Reflection Essay- Role Play of Zenur Levon Negotiation

Reflection Essay- Role Play of Zenur Levon Negotiation Self reflection states about own character, self knowledge, feelings and own thoughts and which part needed to improvement. In other words,Self reflection defines ones own weakness and strengths and about ones own behavior and experience (Neaum, 2012). In this self reflection, I will be explaining about my group experiences, Zenurs plan and how we got a best deal for our company through negotiation process. In this role play we followed the negotiation process steps like planning, discussion, bargaining about proposal offer and closing step. Zenur and Levon were well known companies. Zenur used the interactive model of effectively communication during the negotiation. Both companies had same business market. This negotiation process helped both companies to know about their weakness and strengths. The negotiation of Zenur with Levon went efficiently because both organizations had similar business areas and it was beneficial for both to influence the each others strengths. Zenur got information and data about Levon Company and made plan to achieve their goal and which brought benefit for both companies. In the process of negotiation, we came up with Zenur as a selling company. We discussed about our strategies, data, information, ideas and knowledge which we used during the negotiation to convince Levon Company. Moreover this information helped us to achieve our target. Zenur and Levon discussed their ideas, their company goals, achievements and their future plan with each others while negotiation. Because their share ideas, knowledge and helping each others helps to get a good performance in group activities (Bernstein, 2015). Levon gave three offers to take over Zenur Company which was $350 million with full control and $400 with full control of acquition. Zenur Company CEO (leader) discussed with Finance manager (myself) and we refused this offer because of some valid reason. Levon and Zenur were bargaining and discussed their companies point of view. Both companies agreed with $425 million with 50-50% profit sharing and will keep and give promotion to Zenur staff as we discussed with Levon. After this negotiation, both companies signed written contract and Zenur make sure that Levon will take three months for complete whole process. Zenur used their strategies, skills and styles at the different stages of the negotiation. Zenur meet with their own interests and plan which helped to bring benefits for both companies. In the role play Zenur was able to make their offer better because Zenur focused on their offer and tried to understand Levon current issues and their opinion. Through negotiation and bargaining, Zenur got deal with $425 with 50-50% profit sharing. As a finance manager, I was explained the present position, issues and plans of the Zenur company which will help Zenur and Levon to make their performance better. I was tried to explained companys legal requirement and objectives. I explained why we refused the offer and which are my company requirements? I tried to focus on our company benefits and get a best deal for Zenur. As a finance manager, I was trying to understand the Levons conditions and issues. I was a finance manager who was a one of negotiators of the team, I found some qualities like flexibilities, ability to understand the others point of view and focus on our companys goal. I was able to asked questions and give answers when its needed. I shared my opinions, thoughts and information with others during this process. Because when we working in a group team than every team members have to need to do their best to achieve their group goals and group achievement (DeVito, 2005). Overall, it was a very good experience for me to do work in a group which help me learnt how to communicate with each others. Also we should listen others opinion and ideas and give respect them. Because listening is important this can help us to convey our massage clear to others and helps to make our discussion better (Bernstein, 2015). Moreover as a finance manager learnt how to take a step or discussion immediately in any situation. Moreover, working in group play we can develop our relation with each others and help to make our performance better. I hadnt faced any language barriers in my group. References Bernstein, E. (2015). How active listening makes both participants in a conversation feel better. The wall street journal, 11-13. Cameron, L. (2010). Teaching languages to young  learners. Cambridge: Cambridge University Press. DeVito, J. A. (2005). Essentials of human communication (5th ed.). Boston: Pearson Education. Neaum, S. (2012). Language and literacy ; For the early years. London: Sage Publications Inc.

