The Elite Report Essays - Electronic Music, MIDI, Fanshawe College

The Elite Report Music Industry Arts A Two Year Diploma Program Program Code MIA1 Grounds Code LC LC - London September Admission Program Description The Music Industry Arts program teaches understudies in every single significant part of the contemporary sound industry. The program advances the expert disposition required to work in the melodic, specialized and business zones of Audio Production Engineering and Business. The program approach is seriously active, with proficient media and recording offices only devoted to understudy use. Course educational plans incorporate elements of consoles and recorders, computerized recording, video interlock, MIDI account and sequencing, simple/advanced strategies, agreements, deals and advancement music distributing, copyright, organizing, music hypothesis, ear preparing, amplifier procedures, studio activity and the executives. PC proficiency and MIDI strategies pertinent to the controls of music and after creation recording are offered through hypothesis and pragmatic applications. Vocation Opportunities This program offers an interesting open door for learning the aptitudes required for the music recording industry, the after creation field, and general sound enterprises. The alumni may discover profession openings with sound account studios, after creation offices, recording organizations, marketing, visiting business specialists, journey ships, distributing, the executives, advancement, deals, MIDI/sound plan or studio recording for broadcasting and TV. Program Eligibility CriteriaRequired Academic Preparation OSSD with courses at the General Level with: - Grade 12 English Or BTSD-Level 4 Certificate Or Ontario High School Equivalency Certificate (GED) Or Mature Applicant with remaining in the necessary course expressed aboveRecommended Academic Preparation - Courses in Communications Technology, Keyboarding, Computer Studies, Marketing, Development of Entrepreneurs, Analog and Digital Electronics, Computer Technology - Interfacing.Recommended Personal Preparation It is a favorable position to the understudy to have an expansive foundation in music hypothesis, information and energy about a wide range of music, an enthusiasm for the chronicle business and its job in the present diversion field, involvement in PC and additionally synthesizer/MIDI applications.Applicant Selection CriteriaWhere the quantity of qualified candidates surpasses the accessible spaces in the program, the Applicant Selection Criteria will be: A. Inclination f or Permanent Residents of Ontario. B. Receipt of Application by February first. C. Accomplishment in the Required Academic Preparation. D. Accomplishment in the Recommended Academic Preparation. E. Appraisal of individual reasonableness dependent on: . Strengthening Form Estimated Costs (2000/2001)Fees for: Levels 1 and 2 Levels 3 and 4 $2143.90 Books and Supplies: $2613.00* $2087.00* *this expense remembers access to offices and gear for the program Recording Industry - Digital Applications A One Year Post-Graduate Certificate Program Program Code MRM2 Grounds Code LC LC - London September Admission Program Description The Digital Applications program is a post-graduate program which gives escalated handy guidance and application open doors for getting capability in the MIDI/advanced multi-media field through hands-on gear application and procedure situated guidance. Profession Opportunities Profession openings with sound chronicle studios, record organizations, free creation houses and other 'sound related' ventures, music distributing combinations and anyplace that 'sound' creation as well as blending is required. Program Eligibility CriteriaRequired Academic Preparation Music Industry Arts Diploma Or A comparable capability from another foundation as decided by the College Or Professional foundation and experience surveyed by the College to be proportionate to the aboveApplicant Selection CriteriaWhere the quantity of qualified candidates surpasses the accessible spaces in the program, the Applicant Selection Criteria will be: A. Inclination for Permanent Residents of Ontario. B. Receipt of Application by February first. C. Accomplishment in the Required Academic Preparation. Understudies applying for the Recording Industry - Digital Applications program with a multi year Music Industry Arts Diploma ought to have acquired a 'B' normal in all MIDI and RCRD or PROD courses in the second year of the Music Industry Arts program at Fanshawe College, or a 'B' normal in every single MIDI course from another organization. Candidates with not exactly a 'B' normal will be viewed as just on the suggesti on of the Program Chair. D. Inclination will be given to alumni of the Fanshawe College Music Industry Arts program, with latest alumni having priority.Note: Applications got by February first will be ensured thought. Applications got after February first will be viewed as just if places stay accessible in the program. Inexact Costs (2000/2001)Fees for: Levels 1 and 2 $2143.90 Books and Supplies: $2082.00

Free Essays on Sony In Ireland

With my enthusiasm for Sony as an organization and the way that I have a contributed future with an Irish family, I thought that it was important to pick this organization and this nation to investigate. As I separate Ireland as a nation and break down the business point of view taken by Sony, I plan to teach you on the worldwide business activities of such and what is important for progress. I trust you appreciate. Ireland is a republic incidentally connected with the United Kingdom. Its capital is Dublin and it is found northwest of Europe and involves around 83% of the island of Ireland in the North Atlantic Ocean. The absolute island zone is practically identical to the size of Alabama, of which Northern Ireland contains around 14,000 square kilometers. The atmosphere is moderately wet and temperatures are uniform all through the nation going from 40â º lows in the winter to 60â º highs in the mid year. Mountain areas along the west coast get most noteworthy precipitation at about 60 to 120 inches per year. Alongside such mountain ranges Ireland has a coastline of roughly 1440 kilometers. Ireland has a populace of around 4 million. The populace is for the most part focused on the east and south drifts with a thickness of 54 people for every square kilometer. The proportion of urban to provincial populace is 58% to 42% and generally 40% of the general populace is younger than 25. Christianity is the significant religion of the Irish individuals as 91% of them guarantee to be Roman Catholics and 2.5% having a place with the Church of Ireland (Forrest, 2002). Irish normal business customs are equivalent to those of the United States and Western Europe. The United States and Ireland are comparable in various perspectives, yet unmistakable in others. Ireland has a low force separation file (PDI). This implying subordinates may not hold up until their manager steps up to the plate. Representative co-assurance is basic standard, and anything an individual of intensity does might be tested by any subordina... Free Essays on Sony In Ireland Free Essays on Sony In Ireland With my enthusiasm for Sony as an organization and the way that I have a contributed future with an Irish family, I thought that it was important to pick this organization and this nation to break down. As I separate Ireland as a nation and break down the business viewpoint taken by Sony, I want to teach you on the global business activities of such and what is fundamental for progress. I trust you appreciate. Ireland is a republic sometimes connected with the United Kingdom. Its capital is Dublin and it is found northwest of Europe and involves around 83% of the island of Ireland in the North Atlantic Ocean. The all out island territory is practically identical to the size of Alabama, of which Northern Ireland contains around 14,000 square kilometers. The atmosphere is moderately wet and temperatures are uniform all through the nation running from 40â º lows in the winter to 60â º highs in the late spring. Mountain locales along the west coast get most elevated precipitation at approximately 60 to 120 inches every year. Alongside such mountain ranges Ireland has a coastline of around 1440 kilometers. Ireland has a populace of roughly 4 million. The populace is for the most part focused on the east and south drifts with a thickness of 54 people for every square kilometer. The proportion of urban to rustic populace is 58% to 42% and generally 40% of the general populace is younger than 25. Christianity is the significant religion of the Irish individuals as 91% of them guarantee to be Roman Catholics and 2.5% having a place with the Church of Ireland (Forrest, 2002). Irish basic business customs are practically identical to those of the United States and Western Europe. The United States and Ireland are comparable in various perspectives, yet exceptionally particular in others. Ireland has a low force separation file (PDI). This implying subordinates may not hold up until their supervisor steps up to the plate. Worker co-assurance is regular principle, and anything an individual of intensity does might be tested by any subordina...

