending of the lithosphere because of continental glaciers melting. The earthquake experiences: a ground for further investigations Several suggestions are made concerning the heating that happen in the lithosphere, may result in making the big rocks inside more plastic. This heating may cause the concentration of compression force in the shallow underneath regions, where the faulting happens. There is also a model that describes local stress to happen because of a change in the passage of the mantle below the New Madrid Seismic Zone, due to sinking Carillon Plate. There are three types of tre nds realized when epicenters of modern earthquakes are presented in the form of a map. The first system of a trend is referred to as general northeast southwest. This trend is parallel to the drift of the Reel foot Rift in part of Arkansas. The second system of the trend is called southeast to northwest. This drift is experienced at the southwest part of New Madrid. The third system of a trend is known as northeast to northwestern. It extends to the farthest end of the Reel foot Fault (Penick, 2001). The New Madrid Seismic Zone recorded four of the largest earthquakes that have happened in North America. They were big earthquakes believed to be as large as 8.0. The largest earthquakes that were first experienced in this zone occurred between 1811 and 1812. The New Madrid Sequence is the overall effect of all the earthquakes that happened during that period. It has been always a challenge to measure the effect of one earthquake. The magnitude approximates and epicenters are based on the results of historical records, and this may vary from one period to the other. Earthquakes in the past or the recent ones that have happened for the last 10000 years have been caused by faults, which are not always micro seismically active. According to some of the researches done, it is evident that quiet faults are at times dangerous than the active ones. High built up stress blocks both sides of the fault, hence hindering the occurrence of micro seismic earthquakes. This process happens before the major rupture of the fault happens; investigations are still ongoing to define whether such types of faults do happen in New Madrid Seismic Zone (Weznger, 2010). Further investigations are required to proof, as it would be hard to locate such incidences. For the last 10000 years, people in this zone felt more than two thousand quakes. Crude seismograph instruments were used to detect these quakes, and most journalists managed to record these events in personal journals (Pratt, 2009) . In the central United States, rocks that are found there are hard, cold, and dry. The presence of such rocks makes earthquake in this region to be strong than the earthquakes that happen in California as well as in other areas. The earthquakes, which happen within the New Madrid Seismic Zone, cause damages, which are approximately 20 times larger than in other areas (Penick, 2001). The measurement challenge For many years, it has been a great challenge to estimate the recurrence of earthquake. With approximate locations, time and dates, and the size, it would be capable to provide a rough estimate of recurrence interval (Nixon, 2009)). Currently, some pale seismologists have provided people with information that two or more earthquakes of seven or more magnitude were experienced in the last 2000 years. They used some information to come up with a recurrence interval estimate of 3000 to 1000 years. It was estimated that, after 100 years, the New Madrid Seismic Zone would experience an earthquake of magnitude more than 6. These 100 hundred years were to be calculated since 1812, but this time has already elapsed. The estimates are not always accurate, and that is one of the major issues, which require further investigations. Effects of the 1811-1812 New Madrid earthquakes The 1811-1812 earthquakes in the New Madrid Seismic Zone had many effects. The most obvious of these include sandy blows. These were due to the upsurge of water and sand to the ground surface. This phenomenon is known as earthquake-induced liquefaction (see chart below). This is the process by which a saturated soil substantially loses its power and strength due to a stress that is applied to it by an earthquake shaking. This makes the soil to act like a liquid. Soil liquefaction leads to a number of cascading hazards such as floods, landslides, and river debris (Tuttle Associates, 2011). During the 1811-12 earthquakes, sand blows formed over an extremely large area measuring about 10, 400 s quare kilometers. The effects of these were experienced 200km away in the northeastern part of the NMSZ. Even today, sand blows are visible in the New Madrid region. They appear as sandy patches that have a light color in cultivated fields. Chart 2. Sand blows and the New Madrid earthquakes of 1811-1812. Source: Tuttle, M., Associates. (2011). ‘Sand blows and the New Madrid Earthquakes of 1811-12’. Recent earthquakes of medium magnitude have led to loss of lives and destruction of property worth billions of dollars. For instance, in Northridge, California, an earth quake of magnitude 6.7 led to the death of 33 residents, and destruction of property worth $20 billion. In the following year, an earthquake of magnitude 6.9 occurred