Continental Drift Theory and Plate Tectonic Theory

In the early 20th century, German scientist Alfred Wegener published a book explaining his theory that the continental landmasses, far from being immovable, were drifting across the Earth. He called this movement continental drift. Wegener noticed that the coasts of western Africa and eastern South America looked like the edges of interlocking pieces of a jigsaw puzzle. He was not the first to notice this, but he was the first to formally present evidence suggesting that the two continents had once been connected. Wegener was convinced that the two continents were once part of an enormous, single landmass that had split apart. He knew that the two areas had many geological and biological similarities. For example, fossils of the ancient reptile mesosaurus are only found in southern Africa and South America. Mesosaurus, a freshwater reptile only one meter (3. 3 feet) long, could not have swum the Atlantic Ocean. The presence of mesosaurus suggests a single habitat with many lakes and rivers. Wegener believed that all the continents—not just Africa and South America—had once been joined in a single supercontinent. This huge ancient landmass is known as Pangaea, which means â€Å"all lands† in Greek. Pangaea existed about 240 million years ago. By about 200 million years ago, this supercontinent began breaking up. Over millions of years, Pangaea separated into pieces that moved away from one another. These pieces slowly assumed their present positions as the continents. PLATE TECTONIC THEORY Plate tectonics is the theory that the outer rigid layer of the earth (the lithosphere) is divided into a couple of dozen â€Å"plates† that move around across the earth's surface relative to each other, like slabs of ice on a lake. There are seven or eight major plates and many minor plates. Where plates meet, their relative motion determines the type of boundary: convergent, divergent, or transform. Earthquakes, activity, mountain-building, and oceanic trench formation occur along these plate boundaries. The lateral relative movement of the plates typically varies from zero to 100 mm annually. Tectonic plates are able to move because the Earth's lithosphere has a higher strength and lower density than the underlying asthenosphere. Plate movement is thought to be driven by a combination of the motion of the seafloor away from the spreading ridge and drag, downward suction, at the subduction zones. Another explanation lies in the different forces generated by the rotation of the globe and the tidal forces of the Sun and the Moon. The relative importance of each of these factors is unclear, and is still subject to debate. The geoscientific community accepted the theory after the concepts of seafloor were developed in the late 1950s and early 1960s. Fun Facts: * The highest mountain range above sea level, the Himalayas, was formed 55 million years ago when the Eurasian and Indo-Australian continental plates converged. Due to ongoing convergence, the Himalayas, including Mount Everest, continue to rise by approximately 2 centimeters (?1 inch) each year. * The Mid-Atlantic Ridge runs down the center of the Atlantic Ocean. Along its crest, the ridge has a deep rift valley that, on average, is similar to the depth and width of the Grand Canyon: 1 to 3 kilometers (0. 6 -1. 8 miles) deep and 6. 5 to 29 kilometers (4-18 miles) wide. * Scientists are able to calculate average rates of tectonic plate movement for a given time period. These rates of movement range widely. For example, the rate of spreading at the Mid-Atlantic Ridge near Iceland is relatively slow, about 2. 5 centimeters (1 inch) per year. This is similar to the rate at which fingernails grow. The fastest known rate of plate movement, 15 centimeters (6 inches) per year, occurs on the East Pacific Rise in the South Pacific. SEAFLOOR SPREADING Seafloor spreading is a process of plate tectonics. New oceanic crust is created as large slabs of the Earth's crust split apart from each other and magma wells up to fill the gap. The large slabs of rock that make up the Earth’s crust are called tectonic plates. As they slowly move away from each other beneath the ocean floor, hot magma from the Earth’s mantle bubbles to the surface. This magma is then cooled by seawater. The new rock forms a new part of the Earth’s crust. Seafloor spreading occurs along mid-ocean ridges—large mountain ranges rising from the ocean floor. New bodies of water and even continents can be created through seafloor spreading. The Red Sea, for example, was created through seafloor spreading, as the African plate and the Arabian plate tear away from each other. Today, the northern Sinai Peninsula connects the Middle East (Asia) with North Africa. Eventually, geologists predict, seafloor spreading will expand the Red Sea so that it will completely separate the two continents. . Seafloor spreading disproves an early part of the theory of continental drift. Continental drift was one of the first theories that the Earth's crust was dynamic and always in motion. Supporters of continental drift originally theorized that the continents moved (drifted) through unmoving oceans. Seafloor spreading proves that the ocean floor itself is the site of tectonic activity. Subduction is the opposite of seafloor spreading. Subduction happens where tectonic plates crash into each other instead of spreading apart. In subduction zones, the edge of the heavier plate subducts, or slides, beneath the lighter one. It then melts back into the Earth's mantle. Seafloor spreading creates new crust. Subduction destroys old crust. The two forces roughly balance each other, so the shape and diameter of the Earth remains constant.

