What Is Perfect Can A Person Be As Such - 1334 Words

What is perfect? Can a person be as such? Without getting too philosophical, but dwelling upon my own past, one could conclude I am the furthest from perfect. With a total of five criminal charges, all at the misdemeanor level or lower, some may even say I am a habitual offender. However, to label myself as such would be no different than judging a book by its cover; it’s not about the cover, rather it’s about the contents inside. July 2011 to November 2013 was a deep dark place for myself. I often found myself in with the wrong crowd making terrible choices and jeopardizing my schooling by not allotting the necessary time and effort towards it. In November 2013, I was called into work and informed I was terminated. Not only was I being†¦show more content†¦To this day, I still deal with the consequences of my previous criminal actions, but I do not let it deter myself. Although negative at the time, my criminal history has given me the opportunity to grow and mature as a person, and to truly learn from my mistakes. In having to deal with the hardships of a criminal record, I gained a tremendous amount of motivation. Inside myself is a drive to succeed, fueled by learning from my mistakes. No matter the task at hand, I strive to do my utmost personal best. In terms of schooling, I enjoy challenges as I like to work hard and I do not see failure as an excuse to give up; rather I see it as an opportunit y to learn more and become better than I was previously. For quite some time, I knew that I did not want a bachelor’s degree to be the end of my education; I knew I wanted the challenge of more and could push myself to do so. My motivation to learn and to continue expanding my knowledge also guided me towards law school, as the law and studies of the law are always changing, therefore my education would be too. Becoming an attorney has been a goal of mine for most my life which is why I chose to earn a major in Criminal Justice Studies. However, it was not until college that I truly knew law school was what I wanted to do. Between my own experiences and the courses encompassed with a Criminal Justice major, my interest peaked even more as it gave me hands on experience andShow MoreRelatedDo You Have a Low Self-esteem? Essay926 Words   |  4 Pagesaltogether beautiful my darling; beautiful in every way.† This verse from the Bible sums up what I think about every woman. I believe that every woman, teenage girl, or pre teen sh ould stop putting themselves down! Confidence is key to living a happy and joyful life. Being depressed, being unhappy, giving up on things, being introvert and not feeling good about oneself are some characteristics of a person that does not have self confidence. 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Finance Project - 3247 Words

Spring 2014 Principles of Finance Final Project General Motors Company vs Ford Motor Company Lauren Grippo GENERAL MOTORS CORPORATION (COMPANY) General Motors Corporation (General Motors or GM) was incorporated on August 11, 2009. Also known as GM, the company designs, builds and sells cars, trucks and automobiles parts globally and headquartered in Detroit, Michigan. The company also provides automotive financing services through General Motors Financial Company, Inc. (GM Financial). The company designs, manufactures and markets vehicles under the brands of Buick, Cadillac, Chevrolet and GMC. Along with our strategic partners, we produce cars and trucks, and sell and service our vehicles, through the following brands: Chevrolet,†¦show more content†¦In 2008, Ford produced 5.532 million automobiles and employed about 213,000 employees at around 90 plants and facilities worldwide. The company went public in 1956, but the Ford family still retains 40 percent voting rights. I will be comparing both companies General Motors Company and Ford Motor Company for the past three years. We will be able to see all the trends these two automotive manufacturers have and which one may be better to invest in by looking at the last few year’s ratios and percentages. This will give us a better understanding and the knowledge of who maybe the industry leader and who is the follower. These are both major corporations that strive off customer loyalty and both competing on a global scale to make their mark in the one of the top automotive manufacturers in the world. This analysis will give us an understanding of what lies ahead in the future for these two manufacturers. The following section will show the ratios and percentages figured by using these two companies’ financial statements. A comparison will be used to compare the companies to one another. People will always needs cars to get around whether it’s for education, work or tourism. 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METHOD OF FINANCING A PROJECT†¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦6 5. CONCLUSION†¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦7 6. REFERENCES†¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦8Read MoreIntroduction to the Finance Company Project979 Words   |  4 PagesIntroduction to the Finance Company Project Your team is required to analyze the future business and economic prospects of a major, publicly traded corporation using financial concepts and techniques as well as the concepts and techniques from other business areas. 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Celebration Of The Lizard Essay Example For Students

