Questions On Natural Knowledge Of God - 1679 Words

2. Natural Knowledge of God in Insight Lonergan’s argument, I will offer my assessment of whether or not the constitution permits his philosophical means. Lonergan moves from treating God as an object of thought to treating God as an object of affirmation by way of an argument: â€Å"If the real is completely intelligible, God exists. But the real is com ¬pletely intelligible. Therefore, God exists.† I will refrain from elaborating on the argument itself; works doing this are available. What is important, given the interests of this study, is the following statement by Lonergan in the Epilogue: [O]ur first eighteen chapters were written solely in the light of human intelligence and reasonableness and without any presupposition of God’s†¦show more content†¦The question arises, however, as to what Lonergan’s assessment would be of arguments that proceed more—or at least more explicitly—on the side of the object. One wonders, for instance, how Lonergan would see his argument in relation to Aquinas’s five ways. As it happens, Lonergan makes two illuminating statements about the five ways in chapter nineteen of Insight. First, he writes, â€Å"[T]he five ways in which Aquinas proves the existence of God are so many particular cases of the general statement that the proportionate universe is incompletely intelligible and that complete intelligibili ¬ty is demanded.† Second, he writes, â€Å"[B]esides Aquinas’s five ways, there are as many other proofs of the existence of God as there are aspects of incomplete intelligibility in the universe of proportionate being.† These two statements illuminate what is central to Lonergan’s argument: the incapacity of proportionate being as such to satiate the mind’s demand for complete intelligibility. Alicia Jaramillo contends that Lonergan’s focus on this demand—something on the side of the subject—does not mark an abandonment of classical cosmological arguments. I now return to the question of whether

Coca Cola Supply Chain Management - 1425 Words

1.0 Introduction: How can we explain how important supply chain management is in the business industry? Many business go through the process of supply chain such as Public v Private Primary, Secondary, Tertiary sectors, Financial, Retailing, Manufacturing, Wholesale trades, Construction, Mining Quarrying/Farming, Services and Transport. Our lives moves and grows through supply chain management its part of a system in receiving our products, everyday goods, Raw materials, Packaging materials, Semi - finished goods, Finished goods , Machines spares, Services and Office Equipment. It can be defined as a process of arranging, preparing, applying and taking efficient control, by storing goods or services and taking information from the†¦show more content†¦JIT is used in repetitive manufacturing which means that products are manufactured repeatedly. JIT’s advantage in this case that it can reduce lead time as it can link manufacturing centers and create a balance between them so that th e process can be in order. http://personal.ashland.edu/~rjacobs/m503jit.html 4. Right Quantity: After ordering the supplies the next step will be defining the right quantity and quality. Miscalculation in approximating these statistics may affect the company in over- or under-supply. This would define the increase in holding costs. It is vital to define the right number, size weight of the product in order to identify the right quantity for us to meet the demand. This information is required in every stockroom and storage room, it can also help us define the type of transportation required. For coca cola who are sponsoring the Olympic 2012 it is crucial for them to provide the right amount of quantity of their products during this time. It cannot be too much or too little. Quantities can increase price requirements. 5. Right Quality: What is Quality? â€Å"Quality is whatever the customer says it is† - (Baily) It is what the customer will define the quality of the product or service. it is what any business is supposed to be aware of cause in the end it is all about what the customer requires and what they will purchase. Quality isn’t just about quality of the product it counts as quality of the appearance of theShow MoreRelatedCoca Cola And Inventory Forecasting1112 Words   |  5 Pages COCA COLA AND INVENTORY FORECASTING Name Submission Date Course Name Institutional Affiliation Introduction Coca-Cola is a multi-national corporation that has its headquartered in Georgia, Atlanta. The company involves itself in the business of beverage production. Subsidiary plants are located all over the world i.e. Asia, Africa, Europe, Australia and South America. Since the company has many branches and deals with a whole lot of inventory, there is a need to act proactively andRead MoreCoca-Cola Supply Chain1724 Words   |  7 PagesCoca-Cola is the world’s largest beverage company. They employee over 146,000 employees offer over 3,000 products worldwide and operate in over 200 countries. The company was founded in 1886 but it wasn’t until 1891 when an Atlanta business man secured the rights to the company that the vision of Coca-Cola was established and their expansion begun. In 1899 Coca-Cola’s first bottler relationship was established. This bottling relationship allowed the company to grow aggressively and expand intoRead MoreCoca Cola Supply Chain Analysi s751 Words   |  4 Pages The Coca-Cola Company Supply Chain Student’s Name Institution Affiliation The Coca-Cola Company Supply Chain Introduction The Coca-Cola company is an American multinational beverage company headquartered in Atlanta, Georgia. 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From here, he noticedRead Moreâ€Å"Coca-Cola Is Everything†1204 Words   |  5 Pagesâ€Å"Coca-Cola Is Everything† March 2013 Abstract This paper will provide the answers to questions asked in week two assignment. The paper will explore concepts such as supply chain management, switching cost, and business intelligence and apply them to Coca-Cola’s internal collaboration efforts. Sources in the paper have cited the use of social media tools through Facebook and loyalty programs. Warden (2013) has called Coca-Cola king of social of media. This paper will compare Coca-Cola’s socialRead MoreCase Study : Coca Cola Company Essay829 Words   |  4 PagesCoca-Cola is Everything: SCM, CRM, ERP, Social Media, You Name it Dr. John Stith Pemberton never thought that the development of a new idea, the syrup to create a fountain soda, would become a worldwide company. Dr. Pemberton decided to name the syrup Coca-Cola and then went to sell it to Jacob’s Pharmacy, they teamed the syrup with a carbonated water and â€Å"voila† they started selling a soda fountain drink. Dr. Pemberton sold a portion of the business and later on, Mr. Asa Candler acquires the totalRead MoreThe Development And Integration Of People And Other Resources Like Technological Are Vital For Successful Supply Chain Integration1681 Words   |  7 Pages â€Å"The development and integration of people and other resources like technological are crucial to successful supply chain integration.† The flow of Things into an organization is basically carried out in an order provide to a supplier. It means that a purchasing department looks appropriate suppliers, discusses terms and conditions, organizes deliveries, arranges insurance and payment and everything needed to get material into an organization. Inward transport is contributed towards the movementRead MoreStrategy Levels Companies Approach Essay1165 Words   |  5 Pagesclassify levels of strategy in view corporate-level strategy as responsible for market definition, business-level strategy is responsible for market navigation, and functional-level strategy as the foundation that supplies both of these† (Advameg, Strategy Levels, 2011). Wal-Mart, Coca-Cola, and Sarnoff are companies that use different approach to business such as low cost approach, differentiation, and best value. Corporate-level strategies address the entire enterprise withRead MoreCoca Col A Unique Supply Chain System1179 Words   |  5 Pagesbeverage brand on the world, Coca-Cola has a unique supply chain system. In fact, formula Coca-Cola is held tightly trade secret and cannot know exact ingredients as well as the cost of their supplies. However, some ingredients are known as important components which are used in the manufacturing of syrup such as sugar, Carbonated water, sucrose, high-fructose corn syrup, caffeine, phosphoric acid v. Caramel (E150d) and Natural flavourings. In downstream activities, Coca-Cola uses the franchised distributionRead MoreManagement Style Of Coca Cola Essay1510 Words   |  7 Pagesselected company s management style from the company s inception to the current day. Indicate whether or not you believe the company is properly managed. Provide support for your position. Management style is a complete process of leadership used by managers within Coca Cola. The success of the management team has inspired its employees to meet their objectives. There are three main management styles that Coca Cola use, democratic, autocratic and the laissez-faire style. (Coca Cola 2010) The democratic

