Mendocino Triple Junction Free Essays

The deformational chronicles of the tectonic plates is examined from the standpoint of movement of the numerous faults bounded by the structural topography and environment and by the fault kinematics connected with the lately industrialized San Andreas transform margin. Accumulation and subduction are continuing underneath the continental margin north of the Mendocino fracture zone, with the linkage from the San Andreas fault system from the south. The continuous deformation due to the interactions among the Gorda, Pacific, and North American plates are collectively called the Mendocino Triple Junction. We will write a custom essay sample on Mendocino Triple Junction or any similar topic only for you Order Now The Mendocino Triple Junction stands for the setting of extreme change in plate tectonic processes from the convergence in the Cascadia subduction (north of the Mendocino Triple Junction) and the translation in the San Andreas system (south of the Mendocino Triple Junction. The abrupt changes form this tectonic processes resulted in the dramatic change in the thermic region in North America and the evolution in the lithosphere formation in the said region (Dickinson and Snyder, 561; Lachenbruch and Sass, 195-197; Zandt and Furlong, 377-378). The unstable intersection of the fault zones called the Mendocino Triple Junction divided the Pacific region, and North America, including North California. The meeting point The Mendocino Triple Junction is an unstable triple junction located in the North California west coast that is comprised of the intersection of the Pacific Plate, the North American Plate, and the Gorda Plate (Oppeheimer et al. 1666). The junction has complex plate activities due to seismic destructive above 6.5 in magnitude earthquakes that occurred over the past 100 years (Dengler et al., 48-50). The positioning of the Mendocino Triple Junction has transferred from its original location in the Los Angeles latitude to Cape Mendocino over the last decades. (Jachens and Griscom, 9380-9385).    One of its junctions, the San Andreas Fault, is located in the northwest-southwest portion of North America and the Pacific. The Pacific Plate moves northward simultaneously as the North American Plate moves to another region to collide with the Pacific Plate (Henstock, doi:10.1029/2001JB000902). The precise location of the San Andreas Fault is not established because of the complexities of the area (Simlila, 1402). Since the year 1800, statistics have shown that seven earthquakes have taken place with the least of magnitude four in the scale (Kelsey and Carver, 4799-4811). Another junction in the Mendocino group is the Cascadia subduction zone that is located north of the Mendocino Triple Junction. The 15-degree subduction angle continues to escalate as the depth of the subducting plate increases (Dengler et al., 45). Earthquakes in this area occur after 300 to 560 years, depending upon ruptures if the zone crossing point (Clarke and Carver, 190). The last area to be included in the Mendocino Triple Junction is the Gorda plate. The eastward movement of the Gorda Plate caused a clockwise movement in the Juan de Fuca plates, a plate formerly part of the Gorda region. The Mendocino zone remained still while the Gorda Plate repositions itself and interacts simultaneously with the Pacific Plate, therefore, increasing its deformation over time (Stoddard, 11527-11529). The Mendocino Fault is a zone located between the Pacific Plate in the south and the Gorda Plate in the north. The lateral movement of this fault contributed to seismic activities in Cape Mendocino, extending to the coast of the Gorda Plate. Earthquakes have been reported along the Mendocino Fault in 1994 as the most recent and massive tectonic plate movements with an intensity of 7.4 (Dengler et al., 45-50). In this actively deforming area, imbricate thrusts and the axes of folds overlying blind thrusts in the accretion prism offshore are oriented west-northwest and project southeastward  to align with several moderately low- to steep-dipping faults onshore. In the onshore region, the rocks bounded by these faults correspond to increasingly more distal parts of the uplifted accretion margin from northeast to southwest. The underlying problem is then rooted in the steep-dipping Pacific-North American plate boundary and to be related to ongoing northward propagation of the San Andreas movement. The area south of Cape Mendocino is significantly associated with the Pacific-North American faulting and the transformation of the plate boundary. The Future of Mendocino Triple Junction: The history of the activities in the Mendocino Triple Junction can be a potential benchmark for the cause and intensity of future earthquakes, tectonic plate ruptures, and ground breakdown. The rupture in the plates is the immediate effect of the activities happening in the Mendocino Triple Junction. Ground shaking can deliberately have an effect to structures, which is measured in the logarithmic scale to determine the intensity of the earthquake. Ground shaking is accountable for most loss of life and man-made property destruction throughout an earthquake so the importance of historical evaluation and earthquake assessment can help in the improvement of building and architectural designs and standards. The shaking intensity during an earthquake is dependent on the position of the land area hit by the massive ground activity, the type of soil and the slope of the vicinity, and its distance from the earthquake’s epicenter. Seismologists have monitored that a number of regions tend to repetitively encounter robust seismic trembling than other zones. This