Ap Lang College Board Synthesis Essay Student Samples - the Story

Ap Lang College Board Synthesis Essay Student Samples - the Story Ideas, Formulas and Shortcuts for Ap Lang College Board Synthesis Essay Student Samples In doing this you are going to leave a long-lasting impression on the reader that will assist your document stick out from the rest. A complete topic for a synthesis paper is one which encourages you to have a stance on a debatable iss ue. Expository term papers are not the same as different kinds that encourage the reader to present a particular argument or interpretation, as they're meant to explore and explore a single topic in a comprehensive way. It is possible to write a terrific argumentative synthesis essay sample in the subsequent 3 steps. Write down thesis statement that's the major idea of the entire synthesis essay. In the instance of a synthesis essay, it's supplied by the instructor. In that circumstances, the student has a right to choose any topic because of his synthesis essay. Keep in mind it's important to choose the synthesis essay type. Before you start to compose a synthesis essay, identify all the points that you prefer to discuss. Now once you know what a synthesis essay is that can begin working on it! A synthesis essay is about combination. The conclusion should restate the thesis and the principal ideas, although the sentences ought to be worded differently. Look at more than 1 synthesis introduction example to get a range of distinct thoughts and methods because there is more than one method to compose an introduction on precisely the same topic. If you're writing a background synthesis, in some instances it might be appropriate that you provide an interpretation of the material or have a position (thesis). The remainder of your synthesis essay in English should be constructed around that most important sentence. Critical thinking and analysis must make sure high excellent synthesis essay content. Synthesis topics should not be something which's general understanding, including whether vegetables are good for you. The Key to Successful Ap Lang College Board Synthesis Essay Student Samples The close reading is the procedure which follows any very good research. Students should get an idea of what type of research they'll use before they get started, though the research methods might change when the student begins the research procedure. In the event the parents feel they aren't apt at child rearing and they conceive by mistake, they need to be permitted to undergo abortion. What Has to be Done About Ap Lang College Board Synthesis Essay Student Samples Before It Is Too Late If essay writing help is what you're looking for, all of the while paying a minimal price, then EssayPro writing service is the thing to do! The author makes an effort to break the entire topic into separate parts to represent every one of them clearly. You will have to organize your data in a way so that it's simple for your readers to observe all principal ideas. You're able to discover a lot of lists that present various topics for synthesis papers on the internet but the reality is that not all of these are created equal and not all writing ideas are good if you wish to make a huge essay that will stick out. Students have to compose essays based on the teacher's instructions or their preferred style in writing. They may have to write informative essays for any course that they're taking at any level of study. They are given a 15-minute reading period to accommodate the additional reading required for the question. First, they need to understand the nature of the topic about which they must write. What You Should Do to Find Out About Ap Lang College Board Synthesis Essay Student Samples Before You're Left Behind In most instances, the thesis statement is contained in the very first p aragraph of the expository paper. The thesis for an expository term paper will probably recognize the topic and explain how that topic will be explored. If you're writing your essay with some too brief deadline on an exam, you want to stress on your argument in each and every paragraph. Your own essay should be constructed around that text and your principal argument. Here's What I Know About Ap Lang College Board Synthesis Essay Student Samples View essay outline template before going on reading. There's no ideal solution on how best to compose an effective essay. If you lack ideas for the ideal paper ever, we are here to assist. There are two kinds of synthesis that you ought to beware and classify your essay before writing so you abide by its essay format. Since you can see, it's not that simple to compose a synthesis essay. Synthesis essay is typically an essay that incorporates the rest of the topics a rigorous studying to compose a single essay. A synthesis essay prompt has to be negotiable. In addition, it must be well organized just like any other college papers.