Hudson River a Detailed and Comprehensive Geological History Free Essays

string(88) " than a centimeter in the last couple thousand years and shows no signs of speeding up\." 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‚¬ ¦. We will write a custom essay sample on Hudson River: a Detailed and Comprehensive Geological History or any similar topic only for you Order Now . 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¢ € ¦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 Lake 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 from 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 emerges 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 fo rmed 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 spike 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. You read "Hudson River: a Detailed and Comprehensive Geological History" in category "Papers" 4|Page Hudson River Formation The 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 what 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 periodically moved, basal tic 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 Proterozoic 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. 9 Coarse, 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 Cambrian 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 several 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 interval 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 Hudson 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 amount. Almost at the same time as all this uplifting was happening, a 18 19 Think 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 its 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 few 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 23 This is an extremely short time in geologic history and greatly shows how much the pressure was on the landmass 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 creating 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 dee p. 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 the HRV. 25 The 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 climate 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, Manitoba, 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 th e 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 elevation 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 area, 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. C lay 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 was 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 time 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 ne arly 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 being formed and all it needed was for Henry Hudson to come sailing to name it†¦. Conclusion If 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 terms 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_Canyonoldid=453958227) – Hudson Canyon Data SIO, NOAA, U. S. Navy NGA, GEBCO (2010) – 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 Trip 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 How to cite Hudson River: a Detailed and Comprehensive Geological History, Papers

An Effective Parenting Style Essay Example For Students

An Effective Parenting Style Essay Parents have a major role in their children lives because of how they decided to raise their children. Parents tell their children what is right and what is wrong. According to the Wikipedia, â€Å"Parenting style is a psychological construct representing standard strategies that parents use in their child rearing.† As parents use the technique to raise their children, they also shaped their value and personality. â€Å"Parenting style considers the balance between two aspects of parenting, namely, control, and warmth† (Ginsburg, Durbin, Garcias-Espana, Kalicka, and Winston, p. 1041). The most commonly heard parenting styles are authoritative, authoritarian, permissive, and uninvolved. Authoritative parenting is the one with most control and provide the least amount of support whereas authoritarian parenting also has most control, but with more support. Permissive parenting parents give their children all the supports that are needed and not much of the control. Uninvolved parents are basically similar to carless parents; they give nearly no support and no control to their children. Which style of parenting did your parent(s) use on you? In 2009, the American Academy Pediatrics published a journal along with a research case, Associations Between Parenting Styles and Teen Driving, Safety-Related Behaviors and Attitude. The study was claiming to be how parenting related to the behavior of driving. By the end of the study, it was suggested by professionals that parents should set limits for their children freedom (Ginsburg, Durbin, Garcias-Espana, Kalicka, and Winston, p. 1042-1043). The case study had proven that young adults who were raised by high controlling and least supportive parent(s) had a significant number of differences. ., et al. Parenting and Obsessive Compulsive Symptoms: Implications of Authoritarian Parenting. Journal of Cognitive Psychotherapy 24.3 (2010): 151-164. Academic Search Premier. EBSCO. Web. 28 Aug. 2011. Li, Yan, Philip R. Costanzo, and Martha Putallaz. Maternal Socialization Goals, Parenting Styles, and Social-Emotional Adjustment Among Chinese and European American Young Adults: Testing a Mediation Model. Journal of Genetic Psychology171. 4 (2010): 330-362. Academic Search Premier. EBSCO. Web. 28 Aug. 2011. Partridge, Brian C. Adolescent Psychological Development, Parenting Styles, and Pediatric Decision Making. Journal of Medicine Philosophy 35.5 (2010): 518-525.Academic Search Premier. EBSCO. Web. 9 Sept. 2011. Wikipedia contributors. Parenting styles. Wikipedia, The Free Encyclopedia. Wikipedia, The Free Encyclopedia, 10 Aug. 2011. Web. 14 Sep. 2011.