The healthcare Law

The medicinal services Law The medicinal services law that was established this spring by the U.S. President Barrack Obama planned for giving U.S residents clinical spread. The law built up widespread clinical administrations to all U.S. residents and to be paid for by the government. The establishment of the law parts of the bargains private clinical protection in the nation that will currently give advantageous clinical inclusion. Promoting We will compose a custom exposition test on The medicinal services Law explicitly for you for just $16.05 $11/page Learn More The administration would finance the national human services through tax assessment and different supports that would supplant the health care coverage premiums that were at first paid by the residents. This paper looks at the use of financial ideas, for example, law of interest gracefully, balance and administrative choices on this human services law. Administrative dynamic Every association targets expanding the benefit made by the association. S o as to expand benefits, the association needs to limit costs. As per Png and Lehman, the administration of an association has an obligation to detail strategies and settle on choices that would prompt the accomplishment of the set objectives (36). Given that the business condition is dynamic, firm troughs for the most part depend on vital dynamic that includes creation of choices dependent on the systems that would amplify the utilization of firm assets. A portion of the key choices settled on by an association remember choices for cost minimization and successful use of firm assets. So as to limit costs, the administration guarantees that the operational procedures are effective, modest quality sources of info are used proficiently while making important items that fulfill customer needs. Basing on the administrative dynamic, the government is like the administration of associations. It needs to guarantee that all medicinal services needs of U.S residents are fulfilled. Consequent ly, it looked to fulfill the social insurance needs by setting up the national human services act that would be financed through tax assessment. This choice to sanction the demonstration is ideal on the grounds that the central government would set up a sound country that would add to financial development emphatically through expanded creation. Request, flexibly and advertise harmony According to Png and Lehman, the two purchasers and venders meet in a market in which there is the trading of products and ventures (121). Financial assets are as a rule hard to find while the necessities that are to be satisfied utilizing the assets are generally inconclusive. Moreover, various individuals and locales are offered with various assets that fulfill diverse human needs. Publicizing Looking for exposition on wellbeing law? How about we check whether we can support you! Get your first paper with 15% OFF Learn More Due to various blessing of assets to nations and districts, a few nations hav e a near bit of leeway in the creation of a given decent or administration over others. Furthermore, the distinctions in assets enrichment have made nations and people inside the nation to be subject to outside economies subsequently; they would consistently request the flexibly of given merchandise and enterprises for the satisfaction of their needs. The law of interest places that the requests for products and enterprises shrivel as the costs of the merchandise/administrations increments while different things are held consistent. Request is given as far as amount of the products. The amounts of merchandise that are requested by customers contrast starting with one individual then onto the next basing on different elements that influence request. Changes in the amount of a given decent/administration that is required by buyers varies after some time based different factors, for example, the degree of continues for shoppers, the cost of the great and accessibility of substitutes am ong different elements. The flexibly of products and ventures happens in the market as well. Providers give merchandise dependent on the amount of the products that buyers require so as to address their issues. The amount of merchandise/administrations provided is an element of numerous variables including the cost of the great/administration, level of pay for buyers, profitability and the measure of products/benefits that shoppers need so as to address their issues. The law of gracefully hypothesizes that the flexibly of a given decent/administration decays as the cost of the great/administration diminishes and the other way around with different variables being held consistent (Png and Lehman 357). Balance in the market is acquired at the level in which the aggregate of products/administrations requested by customers compares the degree of merchandise/administrations provided by various dealers in a similar market. At harmony, the cost at which the dealers offer their items to cli ents is alluded to as the balance cost while the balance amount is the amount provided by merchants and purchased by customers in the market. At harmony, there is no motivator for the providers to build the merchandise provided on the grounds that the cost and pay continues as before for the time being. Publicizing We will compose a custom paper test on The human services Law explicitly for you for just $16.05 $11/page Learn More Similarly, clients have no motivator to expand the measure of merchandise requested for the time being. The progressions in different factors in the business condition can cause the measure of products/administrations provided and requested in the market to change. A portion of the components remember changes for socioeconomics, salary and profitability among different elements (Png and Lehman 123). The financial ideas of interest and flexibly could likewise be applied to the medicinal services act. The clients in incorporate all U.S. residents that needs c linical consideration. The provider is the legislature. The degree of interest would increment if the U.S. populace expanded or the degrees of pandemic or mishaps in the nation expanded. The harmony in the arrangement medicinal services administrations to the residents would be accomplished at whatever point the provided administrations would be equivalent to the requested administrations. Streamlining strategies According to Png and Lehman, an improving firm should continue creating as long as the peripheral expenses caused during creation are not exactly the negligible income (183). During the creation time frame, the organization ought to consistently concentrate on limiting preparing expenses to guarantee that it meets its benefit amplification objective. An association should create until the level wherein the supernatural costs acknowledged over the span of creation are equivalent to the minor income. This is the ideal situation of the firm. Any expansion underway would bring about misfortunes. The administration of an association can modify this position if long haul creation limit is made. This can just occur in new administration apparatuses, for example, interest in new advances and extension of creation space and plant. The utilization of ideal procedures to the social insurance law would imply that the national government should build the arrangement of human services benefits as long as the peripheral expenses acquired in medicinal services administration arrangement is not exactly the negligible duty gathered by the legislature. The ideal degree of human services administration arrangement would be the point at which the negligible expense of the administrations is equivalent to the minor duty gathered. New choices to utilize trend setting innovation and increment human services administrations arrangement limit should looked for once the administration expands administration arrangement to the detriment of medicinal services costs. Customer cond uct and objective decision Organizations are associated with the creation of merchandise and enterprises while shoppers are essentially to settle on utilization choices for the delivered products. The hypothesis of interest proposes that purchasers request products (administrations) so as to meet their boundless needs. After the products/administrations are given, the buyers devour them for fulfillment that is estimated regarding utility. Publicizing Searching for article on wellbeing law? How about we check whether we can support you! Get your first paper with 15% OFF Find out More Buyers are normal in their utilization choices since they generally pick the best bin of provided products that would best address their issues given the predominant conditions. They in this manner choose the amount of products to buy and the measure of cash to spend on the merchandise. Given the judiciousness of customers, the human services administration shoppers in the U.S., the U.S residents are objective purchasers as well. They would settle on choices on the kind of social insurance administrations requested. In any case, the measure of cash to spend on the administrations would not be made by the residents, however by the national government through tax collection. Request capacities Demand capacities show the current connection between the degrees of the great requested and the determinants of the levels requested by the client. The amount of a given decent requested by purchasers is controlled by different factors, for example, the cost of the great, the degree of salary, t he costs of other related products, for example, praises and substitutes and tastes and inclinations. Given these variables, the interest capacity of a given decent can be communicated as demonstrated underneath. D=f(P,I,PXPYT) where D-amount requested, P-cost of the great requested, I-Income, PX cost of related great x, PY Price related great y and T-tastes and inclinations. Use of interest works in the medicinal services law The interest capacity could likewise be applied to the human services law and the interest of social insurance in the U.S. The U.S. residents are the buyers of social insurance administrations gave by the central government under the medicinal services law. The interest of human services benefits in the U.S is dictated by different factors, for example, presentation to hazard factors, levels of salary, cost of medicinal services among other factor. The medicinal services request capacity can be communicated as beneath. H=f(R,I,P, O) where H-human services amou nt requested, R-introduction to hazard factors, I-levels of Income, P-charge child the medicinal services and O-different variables An expansion in any of

Getting the Best Nursing School Personal Goal Statement Samples Essay

Getting the Best Nursing School Personal Goal Statement Samples Essay About the duration of your respective tutorial vocation, you're going to be asked for to compose a good deal of essays and papers on several subjects, based on the schooling routine. More than the period in your tutorial vocation, you could be asked for to compose a number of essays and papers on many subjects, based on the instruction routine. Over the period of a person's educational profession, you're going to be asked for to compose a lot of papers and essays on numerous subject areas, based on the teaching system. Over the period in your educational profession, you could be asked for to compose many papers and essays on many matters, based on the schooling procedure. Nursing School Personal Goal Statement Samples Essay Options Career goals for nurses are determined by the person. They need to envision what excellence looks like and recognize their role in attaining it. In reality, every personal nursi ng statement ought to be related to your career specifics. Your nurse practitioner personal statement has to be in a position to convince the reader you have a true passion for nursing and that you will put what you will learn to good use. Setting goals can help you decide what kind of nursing you would like to specialize in and the path you would like your nursing career to take. The trick is to be brief, particularly if you haven't been asked explicitly about your career progress. Planning a quick term and long-term goal sheet is going to be to your benefit. There are several career alternatives offered in the health care field. Bear in mind, goal setting is a normal activity that ought to be ongoing. Like every well-written tale, your private goal statement should tie the limit to the start. The goal also needs to be realistic in the quantity of time and skill it will require. My final aim is to acquire a post-doctoral certificate in pain administration. My short-term goals include advancing my understanding of quantitative research using I read your private statement with terrific interest. In truth, it is possible to satisfy with all the author on line and concentrate on your research. Fortunately our team consists of professional writers which possess the capability to create remarkable content for you. It's nice if it's a colleague who has somewhat similar objectives, but it may be someone in a whole different industry who's also hoping to generate a change or grow as a professional individual. You're during the right put as our pros are incredibly able to assist you with composition of any ty pe. You are likely to love our work. Regardless of what school, or what kind of statement you require, we can supply you with the assistance you're searching for. Nursing School Personal Goal Statement Samples Essay You are going to want to stand out, and the personal statement portion on the application offers you the opportunity to do it. Use the following ideas to gather the info you should make an exceptional statement. When you're writing your own personal statement for MBA programs, you'll want to ensure your document is genuinely flawless. Reviewing and revising your private statement guarantees that the piece is clear, organized, and totally free of errors. The principal plan of the general essay will likely be your thesis assertion. So for those who have an essay assigned that you will need help with, you can purchase essay online cheap from us. An essay could have plenty of intentions, even though the simple framework of all type of essays will likely be exact sam e. It can have a great deal of intentions, though the basic composition of all type of essays will likely be similar. Who knew essay writing might be so tough. So should you need to employ college essay writer online, we're just the people that you will need to contact. An essay can have a lot of intentions, although the elementary construction of all sort of essays will probably be very same. It is possible to easily buy unique college essays and don't neglect to tell friends and family about it.

How Fluoride Works to Prevent Tooth Decay

Fluoride is the fluorine ion added to toothpaste and dental rinses to help protect your teeth from cavities. While increasing the concentration of systemic fluoride (e.g., through fluoridating drinking water) has not been proven to reduce the incidence of tooth decay, direct contact between fluoride and teeth strengthens and helps remineralize damaged enamel. The Chemistry Behind Dental Health The calcium and phosphate compound which makes up tooth enamel is a modified form of hydroxyapatite, which is susceptible to attack by acids. Bacteria that thrive on the sugars found in the mouth multiply on dental surfaces and produce acids. Mechanical brushing of teeth dislodges these bacteria and rinses them away, but doesnt do anything to address the ongoing damage to enamel from acid exposure. Fortunately, saliva neutralizes these acids and teeth use compounds found in saliva to remineralize the enamel. So, as long as the rate of demineralization and the rate of remineralization remain in balance, teeth remain strong and healthy. When more minerals are lost from teeth than are replaced, dental caries or cavities form. Fluoride helps by interacting with hydroxyapatite to form a stronger compound that is less susceptible to acid attack. Also, fluoride remineralizes damaged enamel (though it cant fix a cavity once one has formed). There is some evidence fluoride may inhibit the growth of bacteria on teeth or limit their capacity for producing acid. Even though you spit out toothpaste and probably rinse your mouth, enough fluoride remains on your teeth and in your saliva to confer protection for a while after brushing your teeth or using a fluoridated rinse.