in Kobe, Japan killing 5, 500 people and destroying property valued at $100 billion (Penick, 2001). These statistics indicate that there is a need for the inhabitants of New Madrid Seismic Zone to be prepared in case an earthquake of such med ium magnitude happens in the future. This is because earthquakes of medium magnitude are likely to occur than those of great magnitude. In deed, seismologists approximate the likelihood of the occurrence of an earthquake that is of magnitude 6.0 or greater within the next 50 years ranges from 25% to 40% (Weznger, 2010). If such a disaster happens, it is bound to affect more people than the incident that occurred on December 1811. This is because the population of the central Mississippi Valley was smaller compared to the current one consisting of millions of people. In addition, the calamity is likely to be dangerous because many structures in the area were not designed to withstand earthquakes as is the case in areas that are more seismic active such as California (Pratt, 2009). Earthquakes in Fulton, Missouri Chart 3. Welcome sign of Fulton City, MO Source: Citi-Data.com. (2011). ‘Welcome to Fulton signs’. Retrieved from http://www.city-data.com/picfilesv/picv25526.p hp Fulton is the largest city in the Kingdom of Callaway County. As of 2009, it population stood at 12, 814. According to the 2000 census, the average household income is $32, 625. Callaway water district provides a lot of employment opportunities for the residents of Fulton City. Other institutions that are of economic value to the city include Fulton State Hospital and Missouri School for the Deaf. According to the 2000 census, the average household income is $32, 625 (City of Fulton, MO., 2011). Geology of Fulton. The city is situated on a low-lying land. Missouri River is the defining physical feature in Mid-Missouri, and it surrounds the southwester border of Callaway County. There are three dominant soil types in the Callaway County. These are alluvium, sandy clay, and clay loam till soils (Chalfant, 2008). Just like the rest of Missouri County, the weather patterns in Missouri are not constant. There are both extremes of temperature. The county has experienced a number of na tural hazards in the history of its existence. These include floods, severe weather conditions, tornadoes, and hail. In the recent past, the most memorial natural hazard that took occurred in this county is the Flood of 1993. This flood affected a large portion of Missouri State causing a lot of damage on commercial properties, public facilities, transportation, as well as agriculture. The geology of Fulton is similar to that of the central region of the U.S. It consists of cold, dry and less fractured rocks. Although the probability of an earthquake is not high as in the case of New Madrid, any occurrence of the same will be more hazardous than it would have been the case in other regions such as California. In the recent past, a number of earthquakes have been recorded in the area. On July 31, 2005, an earthquake of magnitude 3.3 was experienced 43 miles from the city center. On March 30, 2001, an earthquake of magnitude 3.1 was felt 98 miles from Fulton City center (Citi-Data.com , 2011). The above statistics indicate that the risk of, although the magnitude of earthquakes occurring in the city may be small and do mot occur in the city centre, there is a high probability of such occurrences in the future. Nevertheless, the occurrence of earthquakes in Fulton is way below that of the entire Missouri state. However, this does not imply that the phenomenon is not an issue of concern to the city. Although earthquakes in this area have not been very destructive in the past as compared to that in New Madrid, any occurrence of earthquakes in this region can destroy the Callaway Nuclear Facility, hence cutting off the livelihoods of many residents who work in it (American Services, 2011). Summary of main findings Earthquakes are always occurring, with some being too small to be felt while others are large enough to cause irreparable damages. On average, major earthquakes happen once in a year. This will depend on the location of a place on the planet. However, more seismic active areas like the New Madrid Seismic Zone have high risks of experiencing hazardous earthquakes than other areas in the state of Missouri. This high probability is of great concern to Fulton city as it predisposes the latter to this risk. The duration of earthquakes is generally short compared to other hazards such as floods. It could be minutes, or even seconds. The main earthquake event lasts for a short duration. The foreshocks and aftershocks linked with a single geological shift can be detected weeks before or months later. This was the case with the December 1811-12 earthquakes that span for a period of three months until March the following year. The amount of destruction that results from an earthquake depends on several factors, one of them is strength. Earthquakes vary remarkably in their power. Some can be barely felt while others can knock one off their feet or buildings off their foundation. There are two principal methods of measuring earthquakes. These are the Richter scale and Mercalli Scale. The Richter scale is more famous than the Mercalli scale. It was