The Ironies of Social Standards in Sister Carrie Essay Example For Students

The Ironies of Social Standards in Sister Carrie Essay To this day, Sister Carrie remains one of the most controversial novels of its time. The remarkably realistic characters and contentious situations created by Theodore Dreiser illustrate the double standards within a growing American society at the turn of the twentieth century. Naturalism plays a large part in the development of each character and their pathetic inability to evade their trivial fates Theodore. The perverse fascination and distaste surrounding this incapability mirrors a societys hypocrisy of its own social standards. For his first novel, Dreiser opted to paint a realistic portrait of America for what it really was- materialistic Gerber 52. The money ideal would be exposed as the great motivating purpose of life in the United States: ones relative affluence at any level of society determining the degree creature comfort one might enjoy, the measure of prestige one might own, and the extent of social power one might command Gerber 52-53. Sister Carrie completely reiterates Americas obsession with money because there is not one character whose own status symbol isnt determined economically Gerber 53. We will write a custom essay on The Ironies of Social Standards in Sister Carrie specifically for you for only $16.38 $13.9/page Order now At the end of the Civil War, big business boomed and there was now a preoccupation with conspicuous consumption Ward. Capitalism roared and consumers began to see each other for what they thought they really were: money. Dreiser first describes his Caroline Meeber not by her opinions or actions, but by what she owns: a small trunk, a cheap imitation alligator-skin satchel, and a small yellow snap purse Dreiser Sister 3. Although Carrie cannot afford a real alligator-skin satchel, she owns an imitation so that she appears to be something she is not Ward. False appearances are a reiterated theme throughout Sister Carrie. Schafer 2 Upon entering Chicago and meeting Drouet, the reader becomes attentive to Carries fascination with the upper class. In addition to representing consumerism, Carrie also serves as a symbol of the American middle class. Carrie is `ambitious to gain material things Ward. Entering a department store to find a job, Carrie leaves with an unsatisfied desire to own things that she cannot. Carrie sees how much the city has to offer her. She longs for the luxury and wealth of the other shop dwellers Balling 23. All of the fancy items tempt Carrie although she cannot manage to pay for any of them; thus a capitalist economy manipulates the desire of the consumer without ever completely satisfying it Ward. This unfulfilled yearning compels the consumer to work long hours just to struggle to buy more items Ward. With each purchase, the need for material things grows while never completely satisfying the consumer. Carries dream of satisfaction is hastily broken when she realizes she must work in an unpleasant job to get what she wants. In Sister Carrie, money is a main objective at the beginning of many relationships. Carries fascination in Drouet is instigated by his money. Handing her the money gives him the opportunity to touch her hand, the first step of physical intimacy with her Ward.  In a society in which wealth is associated with individual merit, Drouet begins to stir up yet another person into materialism. Through this, he can conduct his life on a splendid basis because Carrie looks to him with desire Balling 25. A world of possibilities is opened to Carrie through Drouet. She has now become an insider to the world of prosperity, excitement, and satisfaction Balling 29. Schafer 3 In meeting Hurstwood, Carrie can only look further upward. He is the symbol of the enlightened, capitalist man Ward. His life with Julia is one greater than Drouets. Unlike Hurstwood, Drouet is awkward and imitative in his dress and actions. This flashy lifestyle screams that he is performing a role Ward. Hurstwood spends just as noticeably, but he does it with a great deal of taste. Overall, while Hurstwood looks like the legitimate article, Drouet just comes off as a fake Ward. Carrie soon takes notice. Although they live a far more affluent lifestyle than Drouet and Carrie, Hurstwoods family is not satisfied. As Carrie craves nice clothing and trinkets, Julia and Jessica are saddened that they cannot afford a European summer vacation Ward. Again, the reader is introduced to the reoccurring theme of the compelling influence behind consumer society: unfulfilled desire Ward. .u63ce4743558b3809bb8eb5d72cf2326f , .u63ce4743558b3809bb8eb5d72cf2326f .postImageUrl , .u63ce4743558b3809bb8eb5d72cf2326f .centered-text-area { min-height: 80px; position: relative; } .u63ce4743558b3809bb8eb5d72cf2326f , .u63ce4743558b3809bb8eb5d72cf2326f:hover , .u63ce4743558b3809bb8eb5d72cf2326f:visited , .u63ce4743558b3809bb8eb5d72cf2326f:active { border:0!important; } .u63ce4743558b3809bb8eb5d72cf2326f .clearfix:after { content: ""; display: table; clear: both; } .u63ce4743558b3809bb8eb5d72cf2326f { display: block; transition: background-color 250ms; webkit-transition: background-color 250ms; width: 100%; opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #95A5A6; } .u63ce4743558b3809bb8eb5d72cf2326f:active , .u63ce4743558b3809bb8eb5d72cf2326f:hover { opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #2C3E50; } .u63ce4743558b3809bb8eb5d72cf2326f .centered-text-area { width: 100%; position: relative ; } .u63ce4743558b3809bb8eb5d72cf2326f .ctaText { border-bottom: 0 solid #fff; color: #2980B9; font-size: 16px; font-weight: bold; margin: 0; padding: 0; text-decoration: underline; } .u63ce4743558b3809bb8eb5d72cf2326f .postTitle { color: #FFFFFF; font-size: 16px; font-weight: 600; margin: 0; padding: 0; width: 100%; } .u63ce4743558b3809bb8eb5d72cf2326f .ctaButton { background-color: #7F8C8D!important; color: #2980B9; border: none; border-radius: 3px; box-shadow: none; font-size: 14px; font-weight: bold; line-height: 26px; moz-border-radius: 3px; text-align: center; text-decoration: none; text-shadow: none; width: 80px; min-height: 80px; background: url(https://artscolumbia.org/wp-content/plugins/intelly-related-posts/assets/images/simple-arrow.png)no-repeat; position: absolute; right: 0; top: 0; } .u63ce4743558b3809bb8eb5d72cf2326f:hover .ctaButton { background-color: #34495E!important; } .u63ce4743558b3809bb8eb5d72cf2326f .centered-text { display: table; height: 80px; padding-left : 18px; top: 0; } .u63ce4743558b3809bb8eb5d72cf2326f .u63ce4743558b3809bb8eb5d72cf2326f-content { display: table-cell; margin: 0; padding: 0; padding-right: 108px; position: relative; vertical-align: middle; width: 100%; } .u63ce4743558b3809bb8eb5d72cf2326f:after { content: ""; display: block; clear: both; } READ: Charles Dickens greatest novel EssayAfter Hurstwood and Carries affair and escape to New York, Hurstwood soon finds himself having to think carefully about small disbursements like rent and cab fare. Although he has sufficient money to invest in new businesses, he turns down many prospects because they are too low-class for him Ward. Not only is his money very important to him now, but so is his respectability. Having to live so frugally as he searches for a job humiliates him Balling 61. The importance of Hurstwoods reputation to himself underscores the materialism in America. Being who you are to yourself is not as important as being someone to others Gerber 60-61. Once Carrie meets Mrs. Vance, she reenters the world of conspicuous consumption Ward. As soon as she finds someone wealthier than she, Carrie again becomes displeased with her life. It seems as if Carrie then sets new goals for herself as she is exposed to new socio-economic levels Ward. Hurstwoods decline pushes Carrie further away from him. Mrs. Vances decision to cut off her connection with Carrie because of Hurstwoods appearance exposes the dehumanizing nature of consumer society Ward. While Hurstwood gradually sinks toward deprivation and suicide, Carrie once again moves foreword and appears on stage Thorp 472. Carries constant drag to something better was not to be denied Thorp 472. Her choice to leave him is almost completely motivated by finances, as was her decision to marry him Ward. The richer Carrie gets, again, the farther up she looks. Despite hardly knowing what to do with all of her money, however, she still suffers from unsatisfied desires Ward. Carries newfound theatrical success does not bring her happiness as she expected, just more urges. Although