is due to the ground beneath these regions is comparatively soft than the other parts of the district. Soft soils intensify and amplify ground Soft soils also intensify shear waves, creating a more hazardous and damaging effects on any structure lay on the ground. Individuals living in the area that have experienced strong earthquakes will be likely to suffer strong earthquakes in the future depending upon the distance of the region to the epicenter (source) of the massive ground shaking. Amplification is caused when a seismic wave moves through subsurface materials and is amplified to produce relatively higher horizontal and vertical motion. In contrast, bedrock has a tendency to dampen seismic waves and therefore reduce ground motion. About one-quarter of the entire earthquake energy released in California during historic times has occurred along the Humboldt County coast. The size, location, and frequency of past earthquakes give an indication of what to expect in the future. Strong earthquakes with epicenters onshore have recurred about every 20 years. Since the 1870s, the largest of the historic seismic activity in the area of the Mendocino Triple Junction reached a magnitude of 7.2, which took place in 1923. The Northern Coast affected areas have been the focal point in the Gorda Plate activity. The recurrence of the earthquakes in this area occurs every two years.   Neighborhood in the coastal expanse from Cape Mendocino to Eureka has been smashed into frequent ground shaking than the remainder of the Humboldt County. Earthquakes have hardly ever affected Northern Humboldt County in history. On the other hand, because the historic documentation is comparatively transitory, regions not distressed in the past may even be at danger. Massive and huge earthquakes have been a part of the lives on the north coast so residents ought to take measures to get ready for any earthquakes to come. Up to date earthquake activity consists of several large-scale happenings in the Cape Mendocino district. Three powerful earthquakes hit Cape Mendocino area, with magnitudes  of 7.1, 6.6, and 6.7, respectively , in 1992. A strong upheaval set upon the north coast in the Cape Mendocino area with a magnitude of 5.6 last January 1997. The earthquake was situated on the Mendocino fault extremely close to the Mendocino Triple Junction. The United States Geological Service (USGS) set up new building codes in preparation for the severe earthquakes in the Mendocino Triple Junction belt. â€Å"Building codes provide the first line of defense against future earthquake damage and help to ensure public safety,† said the USGS.   According to the records of USGS, historical accounts provided a â€Å"firm basis for revising building codes to more fully reflect the need for extra strength in structures built on soft ground.† â€Å"Designing and building large structures is always a challenge, and that challenge is compounded when they are built in earthquake-prone areas. More than 60 deaths and about six billion dollars in property damage resulted from the Loma Prieta earthquake (caused by the San Andreas Fault). As earth scientists learn more about ground motion during earthquakes and structural engineers use this information to design stronger buildings, such loss of life and property can be reduced.† Earthquake-resistant plan and construction are necessary to plummeting earthquake losses. These code amendments are a major step toward better earthquake safety to withstand large earthquakes can be further improved with groundwork bolts, cut off walls, and additional strengthening strategies. References Clarke S. H. Jr. and Carver G. A., Late holocene tectonics and paleoseismicity, southern Cascadia subduction zone, Science, 255:188-192, 1992. Dengler, L., G. Carver, and R. McPherson, Sources of north coast seismicity, Calif. Geol. 48, 43-53, 1992. Dengler, L., Moley, K., McPherson, R., Pasyanos, M., Dewey, J., and Muray, M, 1995, The September 1, 1994 Mendocino fault earthquake, California Geology, v. 48, p 43-53, 1995. Dickinson, W. R. and W.S. Snyder, Geometry of Triple junctions related to San Andreas transform, J. Geophys. Res., 84(#B2), 561-572, 1979. Henstock, T.J., and A. Levander, Structure and seismotectonics of the Mendocino Triple Junction, California, J. Geophys. Res., 108(B5, 2260), doi:10.1029/2001JB000902. Jachens, R.C. and A. Griscom, Three-dimensional geometry of the Gorda plate beneath northern Californa. J. Geophys. Res. 88, 9375-9392, 1983. Kelsey, H.M. and G.A. Carver, Late Neogene and Quaternary tectonics associated with northward growth of the San Andreas fault, northern California. J. Geophys. Res., 93, 4797-4819, 1988. Lachenbruch, A. H. and Sass, J. H., Thermo-mechanical aspects of the San Andras, in Proc. Conf. On the Tectonic Problems of the San Andreas Fault System, edited by R. Kovach and A. Nur, 192-205, Stanford University Press, Palo Alto, Calif., 1973. Oppenheimer, D., G. Beroza, G. Carver, L. Dengler, J. Eaton, L. Gee, F. Gonzalez, A. Jayko, W.H. Li, M. Lisowski, M. Magee, G. Marshall, M. Murray, R. McPherson, B. Randall, G.R., Ammon, C.J, and Owens, T.J., Moment tensor estimation using regional seismograms from a Tibetan Plateau portable network deployment, Geophys. Res. Lett., 22, 1665-1668, 1995. Simila, G.W, Peppin, W.A., and McEvilly, T.V., Seismotectonics of the Cape Mendocino, California, area. Geol. Soc. Am. Bull. 86, 1399-1406, 1976. Stoddard, P.R., A kinematic model for the evolution of the Gorda plate, J. Geophys. Res., 92, 11524-11532, 1987. Zandt, G. and K. Furlong, Evolution and Thickness of the lithosphere beneath coastal Caifornia, Geology, v. 10, 376-3 How to cite Mendocino Triple Junction, Essay examples

