What Is Human Reproductive Cloning Essay Example | Topics and Well Written Essays - 2000 words

What Is Human Reproductive Cloning - Essay Example As the report declares the most prominent theoretical source of objections in the ‘deontological’ school of thought is the moral philosophy of Immanuel Kant, the German eighteenth-century thinker who stressed the ideas of ‘transcendental’ freedom and autonomy. To define his idea of the transcendental autonomy of human reason, Kant presented several formulations of what he called the ‘categorical imperative.’ This is the moral law that he thought people should obey without exceptions. The general idea and two specific formulations of this overarching rule, and see how they can (or cannot) be employed in objections to human reproductive cloning. This paper discusses that Kant’s first formulation, which is of more use, was â€Å"Act only according to that maxim whereby you can at the same time will that it should become a universal law†. The definition of the goodness of genetic diversity does make some sense, but it does not support the Kantian objection to cloning. We can permit cloning in cases where people cannot have children by any other means without allowing it to become the only way of making babies – and without disturbing the human gene pool in any way. Besides, it could be argued that whatever accidental advantages the variety of genetic constitutions has had in the past could in the future be secured by considered genetic enhancements. The more Kantian way to proceed is to say that genetic diversity is good, because it is natural, or intrinsically linked with human reproduction.

Final Exam Part 2 Essay Example | Topics and Well Written Essays - 750 words

Final Exam Part 2 - Essay Example The emergence of Conflict Resolution as an academic discipline was, actually, a culmination of multi-disciplinary studies in social sciences in an effort to find ways and means of averting the occurrence of another world war, after the Second World War (Ramsbotham, Wooodhouse, & Miall, 2011). As it can be seen, therefore, from the understanding of the concept, Conflict Resolution, and the reason that led to the emergence of this discipline as a fully-fledged academic discipline, the main importance of Conflict Resolution is to keep and to maintain peace among warring parties with differences that cannot effectively be solved through the court systems. Conflict resolution seeks to ensure that people co-exist peacefully with one another. Importance of culture in the field of conflict and resolution, and its relation with the idea of peace building Culture is deeply rooted in our past experiences, and as such, it can be viewed as a derivative of our experiences (Avruch, 20). Culture, th erefore, having been fashioned by our past experiences has great experience in our world view. Our world view is determined to a big extent by our cultures, and therefore, culture is quite important in conflict resolution. Culture can sometimes be used as an ideology to accelerate or to cause conflicts (Avruch, 16). In such a situation where a conflict arise due to misuse of culture for egocentric gains, the most effective way to resolve such a conflict is to analyze the cultural ideology that is used to cause the conflict, and after the analysis, you lay bare the inadequacies and the fallacies in the ideology. This will help a great deal in resolving the conflict. Culture can also be used to cause what Galtung calls, cultural violence (Galtung, 39). This happens when one uses their culture to justify their violent acts against other people. This will definitely lead to conflicts. Resolving such a conflict requires an analysis of the culture that is used to justify violence against other people, and after the analysis, the false ideas inherent in the culture should be exposed and logically critiqued. Cultural knowledge, therefore, is quite important in the field of Conflict resolution for it helps us in solving conflicts and maintaining peace. It is therefore related with the idea of peace building. Importance of the Nested Theory of Conflict in the field of Conflict Resolution Nested theory of conflict was propounded by Maire Dugan (Dugan, 14). Dugan propounded the theory after realising that some of the commonly used methods in conflict resolutions did not offer effective solutions, but rather, simplistic solutions that did not take into consideration the root causes of the problems. Dugan, therefore, came up with a nested model of conflict that is based on the structural nature of the conflicts. In the nested model, Dugan identified three levels of conflict. These levels are, issue specific level, relational level, structural subsystem level, and structural system level. The levels are interrelated and are arranged in such a way that the narrow types or levels of conflict are nested within the broader level. For instance, the level of issue specific is nested in all the other three levels, while structural sub-system level is nested only in the structural system level only. The issue-specific category of conflict is the simple issue based conflicts. Relational conflicts are conflicts that have their roots in our relation patterns on our attitudes towards