she has  now gained an identity that is independent of Hurstwoods and Drouets desire for her, she is still dependent on the desire of the public Ward. Even after Carrie has come so far, she still looks towards others opinions of her to make her happy. By the end of the novel, Carrie is still dissatisfied. She still experiences the unceasing discontent that is the major force behind consumerism Ward. A consumer-based society can only survive if there is always something more to want. With eyes so fixed on mountaintops yet to be attained, they never stop to wonder this way madness lies Gerber 53. As Carrie reaches the top, she and the reader no longer know what she desires. The brutal forces governing life dictate that any achievement permitted a human creature be diluted by dissatisfaction Gerber 56. At this time in America life had much to do with `chemisms and `magnetisms; it was dominated by invincible material forces; and of these the drives for power, money, and sex were primary Gerber. Sex and the relationships between men and women were solely based on finances, just as were Carries relationships with Drouet and Hurstwood. Even Dreiser himself expects Carrie to do nothing more than rely on a man. When a girl leaves her home at eighteen, she does one of two things. Either she falls into saving hands and becomes better, or she rapidly assumes the cosmopolitan standard of virtue and becomes worse Dreiser Sister 3. This statement also implies that Carrie or women in general uses seduction to get what she wants Thorp 472. Dreiser makes of her a symbolic figure who must sacrifice a certain amount of innocence in order to make progress of any kind. Thus Carries dream is the American Dream as well; it is a dream of rich finery, financial success and power Balling 30. When Drouet offers Carrie the twenty dollars, he is essentially buying the prospect for sex Ward. Because she owes him money, she feels tied to return his kindness with the only material object she owns- her body. Exposed of all its trimmings, Drouet and Carries relationship is no more than a form of prostitution. Because Carrie is paid more for her body than she is for her employment, she realizes that a womans most marketable product is sex Ward. .uc5b11c29873868d88a1fcefa2093902e , .uc5b11c29873868d88a1fcefa2093902e .postImageUrl , .uc5b11c29873868d88a1fcefa2093902e .centered-text-area { min-height: 80px; position: relative; } .uc5b11c29873868d88a1fcefa2093902e , .uc5b11c29873868d88a1fcefa2093902e:hover , .uc5b11c29873868d88a1fcefa2093902e:visited , .uc5b11c29873868d88a1fcefa2093902e:active { border:0!important; } .uc5b11c29873868d88a1fcefa2093902e .clearfix:after { content: ""; display: table; clear: both; } .uc5b11c29873868d88a1fcefa2093902e { display: block; transition: background-color 250ms; webkit-transition: background-color 250ms; width: 100%; opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #95A5A6; } .uc5b11c29873868d88a1fcefa2093902e:active , .uc5b11c29873868d88a1fcefa2093902e:hover { opacity: 1; transition: opacity 250ms; webkit-transition: opacity 250ms; background-color: #2C3E50; } .uc5b11c29873868d88a1fcefa2093902e .centered-text-area { width: 100%; position: relative ; } .uc5b11c29873868d88a1fcefa2093902e .ctaText { border-bottom: 0 solid #fff; color: #2980B9; font-size: 16px; font-weight: bold; margin: 0; padding: 0; text-decoration: underline; } .uc5b11c29873868d88a1fcefa2093902e .postTitle { color: #FFFFFF; font-size: 16px; font-weight: 600; margin: 0; padding: 0; width: 100%; } .uc5b11c29873868d88a1fcefa2093902e .ctaButton { background-color: #7F8C8D!important; color: #2980B9; border: none; border-radius: 3px; box-shadow: none; font-size: 14px; font-weight: bold; line-height: 26px; moz-border-radius: 3px; text-align: center; text-decoration: none; text-shadow: none; width: 80px; min-height: 80px; background: url(https://artscolumbia.org/wp-content/plugins/intelly-related-posts/assets/images/simple-arrow.png)no-repeat; position: absolute; right: 0; top: 0; } .uc5b11c29873868d88a1fcefa2093902e:hover .ctaButton { background-color: #34495E!important; } .uc5b11c29873868d88a1fcefa2093902e .centered-text { display: table; height: 80px; padding-left : 18px; top: 0; } .uc5b11c29873868d88a1fcefa2093902e .uc5b11c29873868d88a1fcefa2093902e-content { display: table-cell; margin: 0; padding: 0; padding-right: 108px; position: relative; vertical-align: middle; width: 100%; } .uc5b11c29873868d88a1fcefa2093902e:after { content: ""; display: block; clear: both; } READ: AP by John Updike EssayWhile Carrie illustrates the life of a modern single woman, Julia demonstrates the typical, unhappy married women. Hurstwood attributes his wife as an ornament of his success by regarding her as one of his possessions Ward. Again the marriage serves as a contract to declare her job as a wife: to give Hurstwood sex in exchange for his money Ward. The pragmatic morality and hypocrisy of a males role in a marriage is apparent through Hurstwoods actions. While he keeps a close eye on Julia and all of her interactions, he does not condemn mens extramarital affairs; he only approves if they are carried out discreetly Ward. This disjunction between peoples  conduct and the figure they stage is maintained by a web of lies Ward. Paying close attention to Drouet as he compliments other women, Carrie takes note and tries to develop her identity largely based on what he craves. Through this imitation, she becomes simply a manifestation of masculine desire; Carrie substantiates the conventional idea that women are nothing more than role players Ward. Sister Carrie presents womens identity as virtually non-existent: men can be genuine, but women can only try to imitate Ward. Carrie, again, knows no identity without conceding to a man Markels 533. As a reflection of masculine desire, Carrie cannot express any desires of her own- except for her need for conspicuous consumption. Rather than feeling happiness from her own desires, Carrie is pleased only when others desire her Ward. Carries need for attention again upholds the conventional standard that a woman only has social standing when a man desires her Phillips 553. Dreisers approach of retelling life how it really has created a great deal of unexpected controversy. The sum and substance of literary as well as social morality may be expressed in three words- tell the truth Dreiser True 473. This statement made by Dreiser himself was in response to critics against the publication of Sister Carrie. The depiction of a fallen woman in a success story was considered completely immoral Riggio. As Dreiser entered the literary scene in the early 1900s, a conventional style of writing had already been set into tradition. The function of literature was to appeal to mans `higher nature, to inspire him through the depiction of mans capacity to achieve the ethical life to seek such a life for himself Pizer Dreisers. Basically, the didactic method of literature was there to create an ideal society. When Sister Carrie came along, most reviewers held upon the fundamental circumstances of the novel- a young woman has two forbidden sexual affairs without experiencing either material loss or moral degeneration Pizer Dreisers. Also, since God was not mentioned once in the novel, Sister Carrie was considered immediate grounds for dismissal Pizer Dreisers. Such debate surrounding a novel can really only prove one point: it is a story of real life, of their lives Notman 474. All of these situations- materialism, seduction, adultery, bigamy, and theft- were actually occurring in real life Thorp 469. This denial of Americans own lives further reiterates the hypocrisy in a growing capitalist society. In a brief essay entitled True Art Speaks Plainly, Dreiser concluded a true picture of life, honestly and reverentially set down, is both moral and artistic whether it offends the conventions or not Dreiser True 474. Dreisers Sister Carrie deals with the sordid side of everyday life. Although his characters are mixtures of moral and corrupt, unable to assert their will against natural and economic forces, he rarely passes judgment on them Theodore. These extraordinarily convincing individuals and the litigious circumstances created by Theodore Dreiser demonstrate the ironies within an  emergent American culture after the Civil War. Materialism and capitalism in a booming economy, conventional standards of men and womens roles, and the denial of the American public in response to the novel all prove that Sister Carrie was ahead of its time in portraying the authentic and pessimistic view of real existence.