Mendocino Triple Junction Free Essays

The deformational chronicles of the tectonic plates is examined from the standpoint of movement of the numerous faults bounded by the structural topography and environment and by the fault kinematics connected with the lately industrialized San Andreas transform margin. Accumulation and subduction are continuing underneath the continental margin north of the Mendocino fracture zone, with the linkage from the San Andreas fault system from the south. The continuous deformation due to the interactions among the Gorda, Pacific, and North American plates are collectively called the Mendocino Triple Junction. We will write a custom essay sample on Mendocino Triple Junction or any similar topic only for you Order Now The Mendocino Triple Junction stands for the setting of extreme change in plate tectonic processes from the convergence in the Cascadia subduction (north of the Mendocino Triple Junction) and the translation in the San Andreas system (south of the Mendocino Triple Junction. The abrupt changes form this tectonic processes resulted in the dramatic change in the thermic region in North America and the evolution in the lithosphere formation in the said region (Dickinson and Snyder, 561; Lachenbruch and Sass, 195-197; Zandt and Furlong, 377-378). The unstable intersection of the fault zones called the Mendocino Triple Junction divided the Pacific region, and North America, including North California. The meeting point The Mendocino Triple Junction is an unstable triple junction located in the North California west coast that is comprised of the intersection of the Pacific Plate, the North American Plate, and the Gorda Plate (Oppeheimer et al. 1666). The junction has complex plate activities due to seismic destructive above 6.5 in magnitude earthquakes that occurred over the past 100 years (Dengler et al., 48-50). The positioning of the Mendocino Triple Junction has transferred from its original location in the Los Angeles latitude to Cape Mendocino over the last decades. (Jachens and Griscom, 9380-9385).    One of its junctions, the San Andreas Fault, is located in the northwest-southwest portion of North America and the Pacific. The Pacific Plate moves northward simultaneously as the North American Plate moves to another region to collide with the Pacific Plate (Henstock, doi:10.1029/2001JB000902). The precise location of the San Andreas Fault is not established because of the complexities of the area (Simlila, 1402). Since the year 1800, statistics have shown that seven earthquakes have taken place with the least of magnitude four in the scale (Kelsey and Carver, 4799-4811). Another junction in the Mendocino group is the Cascadia subduction zone that is located north of the Mendocino Triple Junction. The 15-degree subduction angle continues to escalate as the depth of the subducting plate increases (Dengler et al., 45). Earthquakes in this area occur after 300 to 560 years, depending upon ruptures if the zone crossing point (Clarke and Carver, 190). The last area to be included in the Mendocino Triple Junction is the Gorda plate. The eastward movement of the Gorda Plate caused a clockwise movement in the Juan de Fuca plates, a plate formerly part of the Gorda region. The Mendocino zone remained still while the Gorda Plate repositions itself and interacts simultaneously with the Pacific Plate, therefore, increasing its deformation over time (Stoddard, 11527-11529). The Mendocino Fault is a zone located between the Pacific Plate in the south and the Gorda Plate in the north. The lateral movement of this fault contributed to seismic activities in Cape Mendocino, extending to the coast of the Gorda Plate. Earthquakes have been reported along the Mendocino Fault in 1994 as the most recent and massive tectonic plate movements with an intensity of 7.4 (Dengler et al., 45-50). In this actively deforming area, imbricate thrusts and the axes of folds overlying blind thrusts in the accretion prism offshore are oriented west-northwest and project southeastward  to align with several moderately low- to steep-dipping faults onshore. In the onshore region, the rocks bounded by these faults correspond to increasingly more distal parts of the uplifted accretion margin from northeast to southwest. The underlying problem is then rooted in the steep-dipping Pacific-North American plate boundary and to be related to ongoing northward propagation of the San Andreas movement. The area south of Cape Mendocino is significantly associated with the Pacific-North American faulting and the transformation of the plate boundary. The Future of Mendocino Triple Junction: The history of the activities in the Mendocino Triple Junction can be a potential benchmark for the cause and intensity of future earthquakes, tectonic plate ruptures, and ground breakdown. The rupture in the plates is the immediate effect of the activities happening in the Mendocino Triple Junction. Ground shaking can deliberately have an effect to structures, which is measured in the logarithmic scale to determine the intensity of the earthquake. Ground shaking is accountable for most loss of life and man-made property destruction throughout an earthquake so the importance of historical evaluation and earthquake assessment can help in the improvement of building and architectural designs and standards. The shaking intensity during an earthquake is dependent on the position of the land area hit by the massive ground activity, the type of soil and the slope of the vicinity, and its distance from the earthquake’s epicenter. Seismologists have monitored that a number of regions tend to repetitively encounter robust seismic trembling than other zones. This