The Legal Regulation Of Sex Work Essay - 1473 Words

The legal regulation of sex work has become a key issue for many governments in an attempt to tackle the many issues and harms of the industry, many partially or fully decriminalising the industry. Sex work is an intensely complex issue, and even the concept of sex work as a ‘job’ is a contentious issue. Some feminist academics perceive sex work as inherently violent regardless of any regulations and therefore should not be legalised at all. However this in an idealistic notion as inaction and further criminalisation would only exacerbate the existing harms of the sex industry. The next issue to contend with is the partial or full legalisation of sex work, the partial legalisation of sex work, results in a two tiered system of sex work, resulting in higher levels of illegal sex work, as sex workers attempt to avoid the rigorous health testing, identity checks and bureaucratic tape. The only way to ensure all sex workers are working in a safe and autonomous capacity is th e full legalisation of sex work. Further sex work should be regulated in a similar manner to other industries, with full transparency and accountability in order to prevent moral bias and social control models from taking hold. The New Zealand licensing regulations and Australia’s own state laws are good examples of advancements towards the ideal, whilst international comparisons such as Sweden or the U.S. exemplify the negative impacts of partial decriminalisation and social control. While sex workShow MoreRelatedProstitution in America1528 Words   |  7 Pagesillegal. When I say for the most part I mean that in some counties in Nevada prostitution is legal. Downfalls of Legal Prostitution Prostitution is legal (with some restrictions) in Canada, most all of Europe including England, France, Wales, and Denmark. Most of South America including most of Mexico (often in special zones), Israel, Australia, New Zeeland and many other countries. It is either legal or very tolerated in most all of Asia and even Iran. Rapes and Violence EstimatesRead MoreProstitution Between Canada And Canada1712 Words   |  7 Pagesservices have been cautious (Warnica, 2015). Unfortunately, new laws may create more problems than benefits, such as, financial problems due to fewer people buying sex because it is illegal to do so. In this paper, I will explicate and assess the new changes to the law regarding prostitution in Canada, arguing that prostitution should be legal in Canada. Prostitution laws vary all over the world. Some jurisdictions are similar to Canada whilst others are extremely different. The United Kingdom is similarRead MoreShould Adult Prostitution Be Legalized?1262 Words   |  6 Pagespractice or occupation of engaging in sexual activity with someone for payment, (1). Prostitution to this definition is illegal in 109 countries and legal in 77, yet America doesn t fit into either of these categories. America is one of 11 countries where prostitution is restricted, however, this label can be quite misleadi ng. American prostitution is only legal in 11 rural Nebraska counties and is completely illegal in the rest of the country (2). While the legalization of adult prostitution is not aRead MoreThe Problem Of Sex Abuse Essay1519 Words   |  7 PagesShe was a sex worker and a mother of one. A recent law enforcement crackdown targeting sex workers led Mariana to work alone that night, rather than as usual with other women, to avoid arrest. She was also allegedly working late to pay a fine she had received for soliciting. Mariana’s tragedy is not uncommon. Sex workers are 400 times more likely to become a victim of homicide than the average worker. Current legislation regarding prostitution in the United States works directly against sex workersRead MoreThe Legal Acceptance Of Prostitution1608 Words   |  7 PagesThe Legal Acceptance of Prostitution Prostitution is often called the oldest profession in the world. One of the First forms is scared prostitution supposedly practiced among Sumerians. In ancient sources (Herodotus, Thucydides) there are many traces of scared prostitution, starting perhaps with Babylon where each women had to reach once a year the sanctuary of Militia and have sex with a foreigner as a sign of hospitality for a symbolic price. Prostitution is the sale of sexual services (typicallyRead MoreProstitution Is Legal Under Strict Regulations1516 Words   |  7 PagesProstitution in Germany Like many countries in the world, prostitution in Germany is legal under strict regulations. Prostitution in Germany dates back to many centuries and although it was never legalized, prostitution was never illegal and discrete brothels existed. In 2002, Germany implemented the Act Regulating the Legal Situation of Prostitutes that was intended to improve the legal status of prostitutes, improving the social position of prostitutes, improving working conditions of prostitutesRead MoreShould Prostitution Be Legalized?1048 Words   |  5 Pagesprostitution is the exchange of sex for money. Out of the 50 states in the U.S., Nevada is the only states were prostitution is legal. On the other hand, in some European countries prostitution is not illegal and its safety practice with proper regulations. Therefore legalization should not be the issue; instead regulations should be placed to make the practice of prostitution safer. There are more important aspects of prostitution that need to be addressed; regulations on moral, heath, and crime shouldRead MoreProstitution And The United States1044 Words   |  5 Pagesprofessions.Even though that it may increase sex trafficking, prostitution should be legalised in the United States because it would decrease violence and It would boost the economy. Men and women around the world are free to chose prostitution as their own profession, yet not in the US. Only one state has legalized prostitution and some want it made illegal there this would be a mistake as it would exacerbate the problems caused by it not being legal. Many people view prostitution as a deplorableRead MoreProstitution And Its Effect On Society Essay1630 Words   |  7 Pagesgovernment should, alongside prosecuting ‘victimless’ crimes, minimize the opportunity for the corrupt to create victims. Prostitution has been practiced in all ancient and modern cultures. In the United States, prostitution was originally widely legal. Prostitution was made illegal in almost all states between 1910 and 1915 due to the influence of the Woman s Christian Temperance Union which was influential in the banning of drug use and was a major force in the prohibition of alcohol. In 1917Read MoreShould Prostitution Be An Illegal Business?1533 Words   |  7 PagesProstitution is a controversial topic with a faction of the society arguing that the ancient trade should be legalized whereas the opponents insist that prostitution should be an illegal business because it is unethical. The commercial sex effects and its nature elicit divided opin ion because legalizing prostitution as a trade affects its characteristic as a gendered institution and social nature. A section of the society perceives prostitution as an unequivocal exercise of patriarchal control over

Ethical Decision Making in Business

Questions: 1. Does Craig appear to be doing anything wrong? Explain your response.2. Are threre any ethical issues involved here? If so, identify them. Answers: 1. Craig is one of the two stakeholders who are in an advantageous position both personally as well as financially because though he is not doing anything legally but he is making relative contributions that are not legal in a partnership business. However, being a partnership firm which as just commenced there is a high variability that most human endeavours may force the business which will not only challenge the cooperative spirit but will also lead to volatile combination of money and emotion (Thompson 2016). Although, as seen there is brief understanding between the two stakeholders that is Craig and Micelle but Craig is taking undue advantage of Micelles trust because his capital contribution has reduced from $60,000 to $20,000 as compared to Micelle whose capital contribution remains the same that is $50,000. Nevertheless, Craig is aware of his capital contribution in the firm but does not know that his reduction in capital contribution will still receive him more profit than Michelle. Though, in this partnership firm both partners contribute equally and are rewarded against the same capital contribution. Exceptionally it would be better if they share the profits equally such that the interest could be paid on the remaining capital balance to Michelle to avoid any partnership disputes (Bolden-Barrett 2016). Craig as a business partner is cheating on the other partner Michelle as he is committing a fraud because Craig and Michelle have come into business while believing that the other partner will be loyal and trustworthy. However, they have termed to be creditors who have put their capital contribution in the business. In this case, the partnership is in a case of Limited Liability Partnership where the law can be devoid if a fraud is committed when one of the partners poses the attributes of cheating (Morse 2010). However, Michelle is known by the fact that Craig has been withdrawing his capital contribution and contributing the money on a personal asset which means that Michelle is known by the fraud carried out by Craig. Nevertheless with this fraudulent act of Craig, either Craig could be told to reduce his capital contribution as mentioned earlier or the personal asset will now have no exclusive right on the assets and the asset will be reduced to share along with Michelle as the p roperty will turn into proprietary of the firm (Tricker 2015). 2. Michelle and Craig are its initial stage of partnership However, there is a need that the research partnership is decided based on the focus of the research. However, they follow shared decision making that not only highlights the transparent justification but also to follow the correct policies and procedures followed at the initialisation of the partnership agreement (Baker, 2012). Ethical partnership is maintained potentially on a streamlined processing. On the other hand, the two ethical issues that can lead to ethical concerns are given as: 1) Perceived disparity between contribution and reward The disparities between partners can arise when the partners are on the different question. However, the issue lies in the perception of the true reality (Mertens and Ginsberg 2009). 2) Breakdown in trust and respect Here, the main concern lies in the relationship trust and loyalty between the two factors which is at stake. However, if Craig carries on with this behaviour, this may erode the foundation of the business. Moreover, at last, the partnership cold even breaks down. Win Over Partnership Disputes Ironically, the partnership can win over disputes only if lands on success. However, disputes can be avoided on the following risks that could be avoided. 1) Each partner should have a brief understanding of the roles, expectations, responsibilities and the constructive discussion that could change over time. 2) The strengths and weaknesses of the partners should neither be underestimated nor overestimated (Fraedrich, Ferrell and Ferrell 2013). 3) The common vision should be established as both the partnership in this case, Michelle and Craig should share and revise business proceeds. The document vision should not arises the sense of dispute on the question of self-accomplishment first and then the business accomplishment (Thompson 2016). 4) The partnership should be inclusive of all issues under control by keeping an open as well as inclusive partnership that should possess the cliques of partnership and should not reflect lack of trust. However, Craig and Michelle should trust in a partnership as without trust there is no success for the business to proceed (Raftesath and Fitzgerald 2014). Conclusion To conclude, it can be said that there is need of trust and loyalty that is required to sustain the partnership. However, the role of success of partnership is only achieved if Craig does not withdraw his capital contribution anymore and even if he does, he needs to make a fair deal and deny the unjust profit he is receiving. However, disputes can be avoided if there is transparency, borne with key idea of success, sharing the profits and enhancing the weaknesses of the partnerships. References Baker, M. 2012.Choosing ethical partners: one institutions efforts to engage in ethical partnerships. acen.edu.au. Available at: https://acen.edu.au/2012conference/wp-content/uploads/2012/11/142Choosing-ethical-partners.pdf [Accessed 21 May 2016]. Bolden-Barrett, V. 2016.Partnership Ethics. Yourbusiness.azcentral.com. Available at: https://yourbusiness.azcentral.com/partnership-ethics-16406.html [Accessed 21 May 2016]. Fraedrich, J., Ferrell, L. and Ferrell, O. 2013.Ethical decision making in business. Mason, OH: South-Western. Mertens, D. and Ginsberg, P. 2009.The handbook of social research ethics. Thousand Oaks, CA: Sage Publications. Morse, G., 2010.Partnership law. Oxford University Press. Raftesath, D. and Fitzgerald, M., 2014. How healthy is your relationship with your business partners?.Australian veterinary journal,92(3), pp.N16-N16. Thompson, P. 2016.Partnership Disputes. thompsonlaw.ca. Available at: https://www.thompsonlaw.ca/pdf_folder/Partnership_Disputes.pdf [Accessed 21 May 2016]. Tricker, R.B., 2015.Corporate governance: Principles, policies, and practices. OUP Oxford.