Serian Synogoges essays

Serian Synogoges essays Architecture plays a very important role in a culture, and from its remains, historians can gain a wealth of information. It determines the wealth of the community, the weather conditions and many other things. Not only can historians learn what it was like in that area at that time, but also they can learn from it to improve our area now. For example, the Romans built curved roads and sewers to prevent flooding and currently we also build our roads similarly. Another example can be the columns the Greeks used to build; now the White house and many other buildings are built in a Greek style. In fact, the entire Washington D.C. is built just like Paris; it is built in a circle around the White House, as Paris is built around the Eiffel Tower. Architecture and the arts have such power over people that Jews are thought to have horns because of a misinterpretation by Leonardo Divenchi, who portrayed Moses with horns. Now well take a look at architecture from a religious point of view. During the late Fifteenth century, refugees from Spain escaped to Muslim countries, mainly the Ottoman Empire. With them they brought the Sephardic traditions and culture and it quickly spread throughout the Mediterranean region. The Sephardic tradition eventually dominated the Syrian synagogue design and its architecture. Today, this beautiful architecture still remains in the Syrian community in Brooklyn. During the Ottoman period, the basilica form was popular. The Syrian synagogue usually had a wide central aisle and two side aisles. Arcades supported by columns separate it. Different parts of the room would be elevated, especially the tevah for illumination purposes. Many of the synagogues of Syria were very decorative; even the mandatory utensils of the synagogue, such as the lightbox, which was used to give off light to read the torah, would be very fancy. ...

Brave New World Diction Essay

† In chapter 3 of Aldous Huxley’s novel Brave New World, many things are revealed about hot the society in this novel functions. It shows more about the work that the people do and how the society functions. Huxley uses repetition and descriptive diction to provide a deeper look into the society that is shown in this passage. In one paragraph, one specific word helps to clarify the meaning of the repetition of the word â€Å"whisk†. While talking about history, the Controller states that â€Å"History is bunk† to the students. In context, bunk is taken to mean nonsense, or unimportant. It serves the authors purpose by revealing more about the society in this passage. History is irrelevant to the alphas. The word â€Å"bunk† further helps to explain the diction in the next paragraph of this passage. The word â€Å"whisk† is repeated twelve times in one paragraph. It is used to describe how easily history is wiped away and forgotten. It even shows that music and feelings such as passion are gone. The repetition of the word â€Å"whisk† is fundamental in illustrating how insignificant the past is to this society. The authors use of descriptive diction gives further insight about this society. The author uses words and phrases such as â€Å"tactual†, â€Å"Embryo Store†, and â€Å"Psychology Bureau† among many others. This is significant because it illustrates how technologically advanced the society in this passage is. This passage reveals that society has completely disregarded history and advanced in the scientific field. The author uses the word â€Å"forbidden† to describe poetry books and religious books such as the Bible. This further develops the society as a society where feelings evoked by poetry and religious faith are frowned upon. As this passage demonstrates, history and literature have been removed from this society. History and literature are subjects that connect people, and tie them together, but without them, this passage shows that this society is very advanced in the field of science. This society is clearly appalled by life led by their ancestors. They have effectively gotten rid of history, and any feeling that helps them make lasting connections to other people. Through the use of descriptive diction, the authors purpose of providing insight into this society is fully accomplished. The diction in this passage illustrates how dynamic the society in this novel is. This society revolves around science, and wants nothing to do with the past. This passage provides very important insight into how this society functions, and the structure of the society. The author successfully achieves his purpose through the use of repetition and expressive diction. Brave New World Diction Essay † In chapter 3 of Aldous Huxley’s novel Brave New World, many things are revealed about hot the society in this novel functions. It shows more about the work that the people do and how the society functions. Huxley uses repetition and descriptive diction to provide a deeper look into the society that is shown in this passage. In one paragraph, one specific word helps to clarify the meaning of the repetition of the word â€Å"whisk†. While talking about history, the Controller states that â€Å"History is bunk† to the students. In context, bunk is taken to mean nonsense, or unimportant. It serves the authors purpose by revealing more about the society in this passage. History is irrelevant to the alphas. The word â€Å"bunk† further helps to explain the diction in the next paragraph of this passage. The word â€Å"whisk† is repeated twelve times in one paragraph. It is used to describe how easily history is wiped away and forgotten. It even shows that music and feelings such as passion are gone. The repetition of the word â€Å"whisk† is fundamental in illustrating how insignificant the past is to this society. The authors use of descriptive diction gives further insight about this society. The author uses words and phrases such as â€Å"tactual†, â€Å"Embryo Store†, and â€Å"Psychology Bureau† among many others. This is significant because it illustrates how technologically advanced the society in this passage is. This passage reveals that society has completely disregarded history and advanced in the scientific field. The author uses the word â€Å"forbidden† to describe poetry books and religious books such as the Bible. This further develops the society as a society where feelings evoked by poetry and religious faith are frowned upon. As this passage demonstrates, history and literature have been removed from this society. History and literature are subjects that connect people, and tie them together, but without them, this passage shows that this society is very advanced in the field of science. This society is clearly appalled by life led by their ancestors. They have effectively gotten rid of history, and any feeling that helps them make lasting connections to other people. Through the use of descriptive diction, the authors purpose of providing insight into this society is fully accomplished. The diction in this passage illustrates how dynamic the society in this novel is. This society revolves around science, and wants nothing to do with the past. This passage provides very important insight into how this society functions, and the structure of the society. The author successfully achieves his purpose through the use of repetition and expressive diction.