Causes of Earthquakes

Causes of Earthquakes Shreyas Patel The Earthquake ABSTRACT The purpose of this paper is to gain the knowledge on natural occurring disaster. I will be writing about the earthquakes and mainly how the earthquakes are formed all over the world in the earth crust. In this article, I will be elaborating the reasons of earthquakes. The impacts of an earthquake will also be illustrated with pictures which explain that how they were caused. And finally, I will include the mitigation for earthquakes, i.e. the measures that can be taken to prevent from the earthquakes and minimize the damage caused when they strike. All key factors and illustrations surrounding the causes, effects, and solution will be explained in detail to provide a complete understanding of â€Å"how earthquakes are formed†. After devoting my time in this research, I clearly understand the concept of how earthquakes are formed and how they occur over the period of time. I found that sea bed increases in surface area when the magma drills up and eventually cools down. The formation of our continent that occurred from 400 million years ago, the rigid terrain in the dessert and the tallest mountain that we have today are all evidences of plate tectonics which caused the earthquakes to occur. I also found that convection cells create hotspot in which magma drills up during a divergent boundary. The solution from experts all refer to common goal of studying landforms where earthquakes are most and collecting the seismographic material over many decades in order to get the data to predict an estimate of when the next earthquake may strike. Solution is to prepare for the worst and I have carefully outlined my solution in this report. The solution can also include international ties between countries. Any country hit by an earthquake can get a relief through charitable donation to help during difficult times. Introduction What is an earthquake? The earthquake is the sudden movement of the ground that discharges elastic energy stored in the rocks and generate seismic waves. These elastic waves radiate outwards from the â€Å"source† and vibrate the ground. What are the earthquake seismic waves? A seismic wave means the transferring of energy with vibrations from one spot to another within the earth. There are different types of waves but we are interested in only two types of seismic waves: P (primary) waves that are similar to sound waves, and S (secondary) which is a type of shear wave. Within the earth, P waves travel through the solids and the liquids, whereas S waves can only travel through the solids. Figure1 Source: http://www.factmonster.com/dk/encyclopedia/earthquakes.html Figure 1 describes the waves that radiates from the center of the focus point of earthquake. It gives the way that earthquake take place through the sudden movement of tectonic plates and causes the waves to spread from the epic centre. The speed of the earthquakes is not constant but it varies with many factors. It is mostly affected by the depth and the type of the rocks. Figure 2 shows the P type and S type seismic waves. In P type, the compressed rock propagating in the same direction as the compression. Also, the P type wave moves faster than S type. In S type, liquid matter prevents S waves from spreading. It moves up and down or side to side. Figure 2 Source : http://www.earth.northwestern.edu/people/seth/B02/lectures/Seismology/pswaves.htm Causes of an Earthquake Earthquakes are caused by the movements of plates under the surface of the earth’s crust. Movement between two plates is not smooth and it causes elastic energy to gradually build up over time. When we feel the ground is moving or shaking this energy is released as seismic waves from the epic centre. They usually occur on the boundaries of the plate margins which cover the earth like an egg shell. There are two main causes of earthquakes. Firstly, earthquakes can be linked to explosive volcanic eruptions. When a volcanic eruption occurs, lava spreads across the land (Skinner and Murck, 175). These are very common in the areas of volcanic activity where they either follow or accompany eruption. Figure 3 shows the image of volcanic earthquake eruption occurs and spreads the lava around it. Figure 3 Source: http://www.cbc.ca/news/technology/volcanoes-drop-hint-before-deadly-eruptions-study-1.1063506 Secondly, earthquakes can be triggered by tectonics activity related to plate margins and faults. The majority of the earthquakes occurring all over the world are caused by this process. Convection cells under the earth’s crust create a push and pull mechanism and forces the plates to move creating interaction between the plates. Figure 4 Source: http://www.globalchange.umich.edu/globalchange1/current/lectures/evolving_earth/evolving_earth.html Figure 4 shows the process of plate tectonics occurrence. The plate tectonics tells us