Interview Narrative free essay sample

Interview Narrative With a loud creak, the door of my sisters apartment opens and in comes Brianna freshly from a long, hard day of work at the National Wildlife Research Center. She doesnt seem to be in the best of moods at first, but as soon as she sees me she cant help but grin, for we hadnt seen each other in months. She takes a seat beside me on the small yet comfortable couch in the center of her living room. As she had Just gotten off of work she remains in her work clothes, which consists of a classy black polo. Khaki pants, and a pair of dainty black flats. I let her relax for a couple moments and then I begin asking her questions about her past and high school experience. She then begins fondly reminiscing on her former memories of the activities, goals, and such that she had and took part in throughout high school. We will write a custom essay sample on Interview Narrative or any similar topic specifically for you Do Not WasteYour Time HIRE WRITER Only 13.90 / page She first begins by recalling the goals she once had throughout high school and what measures she took to try and reach them. Her biggest goal in high school starting from freshman year was to obtain a 4. 0 GPA and letter in academics. She studied awfully hard and really focused on her academics to attempt to achieve her oal. Unfortunately she did not reach this goal, l got very close, having all As and one B my sophomore year, she says disappointedly. However, it seems that she has made her way passed it as she says, It was kind of devastating if Im honest, but I mean what can I do now, IVe moved on. This then lead to a description of how the triumphs and trials she encountered helped her to be more prepared to face the world after high school. She describes high school as Just another four years of my life, and that what took place then doesnt really affect her regularly today. High chool showed me that if life brings you down, you will get back up, move on, and get through it; there is always a new tomorrow. Brianna seemed very proud to say that she took part in plenty of extra curricular activities at her high school. She played soccer from her sophomore year to Junior and was involved with FBLA (future business leaders of America) in her freshman year. Brianna also played softball and was in DECA from her sophomore year to her senior year, in which two of those years she was an officer in DECA. She took part in JROTC for two years, and in MECHA for all four years serving as president her senior ear as well. l tried to dip my toes in as many extra curricular activities as I could. I just loved being involved in extra curricular activities because in a way, they give you a sense of belonging, she says warmly. Under her breath, seeming as if she didnt mean for me to hear her, she admits that DECA was her favorite of the activities she was involved in. However, she noticed that I caught what she said and fondly said, l loved the people I was with in DECA, managing and organizing events such as MORP and I Just loved business in general. She feels that she lived her high school life to ullest extra curricular activity-wise however she regrets not attending some big events that took place while she was in high school. l do wish that I would have gone school to its fullest, however there was always a reason behind everything that I did and did not attend and to this day I stand by those choices. Brianna begins to dig deep as she recalls her fondest memory throughout her entire high school career. Her proudest and most memorable moment in high school was in her senior year when she happened to take 4th place at the State DECA Conference. l took 4th place in entrepreneurship written, which is one of the ategories, and I was the only one to compete by myself that year, writing a 30-page business manual and presenting it, she says humbly. Taking 4th at the State Conference brought her to the National Conference in Orlando, Florida. l was the only one from my high school that had made it to Nationals that year and it was nice to see how my 30-page business manual actually paid off in the end, and was totally worth the hard work and determination it entailed. With this achievement in mind, reminds her of some not necessarily downfalls that took place in high school, but something that she isnt particularly proud of. That certain something happens to be procrastination. Procrastination played a heavy role in her high school career because once she procrastinated something for the first time; it became a bad habit of hers. With indignity, she put her head down and said, Lets Just say I put the pr0 in procrastination. She looks back on one of her least proud moments that not surprisingly, had everything to do with procrastination. In my Junior year, I had a poster-presentation due in my fifth hour class, and on that very day that it was due I purchased a poster board from the high school in my first hour. In my first through ourth hour, I rushed through it and completed it and turned it in the board on time in my fifth hour and surprisingly ended up receiving a 100%. She felt that in this situation, she Just got lucky and highly suggests to everyone to not procrastinate for there are some but very few cases in which it may work out. I tried to consume as much information as I possibly could, and about midway through our discussion, it became so that she is now part of my motivation to obtain a successful yet fun high school experience. Currently, I have the same goal that Brianna once had, which is to get a 4. 0 GPA and letter in academics and to make her nd myself proud, I am going to try my hardest and push myself further than she did to achieve that goal. Also knowing that Brianna regrets not attending massive events such as dances or Friday-night football games, I now know that I should not miss out on such events, as I will most likely regret not going later on in life. Just as my sister did, I hope to take part in plenty of extra-curricular activities and hopefully, I plan to accomplish as much as she did in the clubs she took part in. Perhaps if I get into DECA my sophomore year I can work my way up and make it to the National Conference Just as she did. It became very clear to me that Brianna whom is my older sister is an inspiration to me in a way because she gives me motivation to achieve greatness and hope that there is always a new tomorrow. Its relieving in a sense to know that I will overcome the difficulties that I will be and am currently facing in high school. I began wrapping it up as I transcribed her last few comments, and thanked her for the time she took out her day to do this interview. I hope to use this information she gave me wisely and try to learn from what took place in her high school experience to make mine even more enjoyable.

Non-Hyphenation Is a Nonstarter

Non-Hyphenation Is a Nonstarter Non-Hyphenation Is a Nonstarter Non-Hyphenation Is a Nonstarter By Mark Nichol A friend of mine recently posted online a humorous observation to the effect that it’s ironic that non-hyphenation is hyphenated. In true word-nerd fashion, I figuratively cleared my throat and pushed my taped-together black horn-rimmed glasses up my nose before offering the deflating response that nonhyphenation does not in fact have a hyphen. (What are friends for?) My friend’s misapprehension is a common one. Hyphenation in prefixed words remains rampant in writing ranging from social media posts to scholarly journals, though style manuals have more or less long advocated minimizing their use. Why, then, the persistence of non-profit, multi-billion (as in â€Å"multi-billion dollar budget,† which errs also in lacking a hyphen before dollar), pre-approved, post-modern, and the like? First, some history: The hyphen began as an arc-shaped symbol called the enotikon, which was marked underneath letters in Greek script to denote a connection between two words. (The Greek term means â€Å"uniter.†) During the Middle Ages, a straight line with a similar role was adopted in Latin, and Gutenberg raised the symbol to the middle of the line of text, and furthermore adopted an angled double line resembling an equal sign at the end of a line, borrowing from writing of Latin script, when insufficient room remained to set an entire word with uniformly sized metal type, allowing him to break words to fit where necessary. (Many proofreaders who proof on paper still use an equal sign to denote a hyphen; the rationale for retaining the double line when marking proofs is that it is less likely than a single line to be missed or to be mistaken for an accidental mark.) The trend in English is to phase out hyphenation when terms become more familiar. British English has also historically been more conservative than American English about retaining hyphens not only in prefixed words but also in compound nouns, as in dining-room or shop-keeper, which are now in both forms of English open and closed, respectively; many such constructions were purged from the Shorter Oxford English Dictionary only in the last decade. Meanwhile, style guides strive to minimize inconsistency, but individual or regional preference and specialized occupational usage may resist progress. However, the most significant factor in the persistence of hyphens in prefixed words and in compounds may be that most people, including many professional writers, do not check dictionaries or style guides to verify or correct their assumptions, often relying on what they learned from (sometimes misinformed) teachers or from published resources- sometimes decades ago, before the hyphen became an endangered species in compounds and prefixed words. To recap (not re-cap): Hyphens in such constructions are the exception, not the rule. (They do have valid applications, as many DailyWritingTips.com posts discuss; search the site for â€Å"hyphen† or â€Å"hyphenation† for examples.) If you are inclined to hyphenate a prefixed word or a compound word, double-check a dictionary or a style guide for prevailing style before you commit yourself. There’s no hyphen, and thus no irony, in nonhyphenated. Want to improve your English in five minutes a day? Get a subscription and start receiving our writing tips and exercises daily! Keep learning! Browse the Style category, check our popular posts, or choose a related post below:Cost-Effective vs. Cost-EfficientItalicizing Foreign Words"Wracking" or "Racking" Your Brain?

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

Managment - Essay Example The storm of uprising had comprehensive results across North Africa. The businesses of many multinational companies had been majorly affected. The political volatility and financial breakdown have affected the global supply chain. Many European agricultural and textile companies have been defenseless to counter the uprising in the Middle East and North African (MENA) countries. The political risk in these countries has led to deteriorating financial condition and unavailability of credit. This scenario has brought forward payment risks for multinational companies which are operating in Middle East and North African region. The instability in MENA has created disruption in the oil industry and boosted the prices of petrochemical products. The risk of disorder in those countries has harmfully affected the supply chain and energy production companies (Dun & Bradstreet Limited, 2011). The uprising in Tunisia has increased the business risks. During the protests many business enterprises had shut down their operations. The retailing businesses were affected by raiding and the tourism industry had faced huge losses as travelers escaped from the country. Due to the uprising, the standard capacity consumption in the manufacturing industry reduced to 52.9%. Many banks were demoted by rating agencies and the credit access became limited in the global market (Dun & Bradstreet Limited, 2011). Egypt has followed a path similar to Tunisia. In February 2011, a series of revolutions occurred in many countries of Middle East, and Libya was surrounded by aggressive spiral of protests and it led to civil war. Due to the instabilities in Libya, Egypt and Tunisia the prices of oil reacted quite rapidly. It has been observed that further uprising will increase the price of oil even more and it can affect the business and international economy (Dun & Bradstreet Limited, 2011). Impact of Popular Uprising on Multinational Companies The impact of popular uprising has affected the busine ss and investment of many multinational companies. Libya embraces the most oil funds in Africa and it is the 15th biggest crude oil exporter throughout the world. The losses in Libya had quickly absorbed other countries. Due to the problems related to uprising many Western companies had suspended business operations in these countries. For example, BP vacated its employees and stopped the oil production in Libya. The Repsol–YPF of Spain suspended the oil production in the year 2011. OMV, which is an Austrian Oil related company, minimized their production due to the unrest. Further, the Royal Dutch Shell, Marathon Oil Co., and Wintershall also have started to evacuate their workers (Shanghai Daily Publishing House, 2011). Example of BG Group BG Group is one of the leading companies in international energy and power market. It is a UK based company and its operation is spread worldwide. In Tunisia, BG Group is the biggest producer of domestic gas which is accounted for almost 60% of total gas in Tunisia (BG Group plc, 2011). The uprising and civil unrest in MENA have affected the production of BG group. In the first quarter of 2011, the protestors of Tunisia had cordoned the workers of BG Group and stopped the business operations of the company. The company faced uncertainty due to the long lasting crisis of Tunisia and

How has Robot Technology improved emergency response and will this Research Paper