is due to the ground beneath these regions is comparatively soft than the other parts of the district. Soft soils intensify and amplify ground Soft soils also intensify shear waves, creating a more hazardous and damaging effects on any structure lay on the ground. Individuals living in the area that have experienced strong earthquakes will be likely to suffer strong earthquakes in the future depending upon the distance of the region to the epicenter (source) of the massive ground shaking. Amplification is caused when a seismic wave moves through subsurface materials and is amplified to produce relatively higher horizontal and vertical motion. In contrast, bedrock has a tendency to dampen seismic waves and therefore reduce ground motion. About one-quarter of the entire earthquake energy released in California during historic times has occurred along the Humboldt County coast. The size, location, and frequency of past earthquakes give an indication of what to expect in the future. Strong earthquakes with epicenters onshore have recurred about every 20 years. Since the 1870s, the largest of the historic seismic activity in the area of the Mendocino Triple Junction reached a magnitude of 7.2, which took place in 1923. The Northern Coast affected areas have been the focal point in the Gorda Plate activity. The recurrence of the earthquakes in this area occurs every two years.   Neighborhood in the coastal expanse from Cape Mendocino to Eureka has been smashed into frequent ground shaking than the remainder of the Humboldt County. Earthquakes have hardly ever affected Northern Humboldt County in history. On the other hand, because the historic documentation is comparatively transitory, regions not distressed in the past may even be at danger. Massive and huge earthquakes have been a part of the lives on the north coast so residents ought to take measures to get ready for any earthquakes to come. Up to date earthquake activity consists of several large-scale happenings in the Cape Mendocino district. Three powerful earthquakes hit Cape Mendocino area, with magnitudes  of 7.1, 6.6, and 6.7, respectively , in 1992. A strong upheaval set upon the north coast in the Cape Mendocino area with a magnitude of 5.6 last January 1997. The earthquake was situated on the Mendocino fault extremely close to the Mendocino Triple Junction. The United States Geological Service (USGS) set up new building codes in preparation for the severe earthquakes in the Mendocino Triple Junction belt. â€Å"Building codes provide the first line of defense against future earthquake damage and help to ensure public safety,† said the USGS.   According to the records of USGS, historical accounts provided a â€Å"firm basis for revising building codes to more fully reflect the need for extra strength in structures built on soft ground.† â€Å"Designing and building large structures is always a challenge, and that challenge is compounded when they are built in earthquake-prone areas. More than 60 deaths and about six billion dollars in property damage resulted from the Loma Prieta earthquake (caused by the San Andreas Fault). As earth scientists learn more about ground motion during earthquakes and structural engineers use this information to design stronger buildings, such loss of life and property can be reduced.† Earthquake-resistant plan and construction are necessary to plummeting earthquake losses. These code amendments are a major step toward better earthquake safety to withstand large earthquakes can be further improved with groundwork bolts, cut off walls, and additional strengthening strategies. References Clarke S. H. Jr. and Carver G. A., Late holocene tectonics and paleoseismicity, southern Cascadia subduction zone, Science, 255:188-192, 1992. Dengler, L., G. Carver, and R. McPherson, Sources of north coast seismicity, Calif. Geol. 48, 43-53, 1992. Dengler, L., Moley, K., McPherson, R., Pasyanos, M., Dewey, J., and Muray, M, 1995, The September 1, 1994 Mendocino fault earthquake, California Geology, v. 48, p 43-53, 1995. Dickinson, W. R. and W.S. Snyder, Geometry of Triple junctions related to San Andreas transform, J. Geophys. Res., 84(#B2), 561-572, 1979. Henstock, T.J., and A. Levander, Structure and seismotectonics of the Mendocino Triple Junction, California, J. Geophys. Res., 108(B5, 2260), doi:10.1029/2001JB000902. Jachens, R.C. and A. Griscom, Three-dimensional geometry of the Gorda plate beneath northern Californa. J. Geophys. Res. 88, 9375-9392, 1983. Kelsey, H.M. and G.A. Carver, Late Neogene and Quaternary tectonics associated with northward growth of the San Andreas fault, northern California. J. Geophys. Res., 93, 4797-4819, 1988. Lachenbruch, A. H. and Sass, J. H., Thermo-mechanical aspects of the San Andras, in Proc. Conf. On the Tectonic Problems of the San Andreas Fault System, edited by R. Kovach and A. Nur, 192-205, Stanford University Press, Palo Alto, Calif., 1973. Oppenheimer, D., G. Beroza, G. Carver, L. Dengler, J. Eaton, L. Gee, F. Gonzalez, A. Jayko, W.H. Li, M. Lisowski, M. Magee, G. Marshall, M. Murray, R. McPherson, B. Randall, G.R., Ammon, C.J, and Owens, T.J., Moment tensor estimation using regional seismograms from a Tibetan Plateau portable network deployment, Geophys. Res. Lett., 22, 1665-1668, 1995. Simila, G.W, Peppin, W.A., and McEvilly, T.V., Seismotectonics of the Cape Mendocino, California, area. Geol. Soc. Am. Bull. 86, 1399-1406, 1976. Stoddard, P.R., A kinematic model for the evolution of the Gorda plate, J. Geophys. Res., 92, 11524-11532, 1987. Zandt, G. and K. Furlong, Evolution and Thickness of the lithosphere beneath coastal Caifornia, Geology, v. 10, 376-3 How to cite Mendocino Triple Junction, Essay examples