Celebration Of The Lizard Essay Celebration of the lizard by James Douglas Morrison is a helpless labyrinth of insanity. The poem is a murder that results in insanity. The speaker is the murderously insane madman. In this outrageous maze, the poet is running from his chaotic problems. In the first three stanzas, it starts out as a bad dream that eventually causes the speaker to drive himself to a temporary insanity. During his state of temporary insanity, he murders a man out of jealousy that he cannot control. After the murder, he runs to a hideout on a hill far away. He describes the hideout as a mansion to give you the picture in your mind of how appreciative he is to have a place to hide. The journey is a long and monotonous one but ends in the disappointment of having to turn back. In the last stanza he announces, Tomorrow we enter the town of my birth, I want to be ready. In this poem, James Morrison is taking you with him on a frantic, frightening roller coaster. The poets tone is dark and eerie. The dream in the beginning becomes a reality, which is an example of foreshadowing. When he describes the mansion on the hill, it puts a picture in your mind, which is an excellent example of alliteration. This poem is interesting and frustrating at first because it makes you think about every phrase. To read it requires keeping an open mind because there are a lot of metaphors. I had to read it over 20 times just to get a vague understanding. Please do not let the length and metaphorical contents of this poem discourage you from reading this intriguing poem. This is definitely a poem that you will not find in a schoolbook. If you like this poem, I recommend that you read the work of other dark poets such as Edgar Allen Poe.

