On the Road to New York :: Personal Narrative Traveling Essays

On the Road to New York There is a funny thing that happens when you travel. The people are all the same. Sure they may talk with a slightly different accent, and they may dress just slightly differently, and may think just slightly differently. In the end they are basically the same thing, a human being. I recently took a trip. I was going to a conference in Ithaca NY. Round trip is approximately 3000 miles. Driving time is 20 hours one way. I drove it all by myself in as little time as possible. I ended up taking 24 hours to do it. It is quite a rigorous challenge to do it all in one shot. I can classify the terrain into basically three things that you see: plains, woods, and hills. Sometimes you would see an area that combined woods and hills, but that was usually in a mountainous area. Along the whole route you would switch back and forth between these three characteristics. ND and eastern MN are plains. Central and Western MN and Wisconsin are mostly heavy woods with some lakes. On the plains the highway was pretty straight. Once you got to the woody areas, curves like no ones business. In Wisconsin the trees were son think that they had to cut a swath out just for the interstate crossovers that the HP use to change directions. This patch that was cut out was about fifty meter long. There was a patch of asphalt that was thrown down between the two highways which were about 30 meters apart. The green tops of the evergreens contrasted with the light brown tree trunks which extended up at least 60 feet. There were some small patches of green grass that filled in betwee n the trees and the concrete of the highway. Every fifth exchange a brown Highway Patrol car with a pale yellow stripe down the middle and a low profile light bar would be sitting waiting for the next speeder. Maybe this helps them to blend in? Oddly enough my radar detector never went off. Were they just there to present the threat of being stopped? When I got out of Wisconsin Illinois, Indiana, Ohio and Pennsylvania pretty much look like ND. When you get to Chicago however things take a very different turn. Everything turns into an industrial style. Concrete everywhere, toll booths every 25 miles or so, no seemingly familiar sites other than a slightly wider patch of concrete called the interstate.

Volcanic and Seismic Events Are Major Pieces of Evidence Towards

â€Å"Volcanic and seismic events are major pieces of evidence towards proving that the plate tectonic theory is valid† Discuss the extent to which you agree with this statement (40). The theory of plate tectonics explains the structure and motion of the Earth’s lithosphere. The theory states that the Earth’s crust is split into large sections called tectonic plates, and these move relative to one another creating boundaries at which the plates converge, diverge or move past each other.These plates are either continental or oceanic and are powered by convection currents, which is the circular movement of magma that comes from within the mantle. These currents are powered by the core, which heats the magma, causing it to rise, cool and fall back down. This circular motion causes the plates, which float on the mantle, to move. In 1912, Alfred Wegener, a German meteorologist, was the first man to state that the continents were once joined in a super continent called Pangaea, conversely he couldn’t explain why and what happened to cause the plates to move apart.He based his theory on the extraordinary fit of the South American and African continent coastlines. Notably the eastern edge of South America and the western edge of Africa showed very similar geological features suggesting that at some point in the Earth’s history the landmasses were joined together. Another indicator that the continents were once distributed differently was geological evidence of glaciations in India – it is unlikely that glaciers could ever reach such low latitudes, but this problem can easily be explained by the theory of continental drift.Fossil distribution also provided some of the earliest evidence for plate tectonics. Interestingly, plant and animal fossils were found on the matching coastlines of South America and Africa. These are now widely separated by the Atlantic Ocean, therefore he reasoned that is physically impossible for most of t hese organisms to have swum or have been transported across the wide oceans. From this he suggested that the plates were once connected. Unfortunately, at the time of Wegner’s work many of the geophysical tools that are used today did not exist making the theory much more difficult to support.Since the original theory in 1912, newer evidence has appeared which supports the theory. In 1962 Hess studied the age of rocks around the mid-Atlantic ridge. He discovered that the newest rocks were closest to the ridge and the oldest were towards the USA and Caribbean. He therefore reasoned that the earth’s crust was expanding along the oceanic ridges, so it must be shrinking elsewhere. According to Hess, the Atlantic Ocean was expanding while the Pacific Ocean was shrinking. The old oceanic crust was consumed in the trenches causing new magma to rise and erupt along the spreading ridges to form a new crust.He explained why the earth doesn’t get bigger with sea floor spre ading and why there is so little sediment accumulation on the ocean floor, and why oceanic rocks are so much younger than continental ones. Paleomagnetism is one of the strongest pieces of evidence for plate tectonic theory and was developed to convince scientists of the theories validity. Basalt lava forms volcanoes when it rises to the surface, cools and then forms land. When new crust is formed certain minerals align themselves with the Earth’s magnetic field.Fascinatingly, new technology has shown that the magnetic field of the Earth is known to reverse every few hundred thousand years. So this implies new material is constantly being produced and the sea floor is spreading. However, as the Earth is not changing in size, material is being destroyed in other areas which are called subduction zones, and the position of the Earth’s crust must be constantly changing. Seismic activity can also tell us a great deal about plate tectonics. Plotting the locations of large e arthquakes allows us to see where they most frequently occur.Earthquakes are caused by the movement of tectonic plates. The plates move past each other which causes friction causing pressure to build up resulting in sudden jolts. This only happens on plate boundaries meaning areas that lie on them experience the most intense earthquakes. The fact that earthquakes appear in connected lines as opposed to clusters is good evidence for the theory of global plate tectonics. Volcanic events are also useful as they provide good evidence for the theory of plate tectonics.Similarly to earthquakes, plotting the locations of active volcanoes on a map of the world will also be useful as it will show a similar pattern. The three main places where volcanoes are created are at subduction zones, constructive plate boundaries and in hotspots, with around 75% of the world’s volcanoes being located on the ‘Pacific Ring of Fire’. The area where two plates converge is called a subduc tion zone, here one plate is pushed underneath the other due to differing in density. This results in magma rising up to form volcanoes or volcanic island arcs.At constructive plate boundaries, new material is created by magma rising through the crack. The fact that volcanoes in certain areas have different types of eruption provides good evidence for plate tectonic theory. All the above reasons suggest that the theory is valid. However, there are some anomalies which go against the theory. Not all volcanoes occur on plate boundaries, some occur on hotspots which are areas where the mantle is particularly hot, causing it to rise and create volcanoes on the crust above.This suggests that plate tectonics theory may not be valid as volcanoes can exist without the theory being correct. Hawaii is a notable example of an active hotspot – the islands are volcanic yet lie in the middle of the Pacific plate. It is part of a chain of extinct volcanic islands in the Pacific Ocean which decrease in both age and size as you move north-west. Since the hotspot is created by the underlying mantle this suggests that the crust is moving over this hotspot meaning the volcanoes eventually become extinct and eroded away.Since Wegener’s first theory, there is now a great deal of evidence to support the theory of plate tectonics. Seismic and volcanic events can provide lots of evidence to support the theory, although much of it requires tools which were not available when the theory was first developed such as accurate methods of mapping earthquakes. This made it difficult to prove the theory of plate tectonics as there were no hard facts. Although others may disagree, there are large amounts of evidence to prove the theory and so in my opinion the theory is a valid method.