Ralph Ellisons Invisible Man free essay sample

An analysis of the novel Invisible Man by Ralph Ellison. This paper examines Ralph Ellisons work `Invisible Man.` The author writes it is a book about race in America and, sadly enough, few of the problems it chronicles have disappeared even now. The paper describes the books compelling portrait of this New York community in the decade and a half after World War I as a place of intellectual fervor and intoxicating creativity. It is a commonplace habit of humans, to rely on the visual aspects of humanity as a means of learning who we are. It is also, as Ralph Ellison argued in his 1952 novel Invisible Man, a very dangerous habit. The novel chronicles the travels of its narrator, a young, nameless black man, as he moves through a Dantean series of circles of racism, intolerance and cultural blindness. Despite the harshness with which he is met, he continues to search for a cultural and social context in which he can come to know himself. We will write a custom essay sample on Ralph Ellisons Invisible Man or any similar topic specifically for you Do Not WasteYour Time HIRE WRITER Only 13.90 / page He searches throughout the novel for a way in which he can end his own invisibility; he struggles to be a real man rather than a prism or a mirror or a ghost.

Will the Internet bring people closer Essays - Digital Media

Will the Internet bring people closer? The Internet is definitely the greatest invention of human communication in the 20th century. As technology progresses, the Internet has helped bring adults as well as young people closer together through social media. In todays time and age, communication is received through receiving and sending emails, buying and selling, playing games, and overall just talking to one another whether its via text or through different online programs. Resources online enables people to get the latest news and helps improve their knowledge of what's going on around the world. Social networking is a prominent way to interact with family members or friends that live in different countries or states. It's the easiest, fastest and sometimes, the only way to pass on a message- whether its important or just a filler letting them know how you are. Nowadays, we are updated with their news, pictures, videos, and much more. This not only allows us to commune with them, but gives us assurance knowing that if there were some sort of emergency, we would be informed immediately. Social media has taken a huge toll in young adults everyday life. Many people make online friends through sites such as twitter, Instagram , Facebook, Pinterest , etc These teens can relate to one another and even help each other out with their daily problems. They can even communicate face to face through a video chat called Skype. Blogs are ways to express a person and their interest. People can share their experiences and interests, which can be read by thousands and thousands of people. People all over the world are linking their lifestyles from different nations and countries. People can bond over religion, recipes, cultures, fashion, etc Vlogs are another way to express ones self through videos posted on YouTube. People can leave comments and likes on the video and can even relate to videos being posted. YouTube is accessible all over the world and people from all over the world can watch and enjoy these Vlogs . The Internet has become a very big toll in our everyday lives. Adults, teens, and even young children use the internet for many reasons. It has brought different cultures together, educated many people and it contributes to our everyday lives.

Lord of the flies - Role of Gender Essays - Gender, Sex, Free Essays

