Thursday, March 26, 2020

Hamlet Essays (614 words) - English-language Films, British Films

Hamlet Bryce Nations 4/28/00 Smith Lit112 Crumbling Castle Hamlet is a complex play with many characters that each has an important role in the development of the story line. In the play, Rosencrantz and Guildenstern are inserted for nothing more than comic relief. But on the contrary, in the movie they are hopeless wanderers looking for meaning in the world. The pair is so lost in their mental endeavors that they do not even notice the crumbling of a royal family and ultimately their own deaths. Through Rosencrantz and Guildenstern we learn many lessons of the laws of nature and mathematics. They find answers to some of the worlds most difficult problems that have not even begun to be discovered according to the history books. Such discoveries as Newton's law of gravity, the steam engine, and the theory of probability can all be solved in their own somewhat idiotic ways. They also argue and prove to each other the obvious puzzles in life. When trying to demonstrate the difference in which objects fall, Rosencrantz says, You would think that the iron ball would fall at a faster Nations 2 rate than this feather. Upon dropping the objects the iron ball plummets to the floor while the feather floats to the ground proving a common fact. There are significant differences between the movie and the book. In the book the real world is that of Elsinore to which Rosencrantz and Guildenstern are brought into. The movie puts Rosencrantz and Guildenstern in a make-believe world on a journey through the play of hamlet. In the movie the real world is represented by featureless rock and desolate forests, through which the pair journeys to find meaning. The only thing they can seem to remember is a royal summons given to them from the king of Denmark. Chance is a central image that is associated with the two throughout the film and was shown through the coin toss. The fact that the coin always landed upon the heads side could also serve as foreshadowing the pair's death. For there seems to be an almost one hundred percent probability that the coin will land on heads and an almost one hundred percent probability that they will be beheaded. The players have a key role in both the film and text. They provide an important role in catching King Claudius in the text and serve as comic relief in the film. They are first introduced in the film when they bump in to Rosencrantz and Guildenstern on the way to the castle. They beg for audiences saying that without one actor's are useless and then begin to sound off a list of possible performances. The last scene in the movie shows the players riding off down the same road that Rosencrantz and Guildenstern first traveled. This is hinting that perhaps all the action has taken place within the players wagon and stage. Nations 3 The characters within Elsinore remain constant with their actions between the text and film. The story of Hamlet shows the downfall and desecration of the role Denmark family. All the characters within the walls of Elsinore rot and begin to fall apart by the end of the story. Many of them succumb to plain madness like Prince Hamlet and Ophelia. It is almost as if a wave of evil has attacked the once peaceful castle bringing murder and betrayal upon all within it. At the end of the text the characters all seem to be composed of hatred and vengeance. But this could also be considered their decomposition into wild animal like people who murder at will. In both the film and text no problem seems to have a clear solution. Shakespeare Essays