formulated in 1935 by Charles F. Richter, a seismologist. The scale indicates ground motion in an earthquake. Its values range from 0 to 9 (see appendix). However, theoretically, the range can be higher. The numbers are logarithmic, implying that each whole number is ten times greater than the preceding whole number. For instance, the New Madrid earthquakes of 1811-12 were of magnitude (Heatwole, 2011). The second scale, the Mercalli scale, was developed in 1902 by Giuseppe Mercalli. The scale measures the intensity or violence of an earthquake in terms of damage caused to human-built structures. It is expressed by a series of Roman numerals ranging from I to XII (see appendix). An increase in the scale implies an incr4ease in intensity of the violence caused by the earthquake. Going by this scale, the New Madrid earthquakes of 1811-12 were so intense such that the Mississippi Riv er changed its course, and an island in the river disappeared (Feldman, 2005). In addition, new land arose, forests were cleared, and the ground rolled in visible waves that swept houses away, gardens, and fields. Nevertheless, few people perished during the incident due to the fact the area was sparsely populated then (Missouri Department of Natural Resources, 2011). Mitigating the risks of earthquakes: Prevention is better than cure The decision for mitigation of lifelines against seismic hazard is a quite complex issue as different institutions such as government, local authorities, lifeline companies, or the insurance industry are involved. In addition, the decision is further complicated since it is based on the results of the seismic risk assessment of lifelines which include various uncertainties owing to seismic hazard, vulnerability, performance, and loss estimation. Considering that earthquakes are a natural phenomenon little can be done to adjust the natural events system . As such, any mitigation efforts should be directed to human use systems (Balassanian, 2000). A number of practices can be handy in the mitigation of earth quakes. These include regulation of land use, education of the population about possible extreme events, as well as outfitting infrastructure tom meet local building codes. The readability of structures to withstand stress caused by earthquakes can be. Soil liquefaction caused by earthquakes can be mitigated through the installation of drains or use of deep, resistant pillars in construction (Keith Petely, 2009). Conclusion This report has explored the earthquake in Fulton and New Madrid. It is evident that these two are at a great risk of experiencing an earthquake in the near future. However, the frequency of another big earthquake in New Madrid or Fulton areas of Missouri is debatable. Nevertheless, the undeniable reality is that the region has a high seismic action. There is a need for education programs to enlighten the re sidents on the precaution measures that are highly required in the event of an earthquake. In addition, buildings in these two areas should take into account the vulnerability of the regions. As such, they should be enhanced by use of smart designs along with appropriate materials such as steel and reinforced-concrete. If history is anything to go by, residents of these areas should not throw caution to the wind as far as earthquake mitigation is concerned. They should take the appropriate measure to avoid a repeat of the events December 1811-12. Although an earthquake is a purely natural phenomenon, prevention is of prominence in these earthquake-prone areas. As they say, prevention is better than cure, or even, to be for-warned is to be for-armed. References American Services. (2011). Callaway Plant Profile. Web. Balassanian, S., et al. (2000). Earthquake hazard and seismic risk reduction. Berlin: Springer. Braile, L., et al. (1982). ‘An ancient rift complex and its relation to contemporary seismicity in the New Madrid Seismic Zone’, Tectonics, Vol. 1. Chalfant, M. (2008). Soil Survey of Callaway County Missouri. Web. Citi-Data.com. (2011). ‘Missouri’. Retrieved from http://www.city-data.com/city/Fulton-Missouri.html City of Fulton, MO. (2011). ‘Demographics’. Retrieved from http://fultonmo.org/about-us/demographics/ Feldman, J. (2005). When the Mississippi ran backwards: empire, intrigue, murder, and the New Madrid earthquakes. New York: Simon and Schuster. Heatwole, C. (2011). Geography for dummies. London: Wiley Sons. Keith S., Petely, D. (2009). Environmental hazards- assessing risk and reducing disaster, 5th ed. Michigan: Routledge. Missouri Department of Natural Resources (2011). Web. Nixon, J. (2009). â€Å"Facts about the New Madrid Seismic Zone.† Natural Resources. Web. Penick, J. L. (2001). The New Madrid earthquakes. Missouri: University of Missouri Press. Pratt, T. L. (2009) ‘How old is the NM SZ’. Web. Tuttle, M., Associates. (2011). ‘The geology of NMSZ’. Web. Weznger, B. (2010). The New Madrid Seismic Zone: Whose fault is it anyway? New York: Bibliogov. This report on Scoping report for the earthquakes in New Madrid, and Fulton City, Missouri was written and submitted by user GwenStacy to help you with your own studies. You are free to use it for research and reference purposes in order to write your own paper; however, you must cite it accordingly. You can donate your paper here.