The Importance Of Soil And Evaluation Of Taxonomic Evidence

Introduction Using an object centred approach this narrative will attempt to go beyond the subject’s simple classification of a ‘red-figured Stamnos (The British Museum, n.d)’. Analysis of function, status and meaning of this Stamnos provide evidence of how it has changed over time. This is further achieved by examining the production, consumption and afterlife of ‘Attic pottery (Hughes et al., 2014, p.60)’. Production To begin, an intrinsic measure of soil and evaluation of taxonomic evidence identifies this Stamnos as between 450BC-440BC of Athenian provenance. Raw material excavated from a clay bed then transported to the ‘Kerameikos (Wiley Online Library, 2012)’ became divided into component quantities. For decoration a portion†¦show more content†¦Attic vases gained their distinctive red and black colours from this method of firing, presenting a genre known as ‘red figure painting (Hughes et al., 2014, p.92)’. Consequently, in black figure painting the colours are reversed. Often, the addition of White paint distinguished females, who were otherwise underrepresented in often misogynistic evidence from ancient Greek literature. Consumption Meanwhile, assiduous ‘ethnography (Harrison et al., 2014, p.14)’ provides evidence of the consumption habits of Ancient Greeks. High end pottery, designed to promote the owners status, included the addition of precious metals. Society’s elite paradigm of leisure included boisterous ‘drinking games (Hughes et al., 2014, p.92)’. This Stamnos functioned as a vessel for mixing wine enjoyed by heavy drinking Greeks who seldom enjoyed their wine ‘neat’. The average Ancient Greek pursuing a life of temperance regarded Attic pottery as affordable, functional, ‘multipurpose containers for everyday domestic use (Hughes et al., 2014, p.92)’. Proclivities towards Attic pottery, ‘particularly through marriage and funeral ceremonies (Hughes et al., 2014, p.92)’ maintained the Ancient Greek’s piety. Mythical narratives within Attic pottery appealed greatly not only to modern collectors but to Romans and Etruscans befor e them. An example of this appears on this Stamnos, in the form of the iconography upon the warrior’s shield.

The drowning of Carbonate Patforms Get Solution On Clicks

Question: The main geological, oceanographic and physical factors that cause the drowning of carbonate platforms? Answer: Abstract The destruction of carbonate platforms are mostly linked to the short term processes. The study of climatic changes, induced due to the human interactions, would be important for the saving these valuable assets from drowning and decline. However, beyond these factors there are long term processes constantly weakening the growth of the reefs. The abundance of the drowned reefs in tectonically dormant north eastern Australian margin has been attributed to the rates of sea level changes and the margin subsidence. It has been found that the long term growth rates of the reefs are outpaced by the margin subsidence. Introduction The Carbonate platform is in general used to describe a shallow marine sedimentary relief formed by calcareous deposits, along the continental margins. The development of the carbonate platforms are induced by the sessile marine lives which build up reefs with their skeletal deposits or the micro-organisms which cause the sedimentation of carbonates through metabolism. The carbonate platforms may be few to several hundred kilometres thick and wide. The carbonate platforms are found in interesting topographical geometries which range between the two major ones. On one side there are low and gradually sloping ramps or distally steep ramps and platforms with flat tops which have steep margins. The later can be classified as rimmed and non rimmed shelves. Understanding the growth of the microbes and the water turbulence can explain the variety of structures of carbonate platforms. The development or formation of the carbonate platforms requires typical environment conditions. They have been found in tropical as well as the temperate regions. In the tropical belt they have been found between north and south latitudes, as the region where the tropical platform building microbes are found require warm temperatures ( ), shallow clear water are available. In the temperate belts they are available in the region above north and below south latitudes. These regions have cooler temperatures and they inhabit in the water with low silicates. Thus, they are only found in places where the requisite temperature, abundance of light and clear water are found. Morphology of Platforms The carbonate ramps are found in the tropical as well as the temperate belts where the size and type of grain vary with the relative distance from the shore. They are subdivided into two different types depending upon their slopes. The homoclinal ramps belong to the category of ramps with slow and gradual slopes (less than gradients), with no steep margins or slope