Friday, March 6, 2020

Deserts, glaciers and climate

Deserts, glaciers and climate Geological features have historically provided dramatic and enchanting views for people. Some examples include mountain peaks, desert surfaces and coastal cliffs. Despite providing magnificent sceneries, the potentially harmful nature of some of these features provides hazards to the society.Advertising We will write a custom essay sample on Deserts, glaciers and climate specifically for you for only $16.05 $11/page Learn More Landslides and volcanic eruptions have always been cataclysmic, leading in loss of lives. These features have been used in scientific research studies while others serve as tourist attractions. The features display some similarities and differences depending on whether they are in desserts or glaciers. Desert landscapes cover slightly over one third of the land surface on earth (Hallmann Steinberg, 2000). They are usually dry, receiving extremely minimal rainfall, thus supporting a small number of life forms. The vicinity frequently e xperiences harsh climatic conditions typified by either exceptionally hot or extremely cold. There are diverse forms of deserts classified depending on the quantity of rainfall received and its location. The contrast between the desert and glacial landscape is the extreme weather conditions and landforms dotted across the surface. The desert landscape is characterized by kilometers of dunes and stone surfaces. Stones of unlike solidity and constitution erode at singular rates to fabricate the splendid wilderness imagery. Several features including playas and blowouts make up the desert landscape (Ryan, 2008). Glaciers also face displacement and erosion, similar to deserts, which result in the formation of landforms. The glacier rubs out substances underneath it as it shifts leaving matter on rocks (Ryan, 2008). The glacier accumulates the material which it eventually deposits elsewhere, giving evidence to their direction of movement. The resulting landform of the desert landscapes i s characterized by its configuration through wind actions and weathering. When the globe heats up, warm air, which is less heavy, physically ascends to the summit headed for the poles while cold air settles down. This breeze process is though affected by the revolving of the world thus fashions a sidetracking energy on the current of air. The rotational speeds of the wind depend on the distance from the equator (Ryan, 2008). The speed of rotation is frequently zero and the poles and gradually increases towards the equator.Advertising Looking for essay on geology? Let's see if we can help you! Get your first paper with 15% OFF Learn More Glaciers are formed when it is cold enough for ice not to melt during winter snow. This climate is normally experienced in elevated areas around the polar. Huge accumulations of snow must exist in a gently sloping rocky area which will prevent its loss (Hallmann Steinberg, 2000). Molecules in the ice are reorganized without c hange of physical structure, forming new crystals. Even though it is presently being amplified by the media, climatic changes have historically being there. The year of climatic change can be determined through scientific research in ocean sediments and tree rings. Volcanic upsurges around the terrain and changes in path directions are some of the causes of weather modifications. Some of the effects of this change were ice ages and interglacial periods when the planet was warming. Natural sources like volcanoes result in greenhouse gases such as carbon dioxide (Ryan, 2008). The presence of the gases adds to the chilling and temperate occurrences. The earth may begin to cool due to adjustments in its orbit. More CO2 thus dissolves in the oceans hence making the planet much cooler (Hallmann Steinberg, 2000). Wild forest fires and other sources of heat radiation make the earth warmer. The oceans receive less CO2 hence gets warmer. There was a small cooling event around the 16th centur y caused a slight cooling of the earth. The earth experienced warming during the medieval times across different regions such as Europe. The beginning of the industrial age is however the time when the earth started experiencing continuous warming. This results from the production of greenhouse gases through industries, automobiles and manufacturing activities. Climatic change has resulted in overall heat increase. Patterns of rainfall have changed in various regions, exemplified by more rainfall in certain regions and occasionally in others. Aquatic levels have been progressively expanding, increasing by more than ten centimeters. In the 21st century, temperatures will rise; hence the thawing of glaciers will escalate. There would be extreme weather changes due to the increase in temperatures. The rise of sea levels would interfere with coastlines and activities on beaches. There would be increased erosion and the subsidence of land would thus considerably reduce. The effect on des erts would also be tragic. Life forms, which depend on the little precipitation, would not have any water from streams, which would undoubtedly have dried up. Most deserts on earth are fed by glaciers. Melting of the glaciers due to climate change will impair their water services to the deserts, which will become more arid and incapable of sustaining life.Advertising We will write a custom essay sample on Deserts, glaciers and climate specifically for you for only $16.05 $11/page Learn More They will become hotter and much drier. The soil becomes further degraded through wearing away and compaction (Hallmann Steinberg, 2000). Extreme desertification will lead to more migration and end up overcrowding some areas. There would be further wearing down of the ice resulting in more intense liquefaction. An estimated 1/3 of all glaciers will disappear in less than 100 years. The distribution of river flow and water supply would decrease thus impacting agriculture and production of electricity. Hydrological changes would change navigation systems of rivers, which may provide benefits for shipping industries, which could previously not navigate some areas. Life forms on earth would be threatened if climatic changes exaggerate. Unfortunately, these effects will not be equally distributed across the earth. Some regions will be more adversely affected while some will experience the benefits of the weather changes. Some of its impacts will be irreversible depending on their rate and magnitude. References Hallmann, M. Steinberg, M. (2000). Greenhouse gas carbon dioxide mitigation: Science and technology. Florida: CRC Press. Ryan, J. (2008). Desert and glacial landscapes. Technology: science. November 20, 2008. Web.