Infographic How to Apply for College, Step by Step

Infographic How to Apply for College, Step by Step SAT / ACT Prep Online Guides and Tips The college application process can be a long and difficult journey for high school students. Organizing your application materials well in advance and paying attention to deadlines is critical. You should also start researching colleges earlier rather than later so that you can account for each school's specific application requirements. In this infographic, I've broken down the actions you need to take to be prepared for college applications starting at the beginning of your junior year through to your senior spring. Applying to collegeisn't as intimidating as it might seem! There are certain basic steps you will need to take beginning in your junior year. Ideally, you should take the SAT or ACT for the first time your junior fall to give yourself plenty of time to improve your scores before you apply to college. The early to middle part of junior year is also the best time to begin researching colleges. This ties into potentially retaking the SAT or ACT if you find that the colleges that interest you are looking for higher scores. In the spring of your junior year, it's a good idea to ask teachers if they are willing to write recommendation letters for you. Asking for letters early on will ensure that the teachers you've chosen are on board, and the letters themselves may turn out better since your teachers will have more time to think about what they want to say. In the summer before senior year, you can make your final college list and start looking at the specific requirements for each school. This is also a good time to prep for your last chance at standardized tests and begin thinking about your college essay. You should write a first draft of your essay in the summer so that you won't have to worry too much about it during the school year. When you're trying to fill out applications and manage your classes at the same time, the essay can seem like an overwhelming responsibility. Once your senior year starts, you should submit formal requests for recommendation letters to the teachers who agreed to write them for you in the spring. If you're planning on taking the SAT or ACT one last time, your final chance will be in October or November if you're applying early decision. Most early action and early decision applications are due by November 15th, and you will get back the decisions about a month later in mid-December. Regular decision applications are typically due around January 1st, but colleges have different policies for how late you can submit your SAT or ACT scores. Often, students are permitted to submit scores from tests taken as late as February, but make sure to look up schools individually to see what's allowed. You should be notified about the status of your regular decision applications by late March.All that's left after that is to choose your favorite college out of the schools where you were accepted. This might be the hardest part of the whole process (but in a good way)! What's Next? Are you interested in highly competitive colleges? Find out more about the most selective schools and how to ensure that you have the best chance of being accepted. If you're struggling to start writing your college essay, read this article to learn which prompt you should choose and how you can being the brainstorming process. Extracurricular activities will be an important aspect of your college application. Find out more about extracurriculars and why you should have them! Want to improve your SAT score by 240 points or your ACT score by 4 points?We've written a guide for each test about the top 5 strategies you must be using to have a shot at improving your score. Download it for free now:

Psychology Essay Example | Topics and Well Written Essays - 3000 words

Psychology - Essay Example They encounter serious kinds of attacks frequently while some overcome them with consummate ease, depending upon the nature of stress one has to go through over a period of time. Workplace stress also entails within it issues of anxiousness at work whereby it is regarded as another kind of mental anomaly, which tears down the mind and the body in a number of different ways. Workplace stress leads to different kinds of depressions within oneself on top. The employees start feeling alienated with the tasks and feel their bodies having all forms of aches every now and so often. These people also comprehend the pressures from their job settings which in reality are of a normal nature and have little bearing on them in the real sense. The pressure-exertion effect makes them feel more stressed at the end of the day, which then again is a very perilous thing. Workplace stress can be reduced when employees know that the task they are putting their best energies at, are worth the shot and in the end, the same will help them to grow exponentially. In fact they must be apprised of their hard work and the rewards that they get. This is indeed a nice gesture which means a lot on the part of the hard