breaks. These ramps are believed to be formed by mud producing organisms and there by developing fine grain gradual ramps. The other type of ramps is called as distally steep ramps which are marked with slope breaks and steep margins. The gradient of distally steep ramps is significantly slower than then the flat topped platforms (FTP). They are marked with non uniform slope breaks and coarse grained deposits. Rimmed carbonate shelves are the flat topped carbonate platforms which are characterised with flat tops and are shallow (0-30 m). They have found as narrow deposits with a distinct and sharp slope breaks where the gradient can be greater than .near the shore line. The shallow water frame building organisms which leave the skeletal deposits, may lead to the formation of reefs, which may resist the flow of water into the back reef area leading to the formation of lagoons. These are only found in the tropical regions as the reef forming biota requires warm climates and light. Figure 1: The Morphology of carbonate platforms. Figure shows the different platforms form the structural view. The rimmed margin shelves are characterised with shallow (less than 10 m depth) and high energy wave resistant build ups formed by frame building biota and sedimentation. These structures are compared with bucket fill model with the rim made of hard skeletal organic material while the inside deposits being soft and made of sand. Even though the composition of the rim and the interior are of different compositions, the growth of both of them is dependent on the potential of rim for growth. Another model of development of rimmed shelves suggests that they are built by the progradation of reef and filling material seaward form the interior rather than from the sea platform lagoon ward transportation of materials. It has been suggested that this model of platform development would be applicable to the growth of other platforms. In case of the non-rimmed carbonate shelves there is no break of slope as found in the previous one. This leads to the little protection of the platforms from the waves. These platforms consist of gravel size deposits and the micro-organisms hardly need light or warm temperatures. Thus they are found in both the temperate and the tropical regions. The carbonate platforms are home to the rich reservoirs of hydrocarbons and thus their evolution and formation are of special interests for research. The different carbonate platforms have different geometry, facie, porosity and permeability which results into the differences in the distribution of the reservoirs. The benthic skeletal production of carbonate components is of high importance to the carbonate platforms. However, the open sea or the shallow water production also forms a significant part. The presence of light for the photosynthesis in autotrophic, mixotrophic or heterotrophic organisms is important as the production of carbonates happens mostly in the water at a depth of less than 10 m, below those water levels the production decreases significantly due to unavailability of light. Development Evolution The carbonate producing biota is divided into three major sub groups depending on the light conditions required by them to grow. The first group belong to the autotrophs and mixotrophs which groups which require abundance of light and therefore occupy the shallow water with penetration of light greater than 0.1%. These are known as the euphotic biota. The next group belongs to those autotrophs and mixotrophs which require lesser light penetration (0.001% to 0.1%) and less temperature and are known as Oligophotic biota. The last group belongs to the groups which are photo independent and are found in waters with lesser light penetration (less than 0.001%). They are mostly dependent on the availability of food in the region for their growth. There are other factors like salinity of water, availability of phytoplankton, water movement, the resistance posed by the platforms to the water waves. Figure 2: Distribution of biota along the carbonate platforms Based on the type of biota producing carbonate deposits, there has been proposed different production medium or factories. The tropical carbonate producing, shallow water euphotic, biota produces the rimmed shelves. The heterotrophic cool water skeleton producing biota produce the non-rimmed carbonate shelves. The light independent biota consists of mud producing microorganisms which develop the ramp carbonate platforms. The carbonate producing factories are developed through the intrinsic factors like presence of micro organisms and the factors leading to their growth (light availability, temperature, water turbulence, salinity, availability of food etc.) and extrinsic factors like the climate and water conditions. Once developed the carbonate platforms are affected by the wind and water activity like waves, tides, ocean currents etc. Thus it is the hydraulic regime which controls the growth and transport of the material between