Mesopotamia vs. Egypt Essay

When you think about Mesopotamia and Egypt you may think that they are very different. They are, but they also have many similarities and differences as well. Both of these societies have done things that have effected the way we live today. One similarity is they were both polytheistic, meaning that they believed in many gods. Another similarity is the both had their own writing system. Two differences they have are their feelings about the afterlife and their rivers. A similarity between the Mesopotamians and Egyptians is they both had their own writing system. The Egyptians used hieroglyphics which used pictorial symbols that represented sounds, concepts, or syllables. Because it took so long to learn how to read and write using hieroglyphics, scribes and priest were mainly they only ones who used it. The Mesopotamians used cuneiform. Cuneiform was basically wed-shaped symbols that represented words or syllables. Because so many symbols had to be learned, literacy was confined to a very small group made up of priest and scribes. Cuneiform originated in Mesopotamia but was then used by the Sumerian and Akkadian. Another similarity is both the Mesopotamians and the Egyptians were polytheistic, meaning that they believed in many gods. Both believed that everything happened because of the gods, and if you made the gods mad then you would be punished. The Mesopotamians were a little more skeptical about the gods compared to the Egyptians, the Egyptians were very optimistic about the gods. Also, both groups were very dependent on the gods and prayed to them daily. Many of their gods had to deal with nature. A difference between the two is their rivers. The Egyptians relied on the Nile river. It would flood often, but it was predictable. Because of this, the Egyptians built their homes where they wouldn’t get destroyed. They would also used irrigation to help their crops when the river would flood. The Mesopotamians had the Tigris and Euphrates river. It would flood Mesopotamia at unpredictable times at least once a year. The floods would destroy many homes and buildings. Another difference between Mesopotamia and Egypt is their outlook on death. The Egyptians spent their whole lifetime planning for the afterlife, they even planned their burial. After death hey were mummified and buried with their prized possessions and things such as food to help them along their trip to the afterlife. But the Mesopotamians had a bad outlook on death. They believed they gods were harsh, and did not look forward to the afterlife. As you can see Mesopotamia and Egypt have many similarities and differences. They are similar by both having their own writing systems and they were both polytheistic. They are different because of their outlooks on the afterlife and the flooding of their rivers. Both of these civilizations have shaped us today. Without them we wouldn’t be the world we are now.

Organic Chemist Job Profile

This is an organic chemist job profile. Learn about what organic chemists do, where organic chemists work, what type of person enjoys organic chemistry  and what it takes to become an organic chemist. What Does an Organic Chemist Do? Organic chemists study molecules that contain carbon. They may characterize, synthesize or find applications for organic molecules. They perform calculations and chemical reactions to achieve their goals. Organic chemists typically work with advanced, computer-driven equipment as well as traditional chemistry lab equipment and chemicals. Where Organic Chemists Work Organic chemists put in a lot of time in the lab, but they also spend time reading scientific literature and writing about their work. Some organic chemists work on computers with modeling and simulation software. Organic chemists interact with colleagues and attend meetings. Some organic chemists have teaching and management responsibilities. An organic chemists work environment tends to be clean, well-lighted, safe and comfortable. Expect time at the lab bench and at a desk. Who Wants to Be an Organic Chemist? Organic chemists are detail-oriented problem solvers. If you want to be an organic chemist, you can expect to work in a team and to need to communicate complex chemistry to people in other areas. Its important to have good oral and written communication skills. Organic chemists often lead teams or organize research strategies, so leadership skills and independence are helpful, too. Organic Chemist Job Outlook Presently organic chemists face a strong job outlook. Most organic chemist positions are in industry. Organic chemists are in demand by companies that produce pharmaceuticals, consumer products, and many other goods. There are teaching opportunities for Ph.D. organic chemists at some colleges and universities, but these tend to be highly competitive. A smaller numbers of teaching and research opportunities exist for organic chemists with masters degrees at some two and four-year colleges.