Mkt 421 Wk 1 Individual

Marketing Definitions MKT 421 November 27, 2012 Marketing, what is it? And how is it defined? Marketing is sometimes difficult to grasp for the average person. Though, in the business world marketing is extremely important. Defining marketing and the marketing mix gives a great overview of how understanding marketing and the processes involved are important for a successful organization. Many may have the general idea of what marketing is, but looking it at a micro level brings to play many more aspects that the average eye may not see.A lot more goes into marketing and for myself marketing is what gets the consumers to buy into the product. In the book, Basic Marketing: A marketing plan strategy approach states, â€Å"Marketing is the performance of activities that seek to accomplish an organization’s objectives by anticipating customer or client needs and directing a flow of need-satisfying goods and services from producer to customer or client† (Basic Marketing: A ma rketing plan strategy approach, 2011).Whereas The Columbia Encyclopedia says, â€Å"Marketing includes the activities of all those engaged in the transfer of goods from producer to consumer—not only those who buy and sell directly, wholesale and retail, but also those who develop, warehouse, transport, insure, finance, or promote the product, or otherwise have a hand in the process of transfer† (Columbia Encyclopedia, 2008). Finally, the Marketing Management (14th ed) states that, â€Å"Marketing is about identifying and meeting human and social needs.One of the shortest good definitions of marketing is â€Å"meeting needs profitably† (Marketing Management, 2012). The concept of â€Å"meeting needs profitably† is true because at the end of the day that is the entire purpose of marketing. Spending money is a huge deal for any company and the way we spend â€Å"marketing dollars† can really make or break the product being sold. Although, behind the doors of marketing is a lot of planning and developing to make certain the target market buys into the brand and/or product being advertised.Marketing is a cost that a business must evaluate based off of the return on investment. The marketing plan a business develops really is what can make or break a business especially during start up. Once the business is up and running the marketing investments is just as important. However, at a certain point the research has been done and developed so marketing the next product is easier with the target market in place. An example of this would be each time a company such as Apple comes out with a new product.Apple has already established their brand name and has developed the customer base for their product. They will need to strategize about how they can expand their market, but overall they will be able to develop a sound budget based off the last results. Apple’s marketing has a lot to do with their success. Their marketing strateg y since 2007 has been something to talk about. It was stated that since 2007 Apple as been relying mostly on the media to create buzz about the products. They have also used their products for product placement for TV shows and Movies as marketing (Edwards, 2012).Theses different type of strategies is what takes place during the marketing mix. â€Å"McCarthy classified various marketing activities into marketing-mix tools of four broad kinds, which he called the four Ps of marketing: product, price, place, and promotion† (Marketing Management, 2012). These four Ps are what should be focused on when developing a solid marketing plan. A lot goes into the product first such as variety, quality, design, features, brand name, packaging, sizes, services, warranties, and returns (Marketing Management, 2012).Nike definitely used this first P in making sure they marketed an exclusive product. Nike, starting in 1962 hit the ground running with the idea to make a superior and exclusive product to serve athletes (Marketing Management, 2012). They chose a great product idea to potentially make a lot of money in the long run. Nike developed a superior product and backed it up with price, place, and promotional tactics. Eventually Nike began to hire on spokesmen that were athletes such as Michael Jordan in 1985 when he signed to the NBA as an up and coming rookie.This chance paid off for Nike making them over 100 million in sales the first year alone (Marketing Management, 2012). Having a solid marking plan has played important role for companies such as Apple and Nike. Although, there are some organizations that don’t make a profit and these non-profit organizations use these same tactics that Apple and Nike use as they understand