centre and margins of carbonate platforms. The relativ e rise or fall of the sea level and the rate and style of the subsidence determine the development of carbonate platforms. Suppose the relative sea level subsides the carbonate platform above water would start to degrade and erode. Platform Drowning The carbonate platform digenesis and geometry of the facie are dependent on the composition of the sediment and biota which cause the precipitation of carbonate skeletal. Along with these factors it is also influenced on platform scale by long term factors like platform subsidence and drowning. Figure 3: Carbonate production profiles with T: Tropical factory, M=mud factory and C: temperate factory The relative change in the sea level with respect to the carbonate platforms is one of the factors controlling evolution. This is because the production of the carbonates is dependent on light and temperature. The maximum production occurs in the level up to 10 m and decreases thereafter. Throughout the globe there have been changes in the sea level, which is the result of the eustatic changes, sedimentation process and the tectonic movements has happened cyclically throughout he periods. The lifecycle of carbonate platforms range from five to several tens of million years, which is same as the third order sea level cycles. The response of carbonate platforms relative to the sea level changes has been outlined by Moore through the evolution period. The response of the carbonate platforms with relative sea level changes occurs in three different phases after exposure. The first phase is the start up phase where the carbonate sedimentation lags the relative sea level rise. The next phase is called catch up phase when the carbonate sedimentation builds faster than the sea level rise. The third and last phase is the keep up phase where the carbonate sedimentation closely matches the relative sea level changes and the top or crest of the sedimentation is close to the sea l evel. During the first phase start up there is high level growth of the carbonate platform leading to the development of ramp. The high energy currents moves from the shoreline o the centre and here are no developed margins to the ramps which are bathymetrically controlled. The carbonate platform accumulates during the catch up phase when the rise of sea level slows down leading to the growth of vertical stack. The ramp develops into rimmed shelves due to the high production of carbonate. In the next phase the carbonate platform growth is limited along the vertical stack, while the lateral development or evolution of the ramp may happen. The platforms drowned below the sea levels are not morphologically different from the platforms discussed in the previous sections. They comprise of the similar structures like drowned ramps or rimmed shelves. They undergo through the period of evolution and a possibly change in the sea level or the tectonic movement which might have resulted into platform subsidence. The Pacific Ocean and the Indian Ocean are common with the examples of the isolated drowned platforms and atolls, subsided, following the ceased volcanic activity, below the reach of light. This leads to the cessation of the growth of carbonate forming biota and hence the platform growth. Figure 4: The Carbonate platform shaping up due to the relative sea-level changes and the response of the carbonate producing factories The Blake plateau which was drowned during the Holocene and Cretaceous period is currently more than 2000 m deep under sea level. The platform is rich in pelagic, ferrous and manganese deposits which are characteristic of cretaceous period. The Holocene St Croix Island are beginning to drown are formed with coral reefs (W. H. Adey 1976). The Pourtales Terrace (East of Florida), characteristic of Pleistocene period, is about 150 m to 300 m deep. It is rich in algal and pelagic growth. The Miami Terrace which was drowned during the Miocene period, evolved with the growth of the basin during the early Miocene period. The terrace was exposed due to the fall of the sea level during the late Miocene period which was subsequently drowned later. It is endowed with pelagic and phosphorite sediments. The vertical growth of the carbonate platform is approximated to be 100 cm per thousand years which exceed far from the changes in relative and eustatic sea level changes. The platforms drowned as the result of the sea level changes present as a paradox in itself as the rate of sea level rise in the second or third order of eustatic changes is less in magnitude compared with the healthy rise in level of carbonate platforms. According to Schlager, the eustatic changes in the sea level or subsidence could outpace the vertical growth of carbonate accumulation only in case of sudden change in extrinsic factors like the change in the fault lines can lead to the sudden subsidence of the platform. The sudden influx of water due to melting of glaciers can also lead to the change in sea