Geography And History Assessment Of Ancient Olympia

Geography and History assessment Sophia Justice 2016 Ms Touma and Mr Skinner Geography: Question 1: Using two different types of maps show the location of the site of Ancient Olympia. Political map of Ancient Olympia Physical map of Ancient Olympia Question 2: Outline the World Heritage Criteria the site of Ancient Olympia meets. Refer to specific criteria. The Site of Ancient Olympia meets the World Heritage Criteria in points i, ii, iii, iv and vi. The Site of Ancient Olympia is not only a famous masterpiece of beauty, but beneath it’s mask lies knowledge embedded with facts about history, geography and multiple things which we are yet to discover. It also has religious value to the world and is the place where the original Olympic games originated. Point i states that it is a masterpiece of human creative genius which reminds us of the beauty of the architecture in Ancient Olympia. Points ii, iii and vi explain the culture and history behind the site and point iv yet again talks about the amazing architecture which the site has been enhanced with. For these reasons, the site of Ancient Olympia meets the World Heritage Criteria in many ways. The Site of Ancient Olympia Question 3: Explain TWO reasons why the Site of Ancient Olympia needs to be preserved. 1) One of the main reasons that the Site of Ancient Olympia needs to be preserved is because of its religious importance to the society. AncientShow MoreRelatedProject Mgmt296381 Words   |  1186 Pageslearned [8.3.3.4] 9.4.2.2 Individual performance appraisals Chapter 7 Managing Risk Chapter 15 Chapter 16 International Projects Oversight 11.1 Risk management process [F.8] 11.2 Identifying risks 11.3.2.2 Impact matrix 11.4 Risk assessment 11.5 Risk responses (.2–.1.2) 11.6 Risk register 7.1.2.5 PERT analysis 7.1.2.6.3 Contingency reserves 7.3.3.4 Change control management G.7 Culture awareness 1.4.4 Project offices 8.1.2 Continuous improvement 5.1 Requirements vs. actual [5.3]

Admj Free Essays

3 December 2012 Court Proceedings The best part about criminal procedures here in the United States is that criminal defendants have a lot of protections and guarantees. They have the guarantees of due process, equal protection under the laws, the right to have legal counsel present, the right to confront witnesses, the right to a jury trial, and the right to not testify against themselves. In the movie and in real life we see this all the time. We will write a custom essay sample on Admj or any similar topic only for you Order Now For example the way due process was portrayed in the movie was the way that all the information that was against the boys they had the right to have the documents that had the information against them. All defendants get the same protection regardless of the acts they have committed, in the movie the boys had the right to have a lawyer, they just couldn’t afford one so that’s why Billy had to call his uncle. Confronting witnesses was the exact act that Uncle Vinny did when he was almost out of hope, he managed to cause doubts in the jury’s eyes when he showed them that the old woman was nearly blind and when the other two men also began questioning what they had really seen. The boys also had the right to trial by jury, which just means that the judge doesn’t convict the defendant, the jury does instead. The last right defendants have is the right to not testify against themselves, in the movie that was the first thing the boys shouldn’t have done because right away they admitted to a crime that they did not do. Moving on to some of the key points and the purpose, criminal procedure deals with the set of rules which the government enforces law. How to cite Admj, Essay examples

Rock Joints free essay sample

A joint is defined as a fracture in a rock between the sides of which there is no observable relative movement. They are present is most consolidated rocks of igneous, metamorphic and sedimentary origin. Joints may form as a result of either diastrophism or contraction. Description: (i) A series of parallel joints is called a joint set. (ii) Two or more joint sets intersecting each other produce a joint system. (iii) Two sets of joints nearly at right angles to one another, produced by the same stress system, is known as conjugate system. iv) A persistent joint or set which may be horizontal or vertical is called master joint. Classification: 1. According to the mode of origin, three types of joints have been recognised, as follows: (a) Tensional joints: These are also known as shrinkage joints. In igneous rocks, they are produced as a consequence of contraction due to cooling. Columnar Structure which characterises many basic extrusive and intrusive, consists of long hexagonal blocks closely packed together. We will write a custom essay sample on Rock Joints or any similar topic specifically for you Do Not WasteYour Time HIRE WRITER Only 13.90 / page In granites and granodiorites several sets of joints may be observed, but commonly three sets are prominent-one horizontal and two vertical at right angles to each other and to the Horizontal set. If these sets are more or less equally spaced, the fracture planes give rise to cubical blocks; the jointing is then termed Mural jointing. Joints formed in little deformed sedimentary rocks are due to tension caused by compaction and shrinkage as sediments are considerable into sedimentary rocks. Tensional joints may also be due to deformation. b) Sheet joints: These joints develop in sets and are more or less parallel to the surface of the ground, especially in plutonic igneous intrusions such as granite. They may originate due to unloading of the rock mass when the cover is removed through the processes of erosion. (c) Tectonic joints: These are also known as shear joints. They are formed in a rock under compression. They originate as a direct result of folding or thrusting in rocks. Gen erally they are of three types: (i) Strike set: Longitudinal joints parallel to the fold axis. (ii) Dip-set: Also known as cross-joints, perpendicular to the longitudinal joints. (iii) Diagonal set: Which is a conjugate set of oblique joints, -which lie at rather less than 45Â ° to the direction of tectonic-axis. 2. According to the geometric classification of joints, there are three important varieties, like strike-joints, dip joints and diagonal joints, which are totally with respect to the regional strike and dip of the country rocks. Joints may be open or closed. The closed joints are also known as latent, blind or incipient joints. They may become open as a result of weathering, which is commonly found in jointed lime- Stones. Recognition of joints in the field and their effects on out crops: Joints are generally recognised in the field as faults without displacement. Their dimension varies within wide-limits. Sometimes they are very short in their extension, but in certain cases they are found to extend for miles together. Joints commonly control the drainage pattern of an area. They also determine the shape of coastlines, because they provide a passage, whereby water may penetrate deeply into the rockmass, thus allowing weathering to take place. Jointed rocks are pervious to fluids and hence may act as aquifers or reservoir rocks for oil or natural gas. The presence or absence of joints in a region matters much to quarrymen and miners because it determines the ease with which query and mining can be accomplished. Sometimes joints act as avenues for molten rock materials to come above the surface. It also determines the localisation of some mineral deposits.