Lord of the flies - Role of Gender Essays - Gender, Sex, Free Essays Lord of the flies - Role of Gender What was it that caused the aggression and dominance exhibited by the boys of Lord of the Flies? Was it some metaphysical, spiritual force, or perhaps their genetic makeup? Could it have been the influence of their peers or families, or was it the media that inspired this dangerous pattern? Conceivably, their gender had something to do with this appalling trait. It all begs the question, would the same experiences have occurred had females been stranded on the island instead of males? Had females been in a similar situation as the boys in Lord of the Flies, they would have fared abundantly better. Initially, this paper will address society's role in encouraging males' violent behavior, as well as females' politeness and passivity. Secondly, it will be discussed how family socialization influences females' gentle natures and males' aggressive temperaments. Finally, this research will explore both gender's leadership styles, and scientific perception behind these differences. Much of what society dictates can affect children's perceptions of the ideal gender standards, and can lead to abuse and violence. Media has a huge role in perpetuating these dangerous gender stereotypes. Numerous male images are used in advertising and television, representing themes such as "heroic masculinity" and "might is right". These portrayals of violent behavior associated with masculinity target young men and convince them that in order to live up to society's standards, they must resort to aggressive and dominant behavior, the use of assertion, and physical violence. Males are saturated with images of glorified aggression through movies such as Lethal Weapon, sports programs, and "macho" celebrities, like Bruce Willis and Arnold Shwartzenager. Female stereotypes span the opposite extreme. Innumerable young women perceive "ladylike" expectations to be neatness, passivity, politeness, and struggle to meet them, hence they appear nurturing and feminine. Women in the media who challenge these stereotypical behaviors and display assertiveness tend to be slotted into the role of "tomboy" or "dyke". These impositions contribute to the breeding of young men who act in an abusive manner, and are terribly restricting towards boys who covet deep emotion. The antagonist of Lord of the Flies, Jack Merridew, perceives himself to be higher than the others, on the basis of being the choral leader. Jack's hierarchical views cause him to verbally abuse, psychologically torture, and eventually wound and kill other children. With the influences of society's stereotyping, girls would generally more nurturing and caring towards group members. A lot of males' violent behavior and females' complaisance can be accredited to family and institutional socialization. Parents usually raise boys on aggressive sports, such as hockey and football, which encourage violence. Girls, however, are generally brought up on "feminine" activities, dance and figure skating to name a few, which promote a gentle, polite nature. It is the rare parent that heeds their four-year-old son's aspiration to be a ballet dancer by purchasing the child a pair of tights and a leotard. When a boy shows more interest in dolls than in trucks, his family may be distressed, and provoke him to reveal his "masculine" side. After striving for egalitarianism between the sexes for so many years, families still deter young girls from pursuits of hockey stardom, hoping to interest them in Pointe shoes. Displays of emotion by boys are often criticized for being "unmasculine", whereas emotional behavior in girls tends to be expected and accepted. As a result, boys tend to not only hide their feelings, but criticize friends for showing their emotions. Girls, on the other hand, encourage one another to express feelings and console one another naturally. Research shows that boys and girls have different means of reaching decisions and achieving organization. Males, on whole, like to dominate a situation, whereas females would rather resort to consensus and unanimity. Collegiality and cooperation are fundamental female traits, while the need for dominance and individual power goes hand in hand with masculinity. This male yearning is rooted before birth, when the developing nervous system is immersed in testosterone (the predominant male hormone). This pre-natal process is responsible for the maturation of the areas of the brain that arbitrate between the male hormones and their dominant behavior. Steven Goldberg, the chairman of the Department of