level. Other factors like the change in the salinity, temperature, water turbulence, depletion of the nutrients, rise of silicates in water, change in the photic levels of sea water can also lead to the sudden decrease or death of the underwater organisms. It has been pointed out there may not be a singular factor responsible for the drowning of the carbonate platforms but there may be a combination of two more factors. Schlager has pointed out that to contain the growth of reef forming biological growth, the factors should appear in brief periods and should repeat themselves at regular intervals, once in period less than a million years. Architectures of Drowned Platforms Even though there may be a multiplicity of reasons for drowning of the platforms, the major role is played by the interactions between the change of relative or eustatic sea level and growth of the carbonate factory. The different rates of sea level changes have a different level of impact and responses of the carbonate factory change accordingly. The carbonate platform may shift basin ward (prograde), stack on vertically (aggrade), step back (retrograde) or step down. These responses can be traced back to the changes in eustatic or relative sea level changes. The responses are of importance to predict the changes in the platform. Figure 5: The phases of evolution and drowning of the carbonate factories The carbonate platforms which have drowned in the recent past are results of the sea level rise exceeding the potential growth of the platform. However, it has not been enough to stop the production of the carbonate factory. These carbonate platforms are above the sea level along the rimmed side but are under water towards the shoreline (lagoon wards).The platforms subsidence which have been caused by the movement of the tectonic plates are more susceptible to drowning of the entire platform. These subsided platforms may recover with the cycles of rise and fall of the relative sea level. The carbonate ramp platform of Barbados is currently around 100 m below the sea level. The Mayotte drowned platform is mostly drowned while only a part of it, drowned in the Holocene period, has the continued growth of reefs. The carbonate platforms may respond to the relative rise in the sea level, in case the rise is no rapid with respect to the growth of reef, by retreating or back stepping. The retreating is rare while the back stepping can be seen in the rimmed shelves. The back stepping can be advantageous to the reef growth, as the platform recedes to the shallower water. This reduces the platform width basin wards while the high growth potential of the carbonate factory is resumes equilibrium with respect to the rise in the sea level. Another advantage of the back stepped platform is the reduced destructive forces of high energy sea waves. The energy of the high energy waves is dissipated with friction with the bottom towards the platform or the shoreline. The back stepping saves the platform from the subsidence towards the higher topography. This again saves the platform from subsiding along the fault lines. The back stepping creates a step like structure of the platform. Figure 6: Incipiently drowned carbonate platforms The back stepping of the rimmed carbonate platform happens faster than the lagoon. In case the rim drowns under the sea level there are lesser chances to recover the platform. The back stepped platform would lead to higher growth of the reef in the equilibrium period, while the fall of the sea level in the ensuing period may lead to basin ward growth of the platform. The cycle of back stepping and basin ward growth leads to development of step like morphology. Tools for Measuring Drowning Characteristics As the platform evolves through growth and drowning, it interacts with the environment which leaves a mark on the topography. During the growth phase the platform may prograde or aggrade accumulating the sediments along the basin or vertical stack. The platform may subside during the phase of eustatic change of the sea level leading to the retrograde and back stepping of the platform. The platform may get exposed to the air due to the relative fall of the sea level and undergo through erosion, decay of reef and diagenesis. Each of evolution passes leaves its own signature. These signatures are helpful in tracking the history of evolution and reservoir of resources. These tools include: 1. Taphonomic signatures: These are associated with the analysis of the history of the organic accumulation in the platforms, including the skeletal material. These are mainly related to the understanding of Taphonomic and diagenesis of the reef material under the sea level. 