The Transition from Applicant to New Employee Essay

The Transition from Applicant to New Employee - Essay Example This study highlights both the employee and employer struggle in the initial period of the recruitment process to make the transition as smooth as possible and shorten the learning curve. Organizations start this process as soon as they get an application against a vacancy. The interview process and the orientation for the new employee become the foundations of a lasting relationship. Successful organizations foster a learning environment in which employees get to build their skills and eventually become more productive with time. The employee entering the organization relies on the existing culture and workforce for guidance and deliverance. Employees adopt the values of the culture prevailing in the organization and will easily adapt to the new environment if they feel comfortable to it. Employees will also be more receptive of information if they feel attached to the work they are put to do. As the discussion stresses millions of students graduate every year form colleges and universities around the globe. Many of them could be in search of their first real job. The past twenty years of their life they have been cradled with support from friends, family, counsellors, instructors and the corporations that hold yearly seminars. After graduating from college, they may find themselves completely alone, standing in front of a tall building, thinking of which door is the entrance and which door is the exit. Confidence matters a lot as they go in for an entry test or start the interview process.

Romantic music and development of Renaissance painting Essay

Romantic music and development of Renaissance painting - Essay Example Another similarity between Romantic music and paintings during Renaissance lies in the fact that they both put a great emphasis on the importance of the figure of the artist. It would not be a mistake to suggest that the cultural titans of Italy were as much respected as their counterparts in the musical world of Europe during Romanticism. Indeed, in that period every person who was able to create a fine piece of music was considered to be extremely talented and was approved by the public. Just like art in the times of Renaissance, music during Romanticism was considered to be the highest of arts; so the people who wanted to devote their live to it were considered to be exceptional. There is one more point that should be mentioned while considering the development of the two concepts that were discussed above. Thus, just like during Renaissance, Romanticism in music contributed to the emergence of the new perception of this kind of human activity. One might point out that visual art, just like music have existed in within human civilization for thousands of years, it was those two periods when people started to treat them in a different manner. This process, accompanied by the revival of interest, is what truly differed those periods from others. Some researchers argue that Renaissance made the aesthetic thought of humanity look backwards, but move forward with what they saw in the past. However, in order to get a better understanding of the relationship between the two notions in question.

Franklin D. Roosevelt Essay Example for Free

Franklin D. Roosevelt Essay Franklin D. Roosevelt is one of the most important and influential American political figures in the 20th century. Elected four times in office, his twelve years in the White House proved to be a testament to American courage, especially when faced with great challenges such as the Great Depression and the Second World War. Franklin D. Roosevelt, often called FDR, was born to James and Sara Delano Roosevelt in January 30, 1882 at Hyde Park, New York. (Potts, 5) The Roosevelt family was a rather affluent and Franklin was educated most of his younger years with tutors. In 1900, he enrolled at Harvard University and ended his college career at Columbia University Law School. (Potts, 7) On St. Patricks Day, 1905, Franklin married Anna Eleanor Roosevelt, a distant cousin and the niece of President Theodore Roosevelt. Franklin Roosevelt greatly admired his fifth cousin, President Theodore Roosevelt who ascended to the presidency during Franklin’s freshman year at Harvard. On several instances, Franklin visited the White House to discuss issues with his cousin Teddy. It is inevitable then that Franklin would have a growing interest in joining politics. He entered public service just as his cousin did, but as a Democrat in New York, a known Republican state. This proved to be a liability and problems arose but eventually, in 1910, Franklin was elected to the New York Senate. (Coker, 11) Three years later, in 1913, President Wilson appointed him Assistant Secretary of the Navy, something he had in common with his cousin Teddy. In the years that passed Franklin proved his mettle in politics and became the 1920 Democratic nominee for Vice President. Things went well in Franklin’s life until at age 39, in the summer of 1921, he got a stricken with poliomyelitis. This was a major setback but never deterrence to his courage. Franklin fought hard to be able to use his legs again through swimming. At the dramatic 1924 Democratic Convention, Franklin appeared, wearing crutches, to nominate Alfred E. Smith as the Happy Warrior. In 1928 Roosevelt became Governor of New York. (Friedel, 69) By this time, the economy is collapsing and as governor, he retained his reformist stance pushing for the conservation of the state aid to the unemployed citizens. His political career eventually reached its culmination when he was nominated for the 1932 presidency by the Democrat party. In his acceptance of his nomination, he said â€Å"I pledge you, I pledge myself, to a new deal for the American people.† This was what he came to be known for and in November 1932, Franklin was elected to his first term in as president of the United States. His administration became synonymous to the new deal he had pushed for in his campaign. (Heale, 3) It was not an easy term though. When he was elected for president, Franklin had inherited a lot of problems. This was the time when America was at the depth of the Great Depression and by March, four months into his presidency, 13,000,000 Americans were unemployed, and almost every bank was closed. The first hundred days of his office proved to be difficult. In these days Franklin had Congress implement a sweeping program to resurrect the ailing business and agriculture, to give relief to the unemployed and to those about to lose their homes and farms. He pushed for reform, especially through the Tennessee Valley Authority. Franklin Delano Roosevelt showed the people that something can be done. He gained immense admiration by helping the American people regain faith in themselves. He brought direction and hope as he assured prompt, vigorous action towards the depression. As Franklin asserted in his Inaugural Address, the only thing we have to fear is fear itself. This was precisely the attitude of his administration that created impact. In three years, the FDR administration led the United States to some measure of recovery, but the experimental and aggressive nature of Roosevelt’s New Deal program had turned up the noses of businessmen and bankers. They feared his ventures, were dismayed by the allowed deficits in the budget and being taken off the gold standard, and more so, the businessmen and bankers alike were hated the concessions to labor. Sensing this, Roosevelt created a new program of reform: Social Security, larger taxes on the wealthy, new controls over banks and public utilities, and a massive relief program for the unemployed. This new burst in legislation helped Roosevelt to a re-election in 1936. Roosevelt brought in more reforms to his administration. Feeling he had a favorable and popular mandate, he then sought legislation to enlarge the Supreme Court, which had been creating problems with his New Deal policies. Roosevelt lost the Supreme Court battle, but this sparked a revolution in constitutional law. Thereafter, the Government could legally regulate the economy. (Friedel, 69) During the latter part of his second term however, foreign crises loomed over domestic problems. In 1939 the war in Europe broke out and the fear that America would get entangled in this gave Roosevelt an opportunity to get elected again in 1940. This was defiance to what should have been a maximum of two presidential terms. (Heale, 4) Nevertheless, Roosevelt received strong support from big cities and on his third term as president, he pledged the United States to the good neighbor policy, transforming the Monroe Doctrine from a unilateral American manifesto into arrangements for mutual protection against assailants. He also struggled to keep the United States out of the war in Europe through neutrality legislation but at the same time he pledged to help reinforce nations in danger. In 1940, when France fell and England came under siege, he began to send Great Britain all possible aid except actual military involvement. Inevitably though, on December 7, 1941, the Japanese attacked Pearl Harbor. That day, Roosevelt directed all of the Americas resources and manpower and the nation plunged into global war. Roosevelt, in the years after, devoted careful thought in his dealings and strategies with other nations and allies. He was crucial in the planning of a United Nations, wherein, he hoped, international differences and difficulties could be solved. Roosevelt proved to be highly influential throughout the war but towards the end of the war, his health worsened, and on April 12, 1945, while at Warm Springs, Georgia, Roosevelt died of a cerebral hemorrhage, thus ending the longest presidential term in American history. (Friedel, 69) Works Cited Coker, Jeffrey W. Franklin D. Roosevelt: a biography. Greenwood Publishing Group, 2005 Freidel, Frank. Presidents of the United States of America. DIANE Publishing, 1994 Heale, M. J. Franklin D. Roosevelt: the New Deal and war.   Routledge, 1999 Potts, Steve. Franklin D. Roosevelt. Capstone Press, 2006