How has Robot Technology improved emergency response and will this technology impacts the future of search and rescue - Research Paper Example This paper will describe how robot technology has improved emergency response capabilities and how this technology will influence the future of emergency management, as well as search and rescue operations. In the modern world there is an imminent need for humanitarian operations ranging from small disasters to humanitarian tragedies. Some of these emergencies can be classified as natural disasters while others are human made or human induced. The typical emergency situation can also be a combination of any three of the elements listed above. In such situations, the general approach is to utilise search and rescue (SAR) teams and systems. It has to be kept in mind that the budgets being spent on emergency relief efforts especially for search and rescue efforts is increasing manifold every year. For example, the International Committee for the Red Cross (ICRC) spent some 958.7 million Swiss Francs in the year 2005 while it registered a 16% increase in its overall budget since 2000. This is comparable to the Medecins Sans Frontieres (MSF) who saw a budgetary increase of 13% between the years 2000 and 2004 (Ko & Lau, 2009). With these budgetary increases it must also be seen that most sea rch and rescue efforts feature human beings trying to resolve situations that may be out of their control. With the rapid advances in technology especially robotics, it is ironic that most search and rescue operations still feature dogs on leashes guiding human handlers to save lives. The very nature of emergency response is precarious to say the least. The advances in technology have been unable to feature heavily in these scenarios except for the isolated use of positioning systems, communication systems and camera mounted probing systems. The dangerous nature of these operations requires scapegoats that can tread not only further but also faster into emergency areas. It has been suggested that the

Pyramus and Thisby Essay Example for Free

Pyramus and Thisby Essay In spite of that, Bottom considers his acting to be remarkable, so remarkable that he thinks he can play all the characters of Pyramus and Thisby. I will roar you as gently as any sucking dove; I will roar you an twere any nightingale. Bottom feels that he is fully capable of playing the role of a gentle, charming Thisby, and even that of a monstrously horrifying lion. This characteristic of his is very effective in generating hilarity as he very naively presumes that he alone can handle the production of Pyramus and Thisby. Contrarily, his performance as Pyramus alone is rather alarming. Now die, die, die, die, die. Bottom tries exceedingly hard to convince the audience of Pyramus death. The word die is repeated four times, implying how incessantly Bottom tries to assure the onlookers that he is unquestionably dead. This initiates some final mirth on Bottoms foolishly absurd identity. Bottoms transformation into a donkey is another very amusing part of the play. What makes this idiosyncrasy all the more entertaining is his nescience about it throughout the play. I see their knavery. This to make an ass of me, to fright me, if they could. Bottom never realises the radical change he has undergone and very potently amplifies the hilarity of the comedy since he leads all his actions normally, never comprehending how abnormal he looks. Also very effective in this dialogue of Bottoms is the usage of the word ass as a pun. He is completely unaware that at the precise moment that he is uttering the dialogue, an ass is literally what he looks. His declaration of the other workmen making an ass of him is also humorous since his name Bottom already signifies his existence as an ass. Furthermore, is the levity of Bottoms romance with Titania. Unfamiliar with the fairies, Bottom is far from apprehending why Titania confesses love for him. Methinks mistress, you should have little reason for that. And yet, to say the truth, reason and love keep little company together now-a-days. Bottoms statement is greatly suited to the moment, not only to describe his situation but also that of the four lovers. Like Lysanders immortal line, The course of true love never did run smooth, Bottoms opinion goes well with the obstacles and complications that have developed in the play. Despite that, it does not stop the ridiculousness of his and Titanias liaison from augmenting the humour of the Elizabethan comedy. O how I love thee! How I dote on thee! Titanias love for Bottom is entirely unreasonable. Being the queen of the fairies, she has one of the highest ranks in the play, while Bottom being a workman, has the lowest. The fairies also consider themselves to be of a much higher position than mere human beings. In the face of this, Titania loses both mind and body to an ass-headed and ugly Bottom, a low class workman. This efficiently illuminates the impediments that the love juice can bring about and the thoughtlessness that attaches itself to all that encounter it. The central figure of this Elizabethan comedy is Puck, the mischievous sprite. He conducts all the melodrama of the play; all the confusion, all the mischief, begins with him. What, a play toward! Ill be an auditor, An actor too perhaps, if I see cause. Even before watching any of the drama, Puck has plans to play a part in it. Apart from being Master of Revels to Oberon, Puck forms a schedule of his own; he always satisfies his interests and curiosities. This makes the audience more cognisant of the trickery and complexities going on in the play. Not being related to either the fairies or the lovers, the mechanicals have no reason to be a target of Pucks pranks. Correspondingly, his involvement in the disruption of their rehearsals proves how he has his independent diversions. The roles and traits of Theseus, Hippolyta and Philostrate are rather similar to those of Oberon, Titania and Puck. In theatrical performances of A Midsummer Nights Dream, the actors playing the roles of Theseus, Hippolyta and Philostrate often tend to play the roles of Oberon, Titania and Puck, respectively. In relation to this, Philostrate and Puck have analogous characteristics as Master of Revels. At the beginning of the play, Theseus tells Philostrate to spread celebration and joy of the marriage of Theseus and Hippolyta. Stir up the Athenian youth to merriments, Awake the pert and nimble spirit of mirth, Midsummers Eve was traditionally a time for celebrating with decoration, greenery and a sense of magic. Philostrate obeys the orders of Theseus as Puck obeys Oberon. Puck enters the play as a reflection of Philostrate, spreading magic and havoc with a mischievous side to all his intentions. Notwithstanding, Puck does make a critical mistake amidst his effervescent pranks. The highlight of the play is Pucks misunderstanding of Lysander for Demetrius. Did you not tell me that I should know the man By the Athenian garments he had on? Puck makes an easy error with the love juice. Asked to recognise Demetrius by his attire, he mistakes Lysander for him. This is sure to instigate some tension on the audiences part as they realise that something confusing can happen with the application of the love juice to the wrong person. It also potently marks an Elizabethan comedy because it opens the second phase of the play, where chaos is at its peak. The love juice is the key element of this romantic comedy. Love and friendship turn to hatred in a moment, and vice versa. Injurious Hermia, most ungrateful maid, Have you conspired, have you with these contrived, To bait me with this foul derision? Helena accuses Hermia of deliberately setting up Lysander and Demetrius love for her, to mock her and humiliate her. The love juice has unconditionally distorted the relationships amongst the four lovers. The purpose and positions of love and hatred have interchanged. The circumstances change over in a moment and later, go back to normal in the bat of an eye. This efficiently improves the prospect of a dream. The onlookers will themselves be forced to wonder if all that had happened was real, or just an illusion. Despite the fact that love and companionship instantaneously transfigure into repugnance, all the anger and vexation lacks asperity. Get you gone, you dwarf, You minimus, of hindering knot-grass made, You bead, you acorn. The bitterness amongst the lovers tends to be somewhat mild reflecting that past love has suddenly changed into enmity. The insults, although vociferated under strain and anxiety, do not come across as seriously as they are interpreted amongst the lovers. This helps in enriching the humour. The words dwarf, bead and acorn are tiny, pleasant things that have been used as objects of offence. Construed seriously amidst the characters, these insults are catalysts to laughter from the viewers as they hardly initiate any anger or humiliation. When the plays focus returns to the centre of civilisation in Athens, there is harmony, peace and the order of matrimony for all couples. Marriage itself is one of the chief traits of an Elizabethan comedy. During the Elizabethan era, comedies customarily followed the pattern of order and peace at the beginning, followed by extreme chaos, and ending in harmony with a marriage to mark the return of order. It can hence be concluded that A Midsummer Nights Dream is a thoroughgoing Elizabethan comedy. Yet, throughout the play, the lovers and their love is made fun of. Cupid is a knavish lad, All the love and its intricacies, the anxiety, loss, sorrow, bereavement and broken hearts are the exquisite ingredients of a first-rate tragedy. Nonetheless, A Midsummer Nights Dream is intentionally developed as a romantic comedy, with the disruptive elements to mark its midst. The viewers can efficiently see all the arcane aspects of love and devotion, and at the same time, enjoy the humour of romance. The ending of the play is greatly suited to finish off the confusion and misunderstandings of the past. In the epilogue, the actor playing the role of Puck steps out of character to accost the viewers. That you have but slumbered here No more yielding but a dream, The audience is addressed with an apology for any unsatisfactory or offending presentations. This helps in ending the show on a merry and cordial note. The mention of a dream creates the perfect theme for the epilogue; it relates back to the situations of the four lovers where complexities and discords were passed off as a dream. In my opinion, William Shakespeare has been tremendously successful in portraying this play as Elizabethan comedy. I liked the structure of order at the beginning, followed by despair and disorder and an ending with marriage to restore happiness for all. A Midsummer Nights Dream is by far the best play of William Shakespeare that I have read. I have loved the storyline and the humour as well the legendary characters.

Shakespeares King Lear - The Redemption of King Lear Essay -- King Le

The Redemption of King Lear It is said that no other playwright illustrates the human condition like William Shakespeare. Furthermore, it is said that no other play illustrates the human condition like King Lear. The story of a bad king who becomes a good man is truly one of the deepest analyses of humanity in literary history; and it can be best seen through the evolution of Lear himself. In essence, King Lear goes through hell in order to compensate for his sins. Lear's relationship with his three daughters, Goneril, Regan and Cordelia, is, from the beginning, very uncharacteristic of the typical father-daughter relationship. It's clear that the king is more interested in words than true feelings, as he begins by asking which of his daughters loves him most. Goneril and Regan's answers are descriptive and sound somewhat phony, but Lear is flattered by them. Cordelia's response of nothing is honest; but her father misunderstands the plea and banishes her. Lear's basic flaw at the beginning of the play is that he values appearances above reality. He wants to be treated as a king and to enjoy the title, but he doesn't want to fulfill a king's obligations. Similarly, his test of his daughters demonstrates that he values a flattering public display of love over real love. He doesn't ask "which of you doth love us most," but rather, "which of you shall we say doth love us most?" (I.i.49). It would be simple to conclude that Lear is simp ly blind to the truth, but Cordelia is already his favorite daughter at the beginning of the play, so presumably he knows that she loves him the most. Nevertheless, Lear values Goneril and Regan's fawning over Cordelia's sincere sense of filial duty. ... ...e and determination to repair his life is evident at this point, and continues to show for the duration of the play. Perhaps Lear's most difficult moment to endure is when he discovers his youngest and most prized daughter, Cordelia, dead. His initial reaction is of unbearable pain, but, being in his current state of madness, some of the anguish is alleviated when he "realizes" that she is alive. The king overcomes his earlier mistakes only after losing the one daughter who truly loved him. It's debatable whether Lear is completely conscious of his loss, but more plausible to suspect he is not fully affected by it as he is no longer in his right mind. Finally, Lear has dealt with the consequences of his decisions and is redeemed. Work Consulted: Halio, J. The Tragedy of King Lear. Cambridge: Cambridge University Press, 1992.