2. Diagenesis Signatures: It involves with the study of the physical and chemical nature of the deposits. Bibliography Acker, K.L. and Risk, M.J. Substrate destruction and sediment production by the boring sponge Cliona caribbaea on Grand Cayman Island. Journal of Sedimentary, 1985: 705-711. Adams, A. E. and Mackenzie, W. S. A Colour Atlas of Carbonate Sediments and Rocks Under the Microscope. Manson Publishing, London, 1998: 180. Adey, W. H. and Burke, R. Holocene bioherms (algal ridges and bank barrier reefs) of eastern Caribbean. Geological Society of America Bulletin, 1976: 95-106. Adey, W.H. Crustose coralline algae as microenvironmental indicators in the Tertiary. Historical Biogeography, Plate Tectonics and the Changing Environment., 1979: 459-464. Ahr, W. M. The carbonate ramp - an alternative to the shelf model. Transactions of the Gulf Coast Association Geological Society, 1973: 221-225. Aissaoui, D.M., Buigues, D., Purser, B.H. Model of reef diagenesis: Mururoa Atoll,French Polynesia. Schroeder J. H. and Purser B. H. (Eds.) Reef Diagenesis, 1986: 27-52. Alexandersson, E.T. Micritization of carbonate particles: process of precipitation and dissolution in modern shallow- marine sediments. Universitet Uppsala, Geologiska, 1972: 201-236. Allaby, A. and Allaby, M. A Dictionary of Earth Sciences. Oxford University Press, 1999. Aurell, M., Ba Denas, B., Bosence, D.W.J., Waltham, D.A. Carbonate production and offshore transport on a Late Jurassic carbonate ramp (Kimmeridgian, Iberian basin,NE Spain): evidence from outcrops and computer modeling. Carbonate Ramps: The Geological Society of London, Special Publication, 1998: 137-161. Bak, R. The growth of coral colonies and the importance of crustose coralline algae and burrowing sponges in relation with carbonate accumulation. Netherlands Journal of Sea Research 10, 1976: 285-337. Baker, P.A., Gieskes, J.M., Elderfield, H. Diagenesis of carbonates in deep-sea sediments: evidence from Sr/Ca ratios and interstitial dissolved Sr. Journal of Sedimentary Petrology, 1982: 71-82. Bathurst, R. G. C. Boring algae, micrite envelopes and lithification of molluscan biosparites. Journal of Geology , 1966: 15-32. Berger, A. and Loutre, M.F. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews, 1991: 297-317. C., Bathurst R. G. Carbonate Sediments and their Diagenesis. Developments in Sedimentology, 1975: 658. Ciarapica, G. and Passeri, L. An overview of the Maldivian coral reefs in Felidu and North Mal atolls (Indian Ocean): platform drowning by ecological crises. Facies, 1997: 33-6. Logan, B. W., Harding, J.L. Ahr, W.M., Williams J.C., Snead, R.G. Late Quaternary carbonate sediment in Yucatan Shelf, Mexico. Carbonate Sediments and Reefs. The American Association of Petroleum Geologists Memoirs, 1969: 5-128. Moore, C. H. Porosity Evolution and Diagenesis in a Sequence Stratigraphic Framework. Developments in Sedimentology, 2001: 444. Nash, M.C., Opdyke, B.N., Zhongwei, W., Huifang., X., Trafford, J.M. Simple X-Ray Diffraction Techniques to Identify Mg Calcite, Dolomite, and Magnesite In Tropical Coralline Algae and Assess Peak Asymmetry. Journal of Sedimentary Research 1084-1098. Pigott, J.D. and Land, L.S. Interstitial water chemistry of Jamaican reef sediments:sulfate reduction and submarine cementation. Marine Chemsitry, 1986: 335-378. Read, J.F. Phanerozoic carbonate ramps from greenhouse, transitional and icehouse worlds: clues from field and modeling studies. Carbonate Ramps. Geological Society of London Special Publications , 1998: 107-135. Schlager, W. Carbonate sedimentology and sequence stratigraphy. SEPM Special Publications, 2005: 174. Taft, W.H., Arrington, F., Haimovitz, A., MacDonald, C., Woolheater, C. Lithification of modern carbonate sediments at Yellow Bank, Bahamas. Bulletin of Marine Sciences, Gulf and Caribbean , 1968: 762 - 878. Tucker, M. E. Shallow marine carbonate facies and facies models. Recent Developments and Applied Aspects. P. J. Brenchley and B. P. J. Williams, SpecialPublications of the Geological Society of London., 1985: 139-161. Vail, P. R., Mitchum, R. M., Todd, R. G., Widmier, J. M., Thompson, S., Sangree, J. B., Bubb, J. N., Hatlelid, W. G. Seismic stratigraphy and global changes of sea level. Seismic stratigraphy - applications to hydrocarbon exploration American Association of Petroleum Geologists Memoir, 1977: 49-212. Vaughan, T.W. The results of investigations of the ecology of the Floridian and Bahamian shoal-water corals. Proceedings of the National Academy of Science, 1916: 95-100. Vogel, K., Gektidis, M., Golubic, S., Kiene, W., Radtke, G. Experimental studies on microbial bioerosion at Lee Stocking Island, Bahamas and One Tree Island, Great Barrier Reef, Australia. implications for paleoecological reconstructions. Lethaia, 2000: 190-204. W, Schlager. Sedimentation rates and growth potential of tropical, cool water and mud mound carbonate factories. Carbonate Platform Systems: components and interactions. Geological Society of London Special Publications , 2000: 217227. W., Schlager. Benthic carbonate factories of the Phanerozoic. International Journal of Earth Sciences, 2003: 445464. Webster, J.M. and Davies, P.J. Coral variation in two deep drill cores: significance for the Pleistocene development of the Great Barrier Reef. Sedimentary Geology, 2003: 6180.