the importance of marketing as well. This goes to show â€Å"meeting needs profitability† and most companies are out to make a profit even when â€Å"they are not†. References Edwards, J. (2012, April 5).Apple's Biggest Marketing Secret Was Revealed In Federal Court. In Business Insider. Retrieved November 27, 2012, from http://www. businessinsider. com/apples-biggest-marketing-secret-just-got-revealed-in-federal-court-2012-8 Kotler, P. & Keller, K. L. (2012). Marketing management (14th ed. ). Upper Saddle River, NJ: Prentice Hall, (P. 2-29). Marketing. (2008). The Columbia Encyclopedia, 1. Perreault, W. D. Jr. , Cannon, J. P. , & McCarthy, E. J. (2011). Basic marketing: A marketing strategy planning approach (18th ed. ). New York, NY: McGraw-Hill Irwin.

s Syndrome

Understanding and living with a child that has a syndrome is a heart breaking experience. Today over thousands of parents have to live with children that have down’s syndrome. Children are born frequently with this type of disorder. If someone close had a disorder would you understand what was going on or do you even know what I am talking about? In 1866 the study of Down’s syndrome began. Physician John Langdon Down published and essay in England. The essay talked about a set of children who all looked alike and had mental retardation. These children also looked like people from Mongolia. In 1960 the name Down’s Syndrome became know to people. In the twentieth century there was speculation of a case of Down’s Syndrome. In the 1930’s Waardenburg and Bleyer came up with the theory that it might be chromosomal abnormalities. Jerome Lejeune and Patricia Jacobs found the trisomy of the 21st chromosome. Jerome and Patricia worked separately on the project. A chromosome is a â€Å"thread-like structure composed of DNA and other proteins,† stated Len. Chromosomes are in every cell. They carry the gentic information to the cell to develop. â€Å"Genes, which are units of information, are ‘encoded’ in the DNA,† stated Len. A human is divided into mitosis and meiosis. Mitosis is were the body grows. In mitosis one cell converts to two cells and has the exact number as there parents. Meiosis occurs in the ovaries and the testicles. The one cell will split into two cells. When this happens cells have half the chromosomes the parents have. Down’s syndrome or trisomy 21 is the most common autosomal trisomy. Mader stated â€Å"trisomy is having three of a particular type of chromosome,† and â€Å"autosomal is any chromosome other than the sex-determining pair.† Chromosome 21 usually has one copy and in Down’s Syndrome it has two. Down’s Syndrome has three copies in chromosome 21. In most cases the sperm had the extra 21 ch... 's Syndrome Free Essays on Down\'s Syndrome Understanding and living with a child that has a syndrome is a heart breaking experience. Today over thousands of parents have to live with children that have down’s syndrome. Children are born frequently with this type of disorder. If someone close had a disorder would you understand what was going on or do you even know what I am talking about? In 1866 the study of Down’s syndrome began. Physician John Langdon Down published and essay in England. The essay talked about a set of children who all looked alike and had mental retardation. These children also looked like people from Mongolia. In 1960 the name Down’s Syndrome became know to people. In the twentieth century there was speculation of a case of Down’s Syndrome. In the 1930’s Waardenburg and Bleyer came up with the theory that it might be chromosomal abnormalities. Jerome Lejeune and Patricia Jacobs found the trisomy of the 21st chromosome. Jerome and Patricia worked separately on the project. A chromosome is a â€Å"thread-like structure composed of DNA and other proteins,† stated Len. Chromosomes are in every cell. They carry the gentic information to the cell to develop. â€Å"Genes, which are units of information, are ‘encoded’ in the DNA,† stated Len. A human is divided into mitosis and meiosis. Mitosis is were the body grows. In mitosis one cell converts to two cells and has the exact number as there parents. Meiosis occurs in the ovaries and the testicles. The one cell will split into two cells. When this happens cells have half the chromosomes the parents have. Down’s syndrome or trisomy 21 is the most common autosomal trisomy. Mader stated â€Å"trisomy is having three of a particular type of chromosome,† and â€Å"autosomal is any chromosome other than the sex-determining pair.† Chromosome 21 usually has one copy and in Down’s Syndrome it has two. Down’s Syndrome has three copies in chromosome 21. In most cases the sperm had the extra 21 ch...