A Kantian Interpretation of Demonstrative Reference :: Philosophy Philosophical Kant Essays

A Kantian Interpretation of Demonstrative Reference ABSTRACT: According to Kant, we refer to what is out there in the world by performing a demonstrative act, like pointing at an object with a finger. A Kantian mode of demonstrative reference is characterized by the existence of a real, 2-placed affective relation between an intuiting subject and the referent. Parsons suggests that Kantian intuition is both singular and immediate, and immediacy demands an object of intuition to be present, a condition clearly satisfied by objects within our immediate perceptual field. But since we do not have an immediate relation with remote objects, the scope of our demonstrative reference is severely restricted by intuitional immediacy. I wish to develop a global Kantian intuition in order to extend the scope of demonstrative reference. Kant's ontology of space entails that the global representability of space be given to an intuiting subject as a form of intuition. According to Melnick, Kantian intuition is a kinematic operation which involves dir ecting attention and moving about. To make contact with the world, the subject must move away from its locale: although a spatially remote object (W) is not immediately present, we can shift our location by taking a path such that W will become so. Once we are close enough to be affected by W, we will be able to point at W and say "This." Thus, the intuitive scope of demonstrative reference is globalized as we shift our location. I A. The Semantic Content of "This" It has been suggested that Kantian intuition is analogous to the demonstrative term "This." According to Sellars, "to intuit is to represent a this." The demonstrative "This" provides a semantic model for Kantian intuition, but with some restriction. We can certainly apply the demonstrative "This" to individual items which are not proper objects of intuition, e.g., "This theory," "This thought," or "This proposition." The singularity of "This" is insufficient to characterize Kantian intuition. Since space and time are the forms of intuition, an intuitable object must have a spatio-temporal location. Hence, the demonstrative "This" is a semantic model for Kantian intuition only if it is "spatio-temporized." We can spatio-temporize "This" by performing a demonstrative act. The type of a demonstrative act can be characterized by a "2-placed de re ostension" as suggested by Howell. The function of a de re ostension is to indicate the presence of an object in our perceptual field. Pointing at an object with a finger is an example of a 2-placed de re ostension par excellence.