that the earth’s crust is broken into two different types of plates known as the oceanic and continental plates. These plates can slides over each other and are floating over the uppermost layer of the mantel and convection cells. The plates are in constant motion. Along their margins where they usually interact, important process such as the formation of mountain belts, earthquakes and volcanoes take place. Figure 5 Source: http://sichuanheartquake.wordpress.com/ Figure 6 Source: http://thewatchers.adorraeli.com/2011/03/13/the-failure-of-plate-tectonics/ Figure 5 and Figure 6, both are the same which describes the procedure of the causes of an earthquake. If we carefully observe both the Figure, we see the numbering that describes the way to take place. We see that the less dense oceanic plate collides with the continental plate (more dense) and sinks down and melts due to the high temperatures of the mantle. Also, if we observe the subduction zone, that’s what really, causes an earthquake. It is the constant colliding of the two plates that causes an isostatic rebound and stress to release the energy. Heat from the mantle causes the plates to grind against each other along plate margins commonly known as faults. The convection cells help the plates to move in a particular direction and since the plates are not smooth, they usually find their motion blocked. As a result, due to the tension and stress builds up, the fault breaks, energy is released in the form of seismic waves. Figure 7 Source: http://www.age-of-the-sage.org/tectonic_plates/boundaries_boundary_types.html Figure 7 shows the different types of plate boundaries. From the above figure, (1) represents the Divergent where the plate move away from each other, leaving a gaping hole for the hot spot. This usually leads to volcanic activity and new land formation. (2) Represents the Convergent which is most destructible. High chances of volcanic activity are expected due to the subduction zone. The melting of the less dense oceanic plate sinks along with water which evaporates and moves up with boiling magma. (3) Represents the Transform where the plates, which are not smooth at all, slide alongside each other causing massive vibrations and with enough build up of energy can also cause the huge earthquakes. Effects of an Earthquakes The effects of earthquakes towards the nation can be described in two categories: long term and short term. Long term effects can be the formation of new land, mountain folds and the deep trenches formed by the upwelling of magma at the hot spot. The short term effects can be the seismic waves that are generated during the impact, the broken pipe lines, landslides, mudslides, and the collapsing of the buildings. Tsunamis: Figure10 Source: http://www.howitworksdaily.com/wp-content/uploads/2011/03/Tsunami-formation-large.jpg Figure 11 Source: http://www.giglig.com/environment/tsunami Figure 10 shows the formation of the tsunami waves due to the movement of the plates that cause the earthquake to occur in the sea. Figure 11 shows the image of tsunami that takes place in Japan in 2011. When an overriding plate along subduction zone suddenly breaks free, it moves upwards raising the sea floor and the water above. The waves move outwards in ever-expanding circles. As they approach land, water recedes from the shore. They are able to cross the entire oceans without a great loss of energy. Landslides: Figure 12 Source: http://landslides.usgs.gov/research/inventory/utahttp://landslides.usgs.gov/research/inventory/utah/h/ Figure 12 and Figure 13 shows the views of landslides takes place. Landslides are rocks, earth, or debris flows on a slope due to gravity. During an earthquake, the seismic waves can shakes the ground, enough to cause a landslide, easily on a slope. The effects can be devastating, as the debris won’t stop tumbling down until a flat plain is reached or an obstacle bigger than it is encountered. Buildings and structures: Figure 13 Figure 14 Source: http://sichuanheartquake.wordpress.comhttp://sichuanheartquake.wordpress.com// Figure 13 and Figure 14 shows that effect of earthquakes on the buildings and roadways. After an earthquake, damages occur to buildings, bridges, roads and everything that stand on its own. As a result, large numbers of people may be died, injured or homeless in the aftermath of an earthquake. New land Formation: Figure 15 Source: http://science.howstuffworks.com/nature/natural-disasters/volcano2.htm When the divergent boundaries moves away from each other, magma rises up and cools down to form a new landform. It can form on the land and on the sea bed, increasing the surface area as shown in Figure 15. Solution of an Earthquake Over many years, researchers and scientists have tried to find at least a reasonable prediction of an earthquake to when it will occur, however, it is a natural disaster that can strike at any point in