Hudson River: a Detailed and Comprehensive Geological History

Contents Introduction†¦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‚¬ ¦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‚¬ ¦.. 2 Hudson River Formation†¦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‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦.. 5 Hudson Canyon†¦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‚¬ ¦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‚¬ ¦12 Glacial History†¦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‚¬ ¦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‚¬ ¦.. 14 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‚¬ ¦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‚¬ ¦17 Bibliography†¦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‚¬ ¦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‚¬ ¦18 Maps & Diagrams†¦.. †¦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‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦. 19 Hudson Canyon†¦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‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦.. 19 Geological Processes†¦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‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦. 2 1|Page Introduction In 1872, a naturalist and surveyor by the name of Verplanck Colvin found the source of the Hudson River. It is a small pond on the south western slope of Mt. Marcy, the highest peak in the Adirondacks, called Lake Tear of the Clouds. So little is Lake Tear of the Clouds that if no water was to feed it for seven days it would be reduced to just an empty basin. Nevertheless, the Hudson starts right in its waters. One could say the Hudson River is divided into two distinct sections differentiated by geology and appearance.The first section winds its way through the Adirondack Mountains spanning 166 miles from Lake Tear of the Clouds to the Federal Dam in Troy. This section is un-navigable by boat and in some places somewhat rapid. The second section, which is quite different from the first, starts at the Federal Dam and runs for 149 miles through the â€Å"rolling hills† all the way to the Narrows between Brooklyn and Staten Island. Back up north at Lak e Tear of the Clouds is fed by natural springs and runoff from the sheer steepness of Mt. Marcy and other streams winding down from the high peaks of the Adirondacks.Throughout the whole Adirondack mountain range, the watershed drains and dumps runoff from 3,400 foot peaks into the lowlands less than 410 feet above sea level. From Lake Tear of the Clouds [in the space of a mile] the river drops 1,000 feet down a deep trench to join the Opalescent River1. A bit more southward, the Mohawk River drains much of the runoff from central New York into the Hudson. In fact, over half of the Hudson Rivers water volume comes from the Mohawk, and without it, the Hudson would be practically non-existent.Further south of Albany tributaries flow westward to the Hudson from the Taconic Mountains and eastward from the Catskills. Still further south the tributaries for the Hudson begin to appear rectangular, almost following the trend of the faults and 1 The Opalescent River is not a separate river f rom the Hudson but merely a section named by old Native American tribes. 2|Page ridges that run northeast to southwest of the river while other tributaries join at right angles to the faults along the joint planes.At this point in its path, the river begins to occupy its original bedrock gorge formed millions of years ago, flowing over rock ledge rapids and the coarse cobble point bars2 that are very common from Mt. Marcy to Glens Falls, until it is partially blocked by mountains. It is here that the river makes a sharp turn to the east and flows through the Luzerne Mountain gorge in western New York and then emerges quickly onto glacial lake sediments deposited in the Pliocene Glaciation and forms a very broad, almost meandering path on the lowlands (supported by shale) for the nearly 130 miles to Newburgh.South of Newburgh the river cuts laterally through the hard crystalline rocks of the Hudson Highlands, shifting back and forth in its valley (almost like a cradle) until it emerg es from the highlands and starts to exhibit fjord like characteristics within the towering rock walls around it. The river’s course then slightly curves in front of the Palisades escarpment3, which towers more than 328 feet above the water’s surface. At the Narrows the Hudson breaches its final barrier, the terminal moraine4 of the last glaciation (more on this in the Glacial History section) before it reaches the Atlantic Ocean.At the Atlantic (although tidal) the Hudson behaves as any other river would and deposits its bed load (sediments carried by the river) and some of the fine-grained suspended load (basically fine grained sand and dirt floating in the water) into the form of sandbars. Over millions of years, these have contributed to building up many islands including Staten Island, Hoffman Island, Swinburne Island and many others. The very low slope of the Hudson plays a great role in the amount of discharge and island buildup, too, as it only rises about 0. 4 inches per mile for the last 150 miles of the rivers path. To give some perspective, the Mississippi river rises approximately 6 inches per mile during its course, and discharges about 700 million tons of sediment per year into the Gulf of Mexico 2 Coarse cobble point bars are essentially pointed cobble that has been piled into bar like formations. These formations are generally formed when sediments carrying cobble leave it behind. 3 Ground formed into a steep slope as part of fortification. â€Å"Moraine† is a word used to describe the earth, stones and debris a glacier deposits. â€Å"Terminal† describes that these items were deposited where the glaciers maximum extent was, in this case Long Island. 3|Page and its mouth is approximately a ? -mile wide. The Hudson River discharges about 175 million tons of sediment per year and its mouth is about the same width at a ? mile. With a 2 inch increase in slope geologists predict the discharge rate of the Hudson would spik e up to about 450 million tons per year and the mouth of it would close up to about 250’ wide.This would place Manhattan underwater and greatly limit boat traffic as well as make Long Island more of a true island separated from land by at least 3 miles or so of water5. And so, the geography of the Hudson River today ends here in Manhattan, but the geology of what lies underneath is much more important. Continue reading if you must, and dwell into a mystery of time and a lot of pushing and pulling. 5 Do not worry about this happening now though because the rivers overall slope has not changed more than a centimeter in the last couple thousand years and shows no signs of speeding up. 4|Page Hudson River FormationThe Geology of the Hudson River is complex. Billions of years of folding, pushing, pulling, separating, and moving have formed, deformed and reformed the Hudson River valley into what it is today, a â€Å"giant palimpsest6, a great parchment on which the hand of nature has written and rewritten her bold signature for more than a billion years†7. In the next section, I am going to attempt to condense over a billion years worth of Geologic History into less than ten pages. Despite complex knowledge and strange words it is a simple story of time and rocks, moving and changing: the formation of the Hudson River and its valley.The Hudson’s geological â€Å"personality† very much reflects its structure and the changes made on it, underneath it and all around it from the Pleistocene glaciations8 . The bedrock foundation of the Hudson was established in the space of three oregany’s (mountain building periods) beginning over a billion years ago. These mountain-building episodes re-triggered long intervals of underground erosion and periodic submersion by the epicontinental seas (or oceans) to help start forming the Hudson River Valley. At a point much later in this story, glacial erosion reshaped the landscape of the HRV into wh at it appears as today.The first major mountain building episode, the Grenville Orogeny began about 1. 2 billion years ago. It was one of the biggest Oregany’s and affected a broad region along the coast of what was Ancient North America, from the northeast waters of Canada to northwestern Mexico. The mountains created by the Grenville Orogeny were most likely as tall as or taller than the Himalayas and were driven to these heights by a collision of Laurentia (Ancient N. America) and Gondwana (Africa) in which Gondwana overrode Laurentia. The deep burial of Laurentia resulted in the first 7 Written upon, or engraved on more than once. The Hudson: A History, Chapter 1: The River and the Land, pg. 10 8 A period of ice buildup to form glaciers, or the act of glaciation. 5|Page metamorphism, partial melting of rock and the separation of the light and dark minerals found in the Adirondack gneisses9. Many hundred thousand of years later in the Proterozoic period as the continents p eriodically moved, basaltic volcanic rocks merged into the mountains cutting the anorthosites10 and gneisses laterally across.These gneisses are around one billion years old, while the Highland gneisses may be a bit older. The Fordham gneisses are the youngest and can be dated to just under a billion years old. Over the millions of years, long episodes of erosion on the Grenville Mountains and constant lifting of the crust have brought it to the surface. Later in the Proterozoic period, erosion of this crust formed and provided a thick source of sedimentary deposits that partially submerged the upland area of coastal Laurentia (presently this is the area south of and parallel to the Appalachian Mountains).These deposits are now found mostly in the Appalachians, with almost all of them have been removed from the Hudson valley, leaving hard rock and clay for the Hudson River to rest on. In the early Paleozoic, the sand and gravel that was eroded from the mountains during the Proterozo ic period became basal sandstone and conglomerate11, which is more commonly known as the Potsdam Sandstone in northern NY and the Lower Quartzite that is prized throughout the Hudson Highlands.As the Epicontinental sea inundated this (once) mountainous region the sandstone and Lower Quartzite were buried under a thick cover of marine limestone and shale, which was laid down in an elongated trough that formed on the continental shelf where mountains had once been. The limestone was mostly deposited on the shallow edges of the trough while the shale solidified from the mud carried into the deeper seaward part of the trough. The solidified shale then created the bedrock between Glens Falls and the Highlands. 9Coarse, grained metamorphic rock composed of quartz, feldspar and mica. An igneous rock made up largely of soda-lime feldspar. 11 Rock composed of rounded fragments of various rocks cemented together in a mass of hardened clay and sand, like a composite. 10 6|Page In the Late Camb rian period,12 Laurentia once again collided, but this time with the ancestral core of Europe, Baltica and a large fragment of what is thought to be the continental crust known as Avalonia. This started the mountain building period known as the Taconic Orogeny, which lasted throughout the Ordovician Period.The Taconic Orogeny also resulted in the new supercontinent Laurasia. While much of the activity involving this collision took place well to the east it also affected the HRV. Island arc volcanic structures such as the Cortlandt Complex have been found in the Hudson Highlands. To the North and West in the mid-Hudson Valley, the sedimentary rocks that were deposited in the early Paleozoic Period were folded (with the trend of the folds and faults already in place) parallel to the southwest to northeast facing the Appalachians.These folds and faults eventually became some of the paths of the HRV tributaries. Closer to the coast than these faults, thin sheets of rock were pushed seve ral dozen miles west. This event is known as the Taconic Thrust and took place in the area where today exists the Taconic parkway. Because of this event, the fine-grained shale that was there was crumpled (as if we crumple paper) and pushed into the narrow channel of water west of the mountains near present day Croton. Over many years thereafter blocks of limestone into the channel and were merged into a jumble of shale clumps.Today millions of years later the river flows past the western edge of the channel and then cuts into the disorganized deposits of shale as it continues south. As we travel through time, sandstone, limestone, shale and Proterozoic bedrock from the Hudson Highlands became buried as Laurentia’s coastal margin was subducted13 close to where it and Europe’s plates met. The rocks that met each other from each plate partially melted and transformed into more gneiss, marble and schist14, which was then folded and moved once more to be in alignment 12 00 million years ago Subduction can be described as the action or process in plate tectonics of the edge of one crustal plate descending below the edge of another, almost like a controlled earthquake. 