Formation Of Hawaiin Islands Essay Research Paper free essay sample

Formation Of Hawaiin Islands Essay, Research Paper The Formation of the Hawaiian Island Chain The Hawaiian Islands are one of the most beautiful and popular island ironss in the universe. Millions of tourers visit the islands every twelvemonth to see the great hoarded wealths that they have to offer. Peoples see Hawaii as an ideal holiday topographic point for many grounds including ; a twelvemonth round tropical clime, the exuberant flora, and the legion black sand beaches. However, the Hawaiian Islands are non merely reasonably to look at. The Islands possess alone geological facets that make it possible for the islands to hold these desirable features. The Hawaiian Islands were non pieces of a continent that drifted out to sea, but were really created by vents in the center of the Pacific Ocean. The procedure in which this concatenation of island is formed is rather challenging and complex. The different stairss include the presence of a hot topographic point, the outgrowth of an pelagic vent, the home base tectonics of the part, the submerging of the older vents, and the kineticss of the active Hawaiian vents. Hawaii consists of many vents that were produced by a characteristic known as the Hawaiian hot topographic point. A hot topographic point, or plume, is a big column of magma, liquefied lava, which rises from deep within the Earth s asthenosphere ( Monroe 332 ) . The magma that comes out of these columns is so hot that it can run through the bed of Earth on top of the asthenosphere, called the mantle, and through the Earth s crust ( the top bed of the Earth ) . There are merely 40 known hot musca volitanss that exist today. Hot musca volitanss can be found under a continent or an ocean, at a mid-ocean ridge and even in the centre of a home base, like the Hawaiian hot topographic point ( Duxbury 78 ) . Each hot topographic point channels hot stuff at its ain alone clip intervals. Hot musca volitanss are by and large stationary, nevertheless ; their places may alter somewhat. A typical hot topographic point has a life span of approximately ten million old ages ( Duxbury 78 ) . They are great beginnings of new stuff for the Earth s crust and can make, non merely one, but a concatenation of islands. The outgrowth of an pelagic vent is merely the beginning of an island concatenation. When a hot topographic point is active it will force magma up to the crust above, to make a volcanic extremum if on land, or seamount if in H2O. The primary vents on each of the Hawaiian islands are called shield vents. They are described as gently spilling mountains, looking much like the outer surface of a shield prevarication on the land. They are created by legion lava flows that easy spread out and indurate in really thin beds ( Rubin 1 ) . After the edifice of bed upon bed the vents finally cut through the surface of the ocean organizing an island ( Rubin 2 ) . The eruptions of shield vents tend to hold a quiet, smooth spring of midst, fluxing magma instead than a sudden detonation ( Duxbury 73 ) . However, on juncture, some of the Hawaiian vents, such as Kilauea, have produced big detonations. Explosions normally merely occur when the magma mixes with groundwater, making instant vaporisation. Some of Hawaii s shield vents have lava fountains that spew up from the top of the vent that can make every bit high as 400 metres ( Monroe 89 ) . The mean Hawaiian vent can stay active for 100s of 1000s of old ages before being carried off from its hot topographic point by the traveling Pacific home base ( Rubin 2 ) . The volcanic activity within the sea around the islands is believed to be a factor in the fact that the surrounding Waterss are about 83 grades F twelvemonth unit of ammunition. The home base tectonics of the Hawaiian Island part play a major function in the formation of this alone island concatenation. As the hot topographic point signifiers and fuels a vent, the Pacific home base is continuously traveling westward. Since hot musca volitanss are stationary the traveling home base carries the vent with it, cutting off the changeless supply of magma. Without the magma reserve the vent can no longer break out, go forthing it inactive. After the vent is moved the hot topographic point will no longer hold an mercantile establishment for magma. Soon after the plume will break out one time once more and make a new vent to replace the 1 it had merely lost. As the Pacific home base continuously moves across the Hawaiian hot topographic point back-to-back eruptions have created the additive order of the islands. The home base moves over the asthenosphere Northwest at a rate of 5 to 7 centimetres per twelvemonth ( Rubin 1 ) . The age of the Hawaiian Islands tend to ac quire older as they are observed from the sou-east to the nor-east ( Rubin 2 ) . In drumhead, when compared to an active vent presently under the hot topographic point, the other vents continue to float westward while at the same clip they are acquiring older. One of the northwesterly most islands, Kauai, is estimated to be formed 3.8 to 5.6 million old ages ago, whereas Hawaii, the island presently unde r the hot topographic point, began organizing less the one million old ages ago ( Monroe 102 ) . The land characteristics of the different islands besides tell a narrative of their ages. The island of Hawaii shows small marks of eroding. On the other manus, an older island, like Oahu, exhibits many marks of eroding caused by their uninterrupted motion every bit good as elements like air current and rain. The creative activity and the gesture of the Hawaiian Island concatenation are a really utile tool in assisting geologists to explicate the motion of the Pacific home base. The submerging of old vents is another portion to the rhythm of island ironss. As the islands move off from the hot topographic point the home base cools and contracts. In combination with the catching of stuff, the weight of the vent and the eroding factors, the ensuing consequence is one of a depression. The vent finally sinks lower and lower until it is no longer above the surface of the ocean ( Duxbury 78 ) . Beyond Kure, the oldest, most western island, the Hawaiian Island concatenation continues with a twine of submersed former islands. These islands are known as the Emperor seamounts ( Rubin 2 ) . As the seamounts easy sank, coral began to turn upward making coral reefs and further polishing the beauty of the part. The kineticss of the active vents within the Hawaiian Island concatenation are still at the beginning of the island concatenation rhythm. There are presently three active vents in Hawaii. Two of them are on the island of Hawaii, Mauna Loa and Kilauea. The other 1 is a undersea vent, called Loihi, which has non yet, broke the surface of the ocean. All three of the vents portion the Hawaiian hot topographic point. Mauna Loa is the largest vent in the universe with volume of 9,600 three-dimensional stat mis and lifting 13,677 pess into the air above sea degree. Mauna Loa seems immense in comparing to the volume of Mount Shasta at 40 three-dimensional stat mis, the largest vent on the Continental United States. This vent itself makes up over 50 % of the full province of Hawaii ( Mauna Loa 2 ) . Because of the great mass of Mauna Loa the sea floor has a depression five stat mis beneath the tremendous vent ( Mauna Loa 1 ) . Mauna Loa is considered one of the most active vents on the planet holding erupted 33 times in one hundred 57 old ages. However, Kilauea tops that holding 34 eruptions in merely 48 old ages, non including its uninterrupted lava-lake activity ( Urnezis 1 ) . The name Kilauea means, spiting in Hawaiian, mentioning to the changeless lava activity. Its most recent eruption has been uninterrupted since January 3rd of 1983 ( Kilauea 2 ) . This vent consists of approximately 14 % of Hawaii. Loihi, on the other manus, is non an island, but an submerged seamount. It represents the first phase of the formation of a new Hawaiian island. The seamount rises over 10,100 pess above the sea floor and is merely 3,100 pess within the surface of the H2O ( Loihi 2 ) . Loihi is an active vent that often generates temblors. Scientists from the University of Hawaii have conducted many honkytonks to Loihi in order to piece informations garnering burials on the acme of the vent ( Loihi 2 ) . The informations collected from these burials will give scientists an chance to a nalyze the geological phenomenon in greater item. The active Hawaiian vents are found to be the youngest within the concatenation, nevertheless, they can demo a great trade about what the more western vents looked like while under the Hawaiian hot topographic point. The geological facets of the Hawaiian Island concatenation continue to excite involvement in members of the geological society. Comparing the age and distances in between each island can assist scientists to cipher the velocity of the motion of the Pacific home base. This information AIDSs in the better apprehension of home base tectonics in general. In add-on, the information can assist to foretell where the home base will travel by analyzing where it has been. The rhythm of the Hawaiian Islands: the birth of a seamount, the turning of an island, the displacement in the crust and the decay and submergence of a vent, is an illustration of the how the Earth invariably renews and recycles its stuff. Before these islands submerge into the sea in 1000000s of old ages from now, it is of import for world to look into, explore and bask the events and features determining the Hawaiian Islands. This is of import, non merely to derive a greater apprehension of the planet as a whole, but to bes ides appreciate the tropical Eden that Hawaii is known for. The Hawaiian Islands are so diverse that if a tourer were to travel at that place during the Hawaiian winter they could take to partake in a scope of activities from skiing on snow capped mountains in Hawaii to researching the dry sweets of Kau, besides on Hawaii. There is no admiration why so many people chose this topographic point, all entirely in the center of the Pacific, to pass their barely earned holiday clip.