Blackberry Wine Review Essay Example

Blackberry Wine Review Paper Essay on Blackberry Wine The first sentence of the summary to this book I still alarming: Wine can work wonders and new worlds . Maybe its me so spoiled, but the association is extremely strange. Further annotations author tells about the writer, who had found six old wine bottles, vypivshem them and began to talk with the long-extinct eccentric old-gardener of his past. If you only knew how I was afraid of this description, that the images are born of my violent fantasy! But Joanne Harris apparently much better than me. Her book has left quite a different feel and aftertaste. Im still a little drunk it. In this book, there is a drop of magic. She bewitches. Shes really tasty and fragrant. It is not so fragrant, like Perfume, more like Dandelion Wine Bradbury. If you are expecting from her rapid developments raging passions, it is not for you. She, like a good wine, it should be enjoyed slowly, savoring every word. Smells in this book has everything, including the past. For a moment she thought she heard some kind of smell, strange living aroma of sugar and apples and blackberry jelly and smoke. The smell of nostalgia, and a moment she almost understood why Jay loves this place with its small vineyards, apple and goats that roam the swampy plains. For a moment she again became a little girl and grandmother baking cakes in the kitchen, and the wind from the sea sang in the telephone wires. Somehow, she knew that the smell of this part of it, the smell permeated him like chronic smoke. If you like, you like it, and the whole book. At the same time, it is entertaining. It is about th e search for self, friendship, miracles We will write a custom essay sample on Blackberry Wine Review specifically for you for only $16.38 $13.9/page Order now We will write a custom essay sample on Blackberry Wine Review specifically for you FOR ONLY $16.38 $13.9/page Hire Writer We will write a custom essay sample on Blackberry Wine Review specifically for you FOR ONLY $16.38 $13.9/page Hire Writer

How to Use a Hurricane Tracking Chart

How to Use a Hurricane Tracking Chart A popular activity during hurricane  season is to track the path and progress of tropical storms and hurricanes. Known as hurricane tracking, its a creative way to teach hurricane awareness, learn about storm intensities, and to create and keep your own hurricane records from season to season. Materials Needed: Access to the latest tropical storm and hurricane forecastsA hurricane tracking map/chartA pencilAn eraserColored pencils (blue, light blue, green, yellow, red, pink, magenta, purple, white)A ruler (not required) Getting Started: Monitor the National Hurricane Center for current tropical cyclone activity. Once an invest develops into a tropical depression, subtropical depression, or stronger, its time to start tracking it.Plot the storms first position.To do this, find its geographic coordinates (latitude and longitude). (The positive () number, or the one followed by the letter N, is latitude; the negative (-) number, or the one followed by the letter W, is longitude.) Once you have the coordinates, move your pencil along the right edge of the chart to locate the latitude. Using a ruler to guide your hand in a straight line, move your pencil across horizontally from this point until you find the longitude. Draw a very small circle at the point where the latitude and longitude meet.Label the storm by either writing its name next to the first plot point, or drawing a small box and writing the storm number inside.Continue to track the storm by plotting its position twice daily, at 12 UTC and 00 UTC. Dots repres enting the 00 UTC  position should be filled in. Dots representing the 12 UTC position should be left unfilled. Label each 12 UTC plot point with the calendar day