14 Schist is a metamorphic crystalline rock that has a closely foliated structure and can be split along approximately parallel planes. 13 7|Page with the Appalachians. This set the stage for the modern day continental shelf to form, although it would take millions of more years for it to happen. After the two plates of Europe and Laurentia collided, there was a sort of lull in activity around this area.This allowed streams in the lowlands to follow the valleys formed along the fault lines, or on the softer marble layers around Manhattan. The oceanic crust borders and the rocks around NYC and to the east more or less contained the streams around Manhattan, while the streams in the lowlands and around our area were free to roam and spread out. After the Taconic Orogeny ended, a long inter val of erosion began stripping away the excess crust as the â€Å"new† continent (modern North America, or Laurasia) was very slowly lifted by the compression of the plates.As the upland area was eroded away the epicontinental sea gradually filled the Hudson Valley region from the low lying land of the coastal margin all the way west nearly three-quarters of the way to Pittsburgh. Later during the Silurian and into the early Devonian period shallow seas covered the area and left behind calcium carbonate sediments making the soil very rich. At around the same time rivers formed and flowed from the uplands carrying major amounts of sediment west to the sea to form marine sandstone.While the marine sandstone was being formed, at the shoreline a large delta15 formed over the junk that the marine sandstone left behind. By the midDevonian period, an alluvial plain16 had reached across much the western Catskill region and the shoreline had shifted slightly west about 15 miles or so. At this time, thousands and thousands of feet of sediment from mid-Paleozoic times were piled up over the Hudson Valley and continental red sandstone (one reason why there is so much sandstone around here) from farther east inland were incorporated with the gray marine sandstone from the west closer to the coast.The force of all this happening at once overturned the folds that were in place to the northwest (near present day Schunemunk Mountain along the NYS thruway near Highland Mills) exposing the limestone that 15 A Delta is a triangular alluvial plain, usually where a rivers mouth is. A level or gently sloping flat or a slightly undulating land surface resulting from extensive deposition of alluvial materials by running water 16 8|Page was buried slightly underneath the sediment that had accumulated over the years. This marked the end of the Devonian Period, and the start of the Acadian Orogeny.The Acadian Orogeny began as the North American plates started to compress again and lift up the eastern mountain ranges around New England and western Pennsylvania. This Orogeny was also partially caused and linked to the collision that happened between Laurentia and Gondwana that created Laurasia, and most likely, if this Orogeny had not happened the Hudson River would be a completely different river, and possibly would be connected to the Mississippi River. As the plates began to compress each other again they created volcanic arcs and granite intrusions somewhat east of the Hudson Valley near the coast.Around this time in our little history story the seas started to retreat from the east to west and started to expose the incredibly thick layer of sediment and rocks from the Acadian Mountains all the way to the Catskills. The final compressions dating back to the Paleozoic era continents and the Alleghenian Orogeny now ended and the earth came together to form Pangaea. Because of all this land being pushed up, the Epicontinental Sea retreated from the Catskills to the Poconos in Pennsylvania leaving much of New York and New England dry once again.Now above sea level the strata from the Devonian period became subject to erosion for 250 million years. At some point during this time, the drainage patterns shifted and aligned the ancient Hudson River along a NorthSouth line much like it is today. This was the biggest directional change the Hudson ever underwent. As the strata and sediment were worn away from this new path of drainage, it revealed the granite, marble and schist underneath which became the building materials for our modern world.With the Taconic Mountains now more to the east and the Catskill Mountains to the west the Hudson worked its way down deep into the sediment it was on top of leaving behind a hard bedrock base nearly 5,000 feet deep in places17. This created a solid foundation and left the Hudson with a relatively stable path 17 Over the last several million years, and an Ice age this has all been filled in and now the H udson has an average depth of 32’. 9|Page that has not changed tremendously since. The breakup of Pangaea followed soon thereafter and the coastline of North America began to resemble what it is now.At the same time, the Hudson was filling its banks; basaltic magmas were merged along the fault lines and into the bedrock forming the Palisades Sill18. After that, compression and buildup of sediment and rock slowly built the Palisades up. Today the part of the Palisades that stands is almost like a canyon above the Newark Basin. The â€Å"tabular†19 Palisades still slope to the west, and the eastern edge forms the escarpment, or â€Å"palisade†20 21 of rock joined vertically that we recognize today from miles around New York and from the air as we fly to new places and heights.But to learn how, we must travel to another time in this story, the Mesozoic Period. Some time in the late Mesozoic period, igneous rock deposits were moved yet again and placed along a line going Northwest to southwest from Canada to New England lifting the mountains in its path by several hundred feet and in some cases over 1,000 feet. Because, as you might infer, rock takes up space, and as it lifted up the mountains and separated them, it started to separate North America’s continental plate away from the mid-ocean ridge22 and over a very hot area above the earth’s layer of magma near where the present day Appalachians exist.This caused what geologists think was a shot of magma that melted through that particular part of the plate (which was quite thinner than today) and uplifted the Northern part of the Appalachians. This, in turn reactivated erosion and brought the domed like anorthosites to the surface which is most likely the reason that the Appalachian Mountains are not scraggly and sharp like the Alps, but more rolling with large boulders and open expanses of rock. The Catskills and Adirondacks also experienced lifting, but in a much smaller amou nt. Almost at the same time as all this uplifting was happening, a 18 19Think of this as the palisades foundation. L. Sirkin & H. Bokuniewics – The Hudson River Valley: Geological History, Landforms, and Resources pg. 17. 20 L. Sirkin & H. Bokuniewics – The Hudson River Valley: Geological History, Landforms, and Resources page 17 21 Palisade literally means â€Å"a fence of stakes for defense† The Palisades are called the Palisades by Native American Tribes because they helped as defense for them from other tribes. 22 The mid-ocean ridge is a undersea mountain ridge that is where the North American and European plate meet. While this ridge has hardly ever changed, the plates do move.In this case it is the biggest moves it has ever made. 10 | P a g e hole began to form from sinkholes on the western slope of Mt. Marcy and soon filled with water. This was Lake Tear of the Clouds. After Lake Tear of the Clouds formed and filled with water, the Newark basin reached i ts fullest capacity of water and the Hudson began to â€Å"drive† into its flood plain and carve out its gorge in the gneisses of the Highlands of southern New York. This area is now mostly between West Point and Hastings on Hudson, but it continues as a much smaller â€Å"weaker† gorge almost down to Fort Lee.The Hudson was now a true river, but would still undergo massive changes over the next several million years. At this time in the Hudson River’s history, Long Island did not exist as what it does today. It was a tiny, almost alcove piece of land that was in no way an island. In addition to that, there was no opening to the Atlantic for the Hudson. At the place where the Hudson empties into the Atlantic at the Narrows was a big solid mass of land. The Hudson by definition was a lake. So, as the Hudson filled up and he water put immense pressure on the piece of landmass blocking it from the Atlantic it began to carve out and widen an outlet. It took only a f ew hundred years23 for the Hudson to make it to the Atlantic, bringing with it thousands upon thousands of tons of sediment that had piled up in the Newark Basin. This created the new continental shelf to form the coastal â€Å"plain† we see today that stretches for about a hundred miles out to sea from New York, only in that time and age it stretched for nearly 425 miles, nearly halfway to Bermuda.The Hudson now had an outlet, and the waters started moving south digging, and bringing sediment to the mouth building up Long Island a little bit24, as well as separating it from the mainland with what is now the East River. The sea levels around North America also dropped a few centimeters as the waters made their way up the Hudson forming the Hudson River estuary. This raised the Hudson’s waters by a few centimeters and created its almost permanent banks that have 23This is an extremely short time in geologic history and greatly shows how much the pressure was on the land mass blocking the Hudson from the Atlantic. 24 Although Long Island did get built up at this time, the majority of it was built up during the last ice age nearly 20,000 years ago. 11 | P a g e not changed very much since. Because the sea levels were much lower in that time period the Hudson also began its excavation of the Hudson Canyon with the help of the naturally occurring currents (more on this in the Hudson Canyon section) and more than doubled its length to nearly 895 miles (about 1,440km) long.After nearly 500 million years the Hudson rivers formation had ended and all that was left to change it was its own water wearing away at its bottom and a glaciation that would come in a few million years. Hudson Canyon The Hudson Canyon is possibly the biggest mystery of the Hudson River. How did it form? When exactly did it form? Why did it form? These are all questions geologists and hydrologists ask when looking at it. Most people in fact have never heard of it. To them the Hudson is a river that starts in the Adirondacks and ends at the narrows.To the few that know of the Hudson Canyon, the Hudson River starts in the Adirondacks and ends nearly 925 miles south halfway to Bermuda right after falling over a half mile down a [now] underwater canyon and then fanning out and spreading to the Atlantic Ocean. There, even though underwater it still carries small amounts of the Hudson’s freshwater (out to sea), and most geologists still consider it a part of the Hudson. This makes the true length of the river from Lake Tear of the Clouds to the end of the Hudson Canyon 922 miles, more than double of what we consider the â€Å"Hudson†.As explained in the last section (Hudson River Formation) in the late Mesozoic Period the Hudson River broke the land barrier that held it from emptying into the Atlantic. When it broke the barrier it began to carve a new path out to sea towards Bermuda. At some point, it reached the Continental Shelf and dug into it creati ng a canyon that eventually connected the shelf to the ocean basin, which is about 1. 