time that look how big the earth surface is. So, the data collecting from every fault margin for epic centre is physically possible. Moreover, we cannot physical see an earthquake approaching, it’s just energy (seismic) waves travelling that can compress and shear. Although, there are several ways to be alerted and predict from the incident to be happen. These ways are as follows: Richter scale: The moment an earthquake strikes, the Richter scale extremely sensitive to vibration thereby it will send signals to an alarm and also record the data on a seismograph for the calculation of magnitude. Prediction: In area like the â€Å"Ring of Fire†, is known for volcanic activity. Also, the earthquakes have been recorded along with event that took place. So, there is always a probability of an earthquake in a certain area since it keeps occurring in the same area is clearly an indication that it is very likely that an earthquake can happen. Drills: Training session would be given to teach people that what to do during an actual earthquake take place. Earthquake-resistant buildings: This type of buildings can withstand a certain amount of magnitude and can cope with the seismic waves. The design of buildings depends on providing the building with strength, stiffness and inelastic deformation capacity which are great enough to withstand a given level of earthquake as shown in below images. Figure 16 Source: http://forum.strukts.com/discussion/420/earthquake-resistant-construction/p1 Statistics of an Earthquake Figure 18 Source: http://earthquake.usgs.gov/regional/neic/neic_bulletins_figures.php#figure1 As shown in the above Figure 18, According to the U.S. Geological Survey National Earthquake information Center, there is an increasing in the amount of earthquake during 19th century. Moreover, the magnitude threshold of an earthquake is also estimated across the whole world. Figure 19 shows the magnitude of an earthquake versus different year. Figure 19 Source: http://earthquake.usgs.gov/earthquakes/eqarchives/year/graphs.php Conclusion and Recommendation In my opinion, I believe that finding exact solution of earthquake still needs time to evolve, as it is hard to predict that when an earthquake will strike. It is obvious that prediction can be made from the relevant occurrences of that same activity, but still will not be accurate enough to evacuate millions of people and move then to safe place. At last, I do not believe that we can stop earthquakes, not even in millions of years. It is something naturally unique that cannot be stopped. The only option is to move away from the regions which are prone to earthquakes regularly and to evacuate people who reside near volcano and prepare for the worst case situation until the things can be reasonable fixed. Bibliography Skinner Brian J., Murch Barbara W. â€Å"The Blue Planet: An Introduction to Earth System Science†. United States of America: Library of Congress Cataloging in Publication, 2011. Page 175.Print. http://7bluec1-2012.wikispaces.com/Glossary http://www.bbc.co.uk/newsround/14652682 http://www.astronomynotes.com/solarsys/s8.htm http://www.essaseoutras.xpg.com.br/vulcoes-em-erupcao-as-fotos-mais-incriveis-da-furia-da-natureza-veja/ http://www.enchantedlearning.com/subjects/dinosaurs/glossary/PlateTectonics.shtml http://dirtyclassroom537.blogspot.ca/2012/05/plate-tectonics-caroline-burdick.html http://thewatchers.adorraeli.com/2011/03/13/the-failure-of-plate-tectonics/ http://www.suu.edu/faculty/colberg/hazards/platetectonics/platetectonics.html http://www.age-of-the-sage.org/tectonic_plates/boundaries_boundary_types.html http://www.examiner.com/slideshow/japan-earthquake-tsunami#slide=2 http://news.nationalgeographic.com/news/2011/03/pictures/110315-nuclear-reactor-japan-tsunami-earthquake-world-photos-meltdown/#/japan-earthquake-tsunami-nuclear-unforgettable-pictures-wave_33291_600x450.jpg http://kids.britannica.com/comptons/art-138177/A-landslide-triggered-by-an-earthquake-destroyed-part-of-a http://coastalcare.org/2011/04/japan-quake-caused-surprisingly-severe-soil-collapse/ http://ks3geoblogbytes.wordpress.com/year-7/ http://www.bbc.co.uk/science/earth/surface_and_interior/lava http://mceer.buffalo.edu/infoservice/reference_services/adveqdesign.asp http://earthquake.usgs.gov/regional/neic/neic_bulletins_figures.php#figure1 http://earthquake.usgs.gov/regional/neic/neic_bulletins_figures.php#figure4 http://inventors.about.com/od/qrstartinventors/a/Charles_Richter.htm http://articles.timesofindia.indiatimes.com/2006-03- 28/india/27831302_1_tsunami-scientistsearthquake http://earthquake.usgs.gov/learn/topics/plate_tectonics/rift_man.php http://myweb.cwpost.liu.edu/vdivener/notes/subd_zone.htm http://kobeshakes.wordpress.com/2010/03/26/kobe-shakes/ http://internalenergy.blinkweb.com/ http://www.ussartf.org/landslides.htm http://www.exploratorium.edu/faultline/activezone/slides/pangea-slide.html