Richard Wright Essays - Existentialists, Hollywood Blacklist

Richard Wright Throughout history, many talented authors writings have reflected the time period in which they lived in. Often the overall tone, and attitude of the novel is due to factors, that they have been born with, such as the environment they grew up in, who raised them, or moral ethics were instilled into their way of thinking. Richard Wright is an African-American author whose writings greatly reflected the time period in which he lived in. Native Son and Black Boy are two classic examples of Wright's works that are profoundly influenced by the era in which he lived. Wright was born on September 4, 1908, in Natchez, Mississippi on a small farm much in the same manner that his hero, Bigger Thomas, began his life. Deprived, poor, and segregated against, Wright spent much of his early childhood in pain, fear, and shame. He was repeatedly beaten by his mother and grandmother for trying to fight back at the segregation imposed upon him. He was also beaten by whites to whom he had to turn for jobs and he was resentful of the Jim Crow rules by which he had to live. In Black Boy, Wright's autobiography, he recalls a familiar childhood event: "I would feel hunger nudging my ribs, twisting my empty guts until they ached. I would grow dizzy and my vision would dim." In Black Boy, Wright used his own life to exemplify what qualities of imagination and intellect are necessary of a southern African-American in order to understand the meaning of his life in the United States. Black Boy also reveals it's 'author hero' as a man controlled by an absolute certainty of his own virtues. The ethics of living Jim Crow require that Wright be obedient and silent. So although he was not a slave, he in essence was. He shared the same emotions as the slaves and emphasized for them. Yet everything we know about his character has prepared us to expect rebellion. Wright could not, from his earliest years, tolerate this repression, and Black Boy is the chronicle of his segregation, not only from the white society but from with his own society. While Black Boy represents a picture of a personality corrupted by a brutal environment, it also presents natural human responses to its world by a sensitive child. The very fact that Black Boy is an autobiography of Wright's life is in itself exemplifying how his life was reflected in his works. Wright's life, especially his childhood apparently had a great impact on him, otherwise he would not have written a book about. Native Son, the novel that Wright is most noted for is also greatly reflected by the time in which he lived. Bigger Thomas, the hero and the protagonist of the novel, experiences escape which takes place within an urban maze that has come to be called black ghetto. In essence, Bigger's escape has been blocked, it is destined for failure even before it begins. Just like in Wright's life, he has grown up in a 'ghetto' of Mississippi, in a society in which he attempts to rebel but is condemned for doing so. Bigger Thomas, Wright's fictional character, is in some ways non-fictional, perhaps because Bigger's rebellious persona is what Wright strived to be although was unable to do to factors that he could simply not overcome. Bigger is an example of the black revolt against the injustices of the white asti system, and his revolt takes the form of crime against the white society. Born into a society that is white and hostile, (just as Wright was) Bigger becomes the total embodiment of that society's prejudices and hatreds against the black man. In a way Bigger Thomas is an autobiographical character because so much of what occurs in bigger's life, similarly occurred in Wright's. Thus we see that much of Richard Wright's works have been influenced by the time period in which he lived. Black Boy, Wright's autobiography is the perfect embodiment of just how great his life reflected his writings. Native Son, although a fictional book, in many ways still reflected Wright's life as a rebel. In Native Son, Wright could articulate himself, using Bigger Thomas as a fictional character to express the powerful spirit which tried to overcome the white society which oppressed him.