5-2. 5 miles deep. Technically the canyon begins as a natural channel many miles wide at the mouth of the Hudson in a depression about 12 feet deep in the rivers bed. It 12 | P a g e ontinues then through the Hudson channel and under the Ambrose light25. Soon after the Ambrose light, it reaches the shelf and goes through the real canyon part of it that is called the Hudson Canyon proper. The Hudson Canyon proper is located about 100 miles east of Battery Park City and has walls almost ? mile in height, which can be compared to the Grand Canyon whose cliffs are about 1-1/8 mile deep. The Hudson Canyon is the largest â€Å"submarine† canyon in the United States, partially due to the currents that pass over, and carrying away sediment and rock, thus carving it deeper and deeper.Over the past 30 years since it was discovered, tracking equipment has logged a nearly 12-inch change in its depth and width making the Hudson Canyon also the fastest growing canyon in the Atlantic Ocean. At the same time it is growing wider and deeper, it is also getting closer to the magma underneath and behind the continental shelf. In simple terms, one day in the next couple hundred or thousand years it will break through and magma will come out creating a new island, possibly connecting the East Coast of the United States with a land bridge that extends more than halfway to Bermuda.Many tributaries around the canyon would be raised by the magma, creating a new network of rivers and streams on the land bridge that could host many kinds of wildlife as well as marsh like environments. In addition to this, the Hudson Canyon has large stores of methane hydrates which according to scientists is a very promising clean burning natural energy source, and could help reduce oil consumption. It is a Canyon of great importance to the Hudson River, and also a big clue into the Glacial history surrounding th e HRV. 25The Ambrose light is the site of a Light House that ships going into the New York Harbor and other harbors in the area use for navigation purposes. 13 | P a g e Glacial History The Glacial History of the Hudson River is probably the one of the most important geological event that happened in the Hudson Valley in the last 50,000 years. Evidence points mostly to the Pleistocene Glaciation, which was the last and only Glaciation to reach this far south into the United States for the change that happened on the Hudson River since it was originally formed.The topography of the Hudson Valley enabled the ice from the Pleistocene Glaciation to form a Lobate Ice margin26 about 50 miles north what is now Manhattan long island. Around 22,000 years ago the Ice over the Catskills and Taconic uplands thinned, while it thickened in the Hudson Valley and expanded southward closer to the mouth of the Hudson. Scientists today doing Pollen analysis and radiocarbon dating have found that the c limate back then right before, and as the last Ice age started was much warmer than today. As one can expect, warmer conditions meant more plants, and the sea level was much higher than today27.When the climate cooled and the Glaciers expanded south all these trees, plants and debris were ground down and immense pressure pushed them into the ground, almost dissolving them into dirt. This not 26 Lobate means resembling of a lobe. In this context it is used to describe the shape of the edge of the Glacier, or its maximum extent which was a short of lobe shape. 27 Evidence shows that the waters might have been as far north Albany. 14 | P a g e only made the area much more barren, but also flattened the Adirondacks, and Hudson Highlands down many thousands of feet.The glacier continued to expand 26,000 years ago and merged with smaller glaciers up north to form one big glacier known as the â€Å"Laurentide Glacier†28. This Glacier covered all of Ontario, the St. Lawrence River, M anitoba, Nunavut, and parts of Quebec, as well as the Great lakes down to Chicago where it almost ran parallel to the US/Canada border before dipping slightly down towards present day Manhattan and following the coast of the US up north. At the height of this glaciers advance the ice most likely was more than 1,000 feet thick over the tops of the Appalachians (if you do the math this means that it was over 1. miles deep) meaning immense pressure was being placed on everything flattening the landscape. This also meant that because there was so much pressure, and the water of the Hudson never froze 100%29 the Hudson’s waters literally pushed the earth and carved the floor of the Hudson to a depth similar that of what it was before it broke its barrier at the Narrows. 30 The dirt being compressed turned back into soft metamorphic rock, and created marble where none existed near Warrensburg.A few miles south at Glens Falls the Ice naturally deepened because of the drop in elevati on and gained momentum31 carving out the fjord previously made even bigger, which created Storm King, Beacon and Bear Mountain. All this rock carved out of the Fjord eventually made its way south where it was dumped over Manhattan and Long Island, somewhat accounting for all the Limestone and shale and schist around that area. At this time, the Hudson Canyon was also carved out by the glacial ice melt flowing through it with rocks and debris and became much deeper and wider.When the Laurentide glacier made it to the Narrows its front stopped moving forward, but its back kept on moving forward compressing everything together (Like an accordion) and melting a lot of the ice. Why this happened is not really known by Scientists because glaciers can float. This area became the Glaciers â€Å"dumpster† and the Terminal Moraine was officially formed. Long Island was 28 29 Yes, it was named after Laurentia, ancient North America. Meaning the whole time there was a glacier over this a rea, the Hudson was still flowing but now mostly with ice melt from the glacier itself. 0 Of course this all filled back in as the glacier melted. 31 A glacier is always moving, whether it is 1 foot a year or 1 inch a year. 15 | P a g e built up and out to its current state and the Moraine extended west into New Jersey and Pennsylvania, carrying with it glacial melt creating many of the glacial lakes in that area such as Lake Hackensack, Glacial Lake Hudson and many others. Clay also being carried was dumped all over the region (mostly on the current Rockland County side) and created a nice thick, slippery layer on which the glacier to slide on.This process of dumping and melting continued for many thousand years and started the recession of Laurentide. In a 2,000 year period from 26,000 years ago to 24,000 years ago Laurentide melted and receded so that all of Long Island, Staten Island, New Jersey, Pennsylvania and pretty much everything south of present day Hartford Connecticut w as ice free. The Ice continued to melt over the next 4,000 years until everything south of Glens Falls was free of ice. The ground, sort of like a sponge when you fill it with water, rose a few meters and went nearly back to its state before the glacier.At Glens falls The glacier stopped for a thousand or so years and slowly melted providing the Hudson valley with a constant stream of fresh glacial water. Around 19,000 years ago the glacier started to recede from Glens Falls and the melt water created Glacial Lake Albany which continued to grow throughout the next several thousand years as Laurentide receded. At 15,500 years the Climate suddenly got cold and the glacier advanced back south to near Poughkeepsie and created the Wallkill, Poughkeepsie, Red hook, Hyde Park ad Pine Plains moraine.As suddenly as the Climate got cold, it got warm again and by 13,000 years the glacier was receded north of present day Quebec City. When the climate got warmer again the sea levels rose, this t ime to near Albany, and caused Glacial Lake Albany to drain. For the next couple thousand years as the climate cooled, the Hudson was tidal up to Poughkeepsie and as the Sea retreated. This brought the tides down with it to near Peekskill where it stayed for many thousands of years until around 6,000 years ago it began to go north to nearly 20 miles past Troy32 by 2,000 years ago the sea was at its present place, and the Hudson was in its present 2 The exception to this is the Troy Dam; if it wasn’t built the Hudson would still be tidal nearly 20 miles north of it. 16 | P a g e state. Long Island was as it is now, and the coast was pretty much the same besides what natural erosion as taken away since then. This was the final Glaciation, and the final change to the Hudson River. After nearly 1. 2 billion years, several different Oregany’s, Hundreds of changes, 4 different climate changes and a whole lot of pushing and pulling and moving the Hudson River was finished bei ng formed and all it needed was for Henry Hudson to come sailing to name it†¦. ConclusionIf you have gotten this far along into this history story then you will know that the Hudson River didn’t just appear, it doesn’t formally end at the Narrows between Brooklyn and Staten island and it isn’t just a river. It is the culmination of 1. 2 billion years (and counting) of the earth doing its shtick33 on the world we live on. It took 7 different continents to pull this off, and it worked out beautifully creating a river of outmost importance to our lives, lives before us, and lives to come. I like most of you out there reading this paper did not know a thing about the Geology of the Hudson River when I started this project.It probably took me a proportionate amount of time to learn this as it did to create the whole Hudson. Now, after early 3 months of reading words I don’t know, looking at diagrams I can’t even understand and writing technical ter ms that I can’t pronounce I have learned what it took, and takes to create the Hudson. Like they say, it takes a village to raise a child; it took a whole world and 1. 2 billion years to create this river, a river of small nature compared to others around us such as the Nile, or Amazon which are nearly 5 times the length of the Hudson and took a very disproportionate amount of time to create. 3 â€Å"Piece†, or â€Å"thing† in Yiddish 17 | P a g e So, as I leave you with this 20 page Essay, think about the next time you go to the Hudson and pick up a handful of sand, and know, just know that that handful of sand has been moved around for 1. 2 billion years to end up at your feet. Bibliography L. Sirkin & H. Bokuniewics (2006) – The Hudson River Valley: Geological History, Landforms and Resources Wikipedia (http://en. wikipedia. org/w/index. php? title=Hudson_Canyon&oldid=453958227) – Hudson Canyon Data SIO, NOAA, U. S.Navy NGA, GEBCO (2010)  œ Google Earthâ„ ¢ United States Geological Survey (USGS) (2004) – Sea Floor Topography & Backscatter Intensity of the Hudson Canyon Region Offshore of New York & New Jersey (http://pubs. usgs. gov/of/2004/1441/html/interp. html) Phil Stoffer & Paula Messina (2008) – Introduction to the Geologic History of the New York Bight (http://www. geo. hunter. cuny. edu/bight/Geology. html) Phil Stoffer & Paula Messina (2008) – The Highlands Region (http://www. geo. hunter. cuny. edu/bight/highland. html) R. G.Wilkins Booth (1970) – The Ontario Water resources commission Geology of the upper part of the Severn River basin and the Severn River basin lying within the Hudson River Lowlands. Steven H. Sehimmrich – Geology of the Hudson Highlands Region (www. environmentalconsortium. org) Access Genealogy – Geology of the Hudson (http://www. accessgenealogy. com/newyork/hudson/geology_hudson. html) Charles Merguerian (2010) – Geology 133 Field Tr ip 18 | P a g e Dick Goodman (2013) – Geologist in California, gave much information and advice on this project United States Navy Geological Services (2013) – Maps, Graphs Bradford B.Van Diver (1985) – Roadside Geology of New York John F. Shupe (1996) – National Geographic Atlas of the World Revised sixth edition Kevin Hile (2009) – The Big Book of Answers Tom Lewis (2005) – The Hudson: A History Maps 19 | P a g e The maps presented here on the next couple of pages are all ones used in this essay as reference. They are from many different sources and show many of the things I talked about, visually. Hudson Canyon 20 | P a g e 21 | P a g e 22 | P a g e Geographical Diagrams 23 | P a g e 24 | P a g e 25 | P a g e