Bibliography of Geoffrey Chaucer ::

Bibliography of Geoffrey Chaucer Geoffrey Chaucer was born in the early 1340's, in approximately 1343. Little is known about Chaucer's early life. According to Microsoft Encarta, "there is relatively strong evidence to support the fact that he attended one of the three grammar-schools: either St. Paul's, St. Mary-le-Bow's, or St. Martin-le-Grand's. The next reliable bit of data places him, at around the age of fourteen, as a page in the household of the wife of Prince Lionel, the third son of Edward III. He apparently held this position for a long time" (Mirosoft) According to Grose, "Chaucer's first foray into the King's Business appears in October of 1360, when he couriered letters from the Calais to England during peace negotiations there. For this service he held the official title of clerk of the king attached to the person of Prince Lionel. In this way, Chaucer began to service to his king. In 1368, Chaucer was awarded a royal pension for life, indicating a long and valued service to his liege" (Grose 23). He served as sort of jack-of-all-trades. The only known facts about Chaucer's life between 1358 and 1367 are that he was imprisoned in France during the Hundred Years War and was ransomed in March 1360, for rather large sum. In this time Chaucer also married Philippa Roet, lady-in-waiting to the queen. She bore at least two children. Between 1368 and 1367, Chaucer undertook nearly a dozen diplomatic missions to Flanders, France and Italy. Many were important; indeed many were so secret that they were not mentioned in the histories of the time at all. In 1381, Chaucer was sent to deal with marriage negotiations Bibliography of Geoffrey Chaucer :: Bibliography of Geoffrey Chaucer Geoffrey Chaucer was born in the early 1340's, in approximately 1343. Little is known about Chaucer's early life. According to Microsoft Encarta, "there is relatively strong evidence to support the fact that he attended one of the three grammar-schools: either St. Paul's, St. Mary-le-Bow's, or St. Martin-le-Grand's. The next reliable bit of data places him, at around the age of fourteen, as a page in the household of the wife of Prince Lionel, the third son of Edward III. He apparently held this position for a long time" (Mirosoft) According to Grose, "Chaucer's first foray into the King's Business appears in October of 1360, when he couriered letters from the Calais to England during peace negotiations there. For this service he held the official title of clerk of the king attached to the person of Prince Lionel. In this way, Chaucer began to service to his king. In 1368, Chaucer was awarded a royal pension for life, indicating a long and valued service to his liege" (Grose 23). He served as sort of jack-of-all-trades. The only known facts about Chaucer's life between 1358 and 1367 are that he was imprisoned in France during the Hundred Years War and was ransomed in March 1360, for rather large sum. In this time Chaucer also married Philippa Roet, lady-in-waiting to the queen. She bore at least two children. Between 1368 and 1367, Chaucer undertook nearly a dozen diplomatic missions to Flanders, France and Italy. Many were important; indeed many were so secret that they were not mentioned in the histories of the time at all. In 1381, Chaucer was sent to deal with marriage negotiations