Reporting Stockholders Equity

ckChapter 11 – Reporting and Analyzing Stockholders’ Equity I. Characteristics of a Corporation (Publicly held (closely held)) * Separate legal existence; * Limited liability of stockholders; limited to investment * Transferable ownership rights; * Ability to acquire capital; * Continuous life; * Corporation management: Shareholders Shareholders * Voting rights * Profit sharing * Preemptive right * Residual claim Board of Directors Board of Directors CEO(PRESIDENT) CEO(PRESIDENT) . other vps . other vps CIO CIO CFO CFO COO COO Treasurer Treasurer ControllerController * Government regulations; file application with state government-> corportate charter by-law * Additional taxes. Double taxation II. Stock Issue 1. Basics of Stock Issue: (1) Authorized Stock: The maximum amount of stock that a corporation is authorized to sell by corporate charter. (2) Outstanding Stock: Capital stock that has been issued and is being held by stockholders. Legal capital= # of issued shares x par value per share (3) Par Value Stock: Capital stock that has been assigned an arbitrary value per share in the corporate charter. 4) No-par value Stock: Capital stock that has not been assigned a value in the corporate charter. (5) Stated Value of No-par value Stock: Value per share assigned by the board of directors to no-par value stock. Authorized Issued Outstanding (6) Paid-in Capital: Amount paid to corporation by stockholders for shares of ownership. (7) Retained Earnings: Earned capital held for future use in the business. 2. Accounting for Common Stock Issues: (1) Issuing Stock at Par Example 1: On March 1, 2002, XYZ Company issued 10,000 shares of $10 par value common stock at par. (2) Issuing Stock above ParExample 2: On June 10, XYZ Company issued 5,000 shares of $10 par value common stock at $12 per share. Cash 60,000(=5,000Ãâ€"12) Common Stock50,000 Additional paid in capital14,000 (Paid in capital in excess of par) What if the common stock issued on June 10 is n o par stock with a stated value of $10? Cash60,000 Common Stock50,000 Additional Paid in capital10,000 3. Treasury Stock: * A corporation’s own stock that has been issued, fully paid for, and reacquired by the corporation but not retired. * Issued but not outstanding (1) Corporations acquire treasury stock to †¦ reissue shares to employees under bonus and stock compensation plans; * increase trading of company’s stock in securities market to enhance market value; * reduce number of shares outstanding , and therefore increase earnings per share (EPS); * prevent a hostile takeover. (2) Purchasing Treasury Stock: * Cost method: Treasury stock is increased by the amount paid to reacquire the shares, and is decreased by the same amount when the shares are later sold. Example 3: On October 15, 2002, XYZ Company acquired 2,000 shares of the stock issued on June 10 in Example 2 at $9 per share.On the balance sheet: Stockholders equity Paid in capital Common stock (par) Ad ditional paid in capital Retained earnings Less: Treasury stock (a contra equity account) * Effect of purchasing treasury stock on common stock: * Effect of purchasing treasury stock on stockholders’ equity: III. Preferred Stock * Preferred stock has contractual provisions that give it preferences over common stock in dividends and assets in the event of liquidation. * Preferred stockholders do not have voting rights. Example 4: On November 5, 2002, XYZ Company issued 5,000 shares of $10 par value preferred stock for $13 per share.Cash65,000 Preferred Stock50,000 Additional Paid in capital15,000 1. Dividend Preference * Preferred stockholders have the right to share in the distribution of corporate income before common stockholders; * The first claim to dividends does not guarantee dividends; * Cumulative Dividends: Preferred stockholders receive current and unpaid prior-year dividends before common stockholders receive any dividends. When dividends are cumulative, preferred dividends that were not declared in a given period are called dividends in arrears. Example 5:XYZ Company issued 10,000 shares of 10%, $5 par value cumulative preferred stock On January 1, 1999. XYZ had not declared any dividends until December 31, 2002. 1999: 10,000x 5 x 10% = 5,000 2000: 5,000 2001: 5,000 2002:5,000 Dec 31, 02: $20,000 in cash * Dividends in arrears are not liability. They should be disclosed in the notes to financial statements. 2. Liquidation Preference- Creditors Prefered stock holders common stock holders IV. Dividends * A distribution by the corporation to the stockholders on a pro rata basis. 1.Cash Dividends: (1) To pay a cash dividend, a company must have: * retained earnings * adequate cash * declared dividends (2) Some Important Dates: * Declaration date: the date the board of directors formally authorizes the cash dividends and announces it to stockholders. Retained earnings Dividends payable * Record date: The date ownership of outstanding shares is de termined for dividend purposes. * Payment date: The date dividends are paid. Dividends payable Cash * Cumulative effect of declaration and payment of cash dividends on accounting equation: 2. Stock Dividends: Companies pay stock dividends to †¦ * Satisfy stockholders’ dividend expectations without paying cash; * Increase the marketability of its stock; * Emphasize that a portion of stockholders’ equity has been permanently reinvested in the business. * Small Stock Dividend: If the stock dividend is less than 20%-25% of the corporation’s issued stock, it is recorded at the fair market value per share. * Large Stock Dividend: If the stock dividend is greater than 20%-25% of the corporation’s issued stock, it is recorded at par or stated value per share. Example 6:On February 1, 2003, the balance of XYZ Company’s retained earnings was $2,500,000. XYZ Company declared a 15% stock dividend on its 100,000 shares of $10 par value common stock. The cu rrent fair market value of XYZ Company’s stock is $13 per share. Retained earnings195,000 Stock dividend Distributable150,000 Additional paid in capital45,000 On March 1, 2003, XYZ Company issued the dividend shares. Stock dividend distributable 150,000 Common Stock150,000 – Effect of stock dividends on stockholders’ equity and its components: S/E Retained earnings195,000 (Decrease)Common Stock150,000 (Increase) Additonal paid in capital45,000 (Increase) NET EFFECT: No change V. Stock Splits: * The issuance of additional shares of stock to stockholders accompanied by: * A reduction in the par or stated value; * An increase in number of shares. No entry * Effect of stock splits on stockholders’ equity and its components: S/E Common Stock (Par value per share x total # of issued shares) Add. Paid in capital Retained Earnings VI. Retained Earnings: * Net income that is retained in the business. Revenues (Credit, transfer to credit of income)Income Summary(Tr ansfer N. I to retained earnings credit) Retained Earnings Expenses (Transfer debit to debid of income summary) * Deficit: a debit balance in retained earnings. Deficit is reported as a deduction in stockholders’ equity on the balance sheet. * Retained earnings restrictions- Debt covenants VII. Financial Statement Presentation: 1. Balance Sheet S/E Paid-in-capital Common stock (par value) Preferred stock (par value) Additional paid in capital Retained earnings Less: Treasury Stock 2. Statement of Cash Flows Cash Flows from Financing ActivitiesIssuance of stock (cash inflows) Repurchase of stock (cash outflows) Dividend payment (cash outflows) VIII. Ratio Analysis: 1. Dividend Record * Payout Ratio: Cash dividends declared on common stock/ Net income 2. Earnings Performance * Return on common stockholders’ equity ratio: (NI-Prefered stockholders dividends)/Average common stockholders equity 3. Debt versus Equity Decision | Bond| Common Stock| Owners’ Control| Not affected| Diluted| Tax Benefit| Bond interests are tax deductible| Dividends are not deductible| Financial Ratio(EPS)| Not affected| Lower| Fixed payment| Yes | No|

Gender discrimination in society and the workplace Essay

In recent years women have been making gains toward equality in the workplace, but still there is a pay gap that separates men and women. It is interesting to note that women are consistently compensated less than men who fill similar positions. Discrimination is blamed for the salary disparities. My guess is as long as there are differences between people, there will be discrimination in one form or another. That may be only a general thought about discrimination, but men and women are always going to be different. How are we affected by such forms of gender discrimination? Well obviously those who are directly impacted negatively can feel the effects, but undoubtedly society and the economy are impacted as well. It may be difficult to determine in what ways they may be affected however. It seems that through the years, there has never been a time where women have been as well compensated as men. Just because its something we may be used to, does that mean it’s right? Some people would argue that women shouldn’t even be working as it is. Many people think that a woman’s place is in the home. Perhaps that is the ideal in many societies. It would seem beneficial to have at least one parent in the home caring for children rather than placing them into a daycare facility. Traditionally the husband has been the breadwinner of the household, but with inflation rates skyrocketing, it is increasingly necessary to send the wife off to work as well. Of course women should be treated as equals and be paid the same that a man would be if he were filling the position. One way or another this problem should take care of itself or it could be speculated that there will be an increasing amount of animosity among members of society. Long-term effects of gender discrimination are not clear, but why should we continue to place barriers between different people? The government has seemed to be cracking down on equal opportunity and anti-discrimination laws, as they should be. The United States is a place of equality and equal opportunity, and while we may be huge steps ahead of other countries, gender discrimination is still a factor that must be dealt with.