MidTerm Two Term Paper Example | Topics and Well Written Essays - 250 words

MidTerm Two - Term Paper Example Plato on the other side argues that the best rational political order leads to harmony and unity in a society. He says that behaviors of people determine the outcomes of any political endeavor. If dialogue is initiated, then there is the belief that there would be some political order (Kennedy 152). Plato insists that justice is the best character that leads to a political order. Plato’s argument seems to be best since it urges people to prepare and ensure that everything is in order before politics is initiated. On the other hand, Aristotle argues that only the happy and virtuous people can participate in politics. For both ideas of Aristotle and Machiavelli, there is belief in a spectrum of some diverse categories for exercising social development and organization. Both believe that social organization can function as an on-going negotiation of time among the individuals with desperate aims. It can also function as a partnership that aims at persuading common goals (Gross et al.

Ethics and Business Success Essay Example | Topics and Well Written Essays - 1000 words

Ethics and Business Success - Essay Example They seek ways to improve their productivity, efficiency, and the way their company functions as a whole. Two of the articles printed in the Journal of Value Based Leadership offer ways to improve businesses in two very different ways. The first, "Secrets of Your Leadership Success-The 11 Indispensable E's of a Leader," by M.S. Rao, essentially offers a positive, team friendly approach that will give a path to strong leadership. The second, "The Conscious Organization: Prospects for a Self-Actualized Workforce,† by John Renesch, supports developing your business using the ideas of psychological theorists, Andrew Maslow and Carl Jung, treating the business as you would a person. It places the value on the needs of the whole company, but less on its individual parts. Renesch’s approach to gaining success within a business is mixing the principles of Maslow’s self-actualization and Jung’s â€Å"shadows,† which are things that block a person from achievi ng their highest potentials. The author believes that by viewing businesses in the same way that you look at a person you can make the best of it; pretending that a business has the same need to self-actualize as a person does. He, also, focuses on a tightly structured organization within the business. He explains that anything that gets in the way of the success of the business it should be eliminated for the sake of the business. This is the basis of a â€Å"Conscious Organization,† which the author created in the 1990s. The author promotes that a successful business and successful people are those who are willing to evaluate themselves, their values, and relationships all of the time. â€Å"Living this sort of self examined life is what brings meaning and worth (Renesch 74-77). In the second article, Rao takes a different approach. He discusses how any successful business needs strong leadership if they hope to be successful. He suggests that the â€Å"11 E’s† are those traits or behaviors that can guarantee that someone is on the right path towards leadership, and they are easy to remember as they all start with the letter â€Å"E.† It is the combination of these elements, he says, can and will develop into the best kind leader in the best kind of business. Both articles are very interesting in their approaches. However, Rao’s article offers such a positive way of creating a happy work environment and good teamwork, while Renesch’s view is very cold. It does not seem to care about the needs or issues of the workers. Renesch want to treat the business like it is a living person and the people are like replaceable parts. The two writers are very different. For example, if there was an employee who was not working to their best possible ability; Rao would work to encourage that employee to do better, but Renesch would call this employee a â€Å"bad† employee and want to get rid of them. In this context, there is no room for anything except what is good for the business. Rao’s article appears to value the employees and Renesch’s does not really feel like that. His article feels like he sees individual people are just parts, when one is no good just throw it out and replace with a better one. This kind of heartless business practice does not always make for a good business to be a part of, even if the profits are high. People, I think, will work harder for people and for goals when they feel that they matter and the contribution that they make is important. When I enter into the business world I want to make the best choices that I can. I agree with Renesch when he explained how important being able to change and grow in the business industry, but it is Rao whose article I think will benefit me the most when I enter into my career field. Having a good way of becoming a strong leader