working and committed employees and workers (Harmon 2003). The hard working employees should balance their work commitments with their physical and mental needs as 100 percent commitment can only be made possible when there is zest and enthusiasm from within and not when a person is made to do one thing or the other by force or against his wishes. The reason why one should believe this approach will work is because in the initial sense, it will build a strong rapport between the firm and its employees and also it will convey a strong message that the organization does not compromise on the needs of the employees who are working for it day in day out just for having that extra bit of work completed by them (Bergman 2003). It also means that the organization is thorough and profes sional in its approach and is not willing to surrender in a rat race when the talk goes out loud of competing within the relevant industry or even with companies just for the sake of nothing but competition. The intensity within organizations is pretty much understandable but the madness should not be substituted on the part of the employees and getting work done out of them so that the figures could be reached and new records could be broken within the shortest possible time is nothing but insanity to say the least. Other useful workplace stress removing remedies are accounted for in the form of exercising regularly, having an intake of healthy diet, taking proper sleep, developing trustworthy social support regimes and more than anything else enjoying quality family time (Linton 2000). The physical and psychological implications thus have direct and serious effects on the way the employees look after their work tasks and thus the bottom line remains all jammed up for a number of r easons – most of which are related with stress in one way or the other. It is true to state that workplace stress affects employees at all levels which could include the physical, emotional, cognitive and behavioral stages. The physical indications entail the speech difficulties and complexities, headaches, ulcers, infertility issues, fatigue and sudden weight loss and

Significance Of Teamwork In Organizational Competitiveness Case Study - 1

Significance Of Teamwork In Organizational Competitiveness - Case Study Example Members of the teams benefit from knowledge sharing, which is important in career development and workplace learning. Teams may or may not be effective depending on their formation and leadership. Successful teamwork is characterized by a high team spirit in which every member is contented and willing to take part in accomplishing the tasks. Moreover, the employees working in a successful team tend to be enthusiastic about identifying with it. They also demonstrate loyalty to its leadership as well as among each other, as well as a willingness to work together. Everyone is usually focused on the accomplishment of a shared vision and owns the goals of the team. For this reason, organizations that promote strong teamwork are able to maintain competitiveness by offering effective services to the customers. Beardwell & Holden (2001) observe that customers are attracted to an organization in which they are served in a similar manner regardless of the staff member that deals with them. This paper presents a critique of the view that teamwork is always positive. It highlights U.S and UK organizations that exhibit teamwork in the workforce. It also compares these organizations with others that operate in the international markets Many organizations engage in projects targeted at particular target segments in the market and hence the strategies for the accomplishment of particular organizational goals need to be understood by all the people involved among the workforce. For example, if an organization has engaged 12 people as marketing representatives, it is important for them to work as a marketing team that is composed of employees with similar objectives.

Being young is just difficult Essay Example | Topics and Well Written Essays - 1250 words

Being young is just difficult - Essay Example Since its publication in 2007, Beah’s book has gained significant popularity given that there are a lot of meanings as well as lessons that can be drawn from it. It is not just a story about childhood of a young man who lived in a certain place and certain situation; it is an example of a real story where children are seen to be converted to act like killing machines where the orders to kill people are driven by the owners of these machines and drugs are used as the catalyst to fuel the situation. This particular kind of situation happened to many children in Sierra Leone and the author of this book, Ishmael Beah, personally experienced it. This can happen anywhere else other than Sierra Leone in as far as humanity is absent. This book describes the difficulties faced by young people who are forced to be part of the fight against tyranny by those in authority. This is despite the fact that they are still young and still need to be carefully looked after by their parents.