Police Management Organizing, Planning, Controlling, Leading

March 28, 2012 Dear colleagues: To prepare for learning Motivational Interviewing in the healthcare field, we’d like to start off with a pre-test of your current knowledge. Cut and paste this url address into your websearch engine http://www. ceuuniversity. com/emc/emctesting. html It will take you to an â€Å"interactive† on-line test on Motivational Interviewing. There are 34 questions. At the end of the test you click on submit. It will identify – by number(s) – which questions you scored incorrectly. Write those numbers down.Send them in an email back to Tammy Strickland (for medical staff) or Frank Heitmann (for clinical staff). The reason we need the specific numbers of the questions you answered incorrectly is to see if there are patterns we can address by more focused training. The results will be aggregated – so no one will know anyone else’s score – and we’ll give all of you a report on the results. Secondly, identify your learning preferences. Do you prefer we do one or more of the following: Send you reading material?Send you web url addresses of youtube clips showing actual MI sessions? Send you web url addresses of youtube clips of Power Point reviews of MI / MI techniques? Let you join a group watching one or more DVDs on MI? Or be in a discussion group to role play MI skills from a set of very-common-to-us scenarios? Or ______________________________ (some other preference of yours) This is due no later than Wednesday April 11th (but earlier responses are much appreciated). Best bet is the materials will go out to you as soon as you email your test results.

Managerial Accounting Essay

To Mr. George Friedman and Bill Compton, here are some options on ways to operate base of household incomes. Below are various ways to decide which might best fit in your organization. â€Å"Managerial skills are important in an organization and in leadership, especially managerial decision making. These help achieve the goals of the organization and harness the potential of everyone inside the organization† (Managerial Skills, n.d). The fee for food is $1.25 per student each day. Staff will received a 10% benefit on their salaries in addition $200 for the benefit programs. Variable supplies are $1 per student each month. Step costs are salaries for instructors, averaging $1,600 per instructor for each class. â€Å"As opposed to fixed costs, which remain constant, these costs arise in direct proportion toa business output, increasing and decreasing along with the volume of production† (Schneider, 2012). Experiencing a new class added would be beneficial due to the profits increased by $355. Whatever case of profit adding to the revenue helps Friedman and Compton childcare center. â€Å"A business can have higher revenue, but if the costs are higher, it will show no profit and is destined to go out of business when available capital runs out. Managing costs and revenue to maximize profit is key for any entrepreneur† (Davidson, n.d). If the tuition remains the same the infant care class will be taking, the division would contribute $615 to net income. According to Lynch & Williamson, understanding what makes a profit is important (Lynch, Williamson, 1984, para 2). Although the school may be having some problem with increasing revenue, however, containing the new infant class could assist with the cash flow problem. Reference Davidson, E. (n.d). What are cost, Revenue and Profit Important? retrieved website http://smallbusiness.chron.com/cost-revenue-profit-important-11952.html Lynch, R. & Williamson R. (1984).Accounting for Management, Planning, and Control, Tata Mc-Graw Hill Publishing Co, New-Dehli Managerial Skills (n.d) Decision Making Critical for Managers retrieved website http://www.managerialskills.org/managerial-skills-decision-making/ Schneider, A. (2012). Managerial Accounting: Decision Making for the Service and Manufacturing sectors. San Diego. CA, Bridgepoint Education.