Geography and Overview of Tsunamis

Geography and Overview of Tsunamis A tsunami is a series of ocean waves that are generated by large movements or other disturbances on the oceans floor. Such disturbances include volcanic eruptions, landslides, and underwater explosions, but earthquakes are the most common cause. Tsunamis can occur close to the shore or travel thousands of miles if the disturbance occurs in the deep ocean. Tsunamis are important to study because they are a natural hazard that can occur at any time in coastal areas around the world. In an effort to gain a more complete understanding of tsunamis and generate stronger warning systems, there are monitors throughout the worlds oceans to measure wave height and potential underwater disturbances. The Tsunami Warning System in the Pacific Ocean is one of the largest monitoring systems in the world and it is made up of 26 different countries and a series of monitors placed throughout the Pacific. The Pacific Tsunami Warning Center (PTWC) in Honolulu, Hawaii collects and processes data gathered from these monitors and provides warnings throughout the Pacific Basin. Causes of Tsunamis Tsunamis are also called seismic sea waves because they are most commonly caused by earthquakes. Because tsunamis are caused mainly by earthquakes, they are most common in the Pacific Oceans Ring of Fire - the margins of the Pacific with many plate tectonic boundaries and faults that are capable of producing large earthquakes and volcanic eruptions. In order for an earthquake to cause a tsunami, it must occur below the oceans surface or near the ocean and be a magnitude large enough to cause disturbances on the seafloor. Once the earthquake or other underwater disturbance occurs, the water surrounding the disturbance is displaced and radiates away from the initial source of the disturbance (i.e. the epicenter in an earthquake) in a series of fast-moving waves. Not all earthquakes or underwater disturbances cause tsunamis - they must be large enough to move a significant amount of material. In addition, in the case of an earthquake, its magnitude, depth, water depth and the speed at which the material moves all factor into whether or not a tsunami is generated. Tsunami Movement Once a tsunami is generated, it can travel thousands of miles at speeds of up to 500 miles per hour (805 km per hour). If a tsunami is generated in the deep ocean, the waves radiate out from the source of the disturbance and move toward land on all sides. These waves usually have a large wavelength and a short wave height so they are not easily recognized by the human eye in these regions. As the tsunami moves toward shore and the oceans depth decreases, its speed slows quickly and the waves begin to grow in height as the wavelength decreases (diagram) This is called amplification and it is when the tsunami is the most visible. As the tsunami reaches the shore, the trough of the wave hits first which appears as a very low tide. This is a warning that a tsunami is imminent. Following the trough, the peak of the tsunami comes ashore. The waves hit the land like a strong, fast tide, instead of a giant wave. Giant waves only occur if the tsunami is very large. This is called runup and it is when the most flooding and damage from the tsunami occurs as the waters often travel farther inland than normal waves would. Tsunami Watch Versus Warning Because tsunamis are not easily seen until they are close to shore, researchers and emergency managers rely on monitors that are located throughout the oceans that track slight changes in the height of waves. Whenever there is an earthquake with a magnitude greater than 7.5 in the Pacific Ocean, a Tsunami Watch is automatically declared by the PTWC if it was in a region capable of producing a tsunami. Once a tsunami watch is issued, PTWC watches tide monitors in the ocean to determine whether or not a tsunami was generated. If a tsunami is generated, a Tsunami Warning is issued and coastal areas are evacuated. In the case of deep ocean tsunamis, the public is normally given time to evacuate, but if it is a locally generated tsunami, a Tsunami Warning is automatically issued and people should immediately evacuate coastal areas. Large Tsunamis and Earthquakes Tsunamis occur all over the world and they cannot be predicted since earthquakes and other underwater disturbances occur without warning. The only tsunami prediction possible is the monitoring of waves after the earthquake has already happened. In addition, scientists today know where tsunamis are most likely to occur due to large events in the past. In March 2011, a magnitude 9.0 earthquake struck near the coast of Sendai, Japan and generated a tsunami that devastated that region and caused damage thousands of miles away in Hawaii and the west coast of the United States. In December 2004, a major earthquake struck near the coast of Sumatra, Indonesia and generated a tsunami that damaged countries all over the Indian Ocean. In April 1946 a magnitude 8.1 earthquake struck near Alaskas Aleutian Islands and generated a tsunami that destroyed much of Hilo, Hawaii thousands of miles away. The PTWC was created in 1949 as a result. To learn more about tsunamis, visit the National Oceanic and Atmospheric Administrations Tsunami Website. References National Weather Service. (n.d.). Tsunami: The Great Waves. Retrieved from: weather.gov/om/brochures/tsunami.htmNatural Hazards Hawaii. (n.d.). Understanding the Difference Between a Tsunami Watch and Warning. University of Hawaii at Hilo. Retrieved from: uhh.hawaii.edu/~nat_haz/tsunamis/watchvwarning.phpUnited States Geological Survey. (22 October 2008). Life of a Tsunami. Retrieved from: http://walrus.wr.usgs.gov/tsunami/basics.htmlWikipedia.org. (28 March 2011). Tsunami - Wikipedia, the Free Encyclopedia. Retrieved from: http://en.wikipedia.org/wiki/tsunami

Two kinds by Amy Tan Essay Example | Topics and Well Written Essays - 500 words

Two kinds by Amy Tan - Essay Example She struggles to mould her daughter into fame but her efforts fail as her daughter is rebellious and lacks interest in her mother’s initiatives. The narrator however believes that she can only be her personality and not her mother’s dreams (Tan 132- 143). The narrator and her mother have a strained relationship that exists in two scopes, maternal and mentorship scopes, and identifies their conflict. The narrator’s mother plays her parental role of establishing a basis for her child’s future but the narrator does not appreciate her mother’s efforts. She instead believes that she can only be herself and is rebellious to her mother’s initiatives. At the peak of their conflict, her mother hints to the possibility of a worse interpersonal relationship when she explains that there are â€Å"only two kinds of daughters,† â€Å"those who are obedient and those who follow their mind† (Tan 142). She then declares that Jing, the narrator, can only live in the house if she is obedient and Jing regrets, in her mother’s face, being her daughter. The narrator’s strained relationship with her mother is further identifiable in her domestic orientation in which she does not help her parents when called upon to do domestic chores, a behavior that her mother identifies as a problem (Tan 132- 143). The narrator also identifies a poor relationship with her mother in the mentorship role. She does not appreciate her mother’s ideas and even though she communicates her feelings and attitudes, her mother ignores these and insists that Jing must follow her path to success. This generates a conflict that the two characters fail to resolve amicably (Tan 142). The strained relationship between the narrator and her mother develops from the mother’s high expectations in her daughter and her desire that the child attain fame. The mother’s strong belief that all achievements are

Dominant Cultures and Subcultures Essay Example | Topics and Well Written Essays - 250 words

Dominant Cultures and Subcultures - Essay Example Subcultures are mainly possessed by minority groups in the society and, therefore, have little or no influence to the dominant culture. Understanding the impact of culture is essential since one is able to learn people’s behavior. In essence, understanding the impact of culture facilitates proper planning of activities. In addition, one can study the behavior of others and make a proper judgment regarding people’s ethics. There are various avenues where cultural differences are clearly shown in the society, for instance, on religious matters and social structures. In many instances, people in the society have varied religious faiths and believe in different social constructions. Dominant cultures seem to control the political, socio-cultural and economic structures in the society. These differences in cultural constructions stress the need for comprehensive studies on culture diversity in order to know how to live harmoniously in a cultural diversified society. In order to embrace cultural diversity, the society should accept all cultures and provide a common ground for both the dominant and subcultures. In addition, proper education structures should be developed so that members of the society can learn the importance of cultural diversity. In summary, cultural diversity is an important feature for steering development in any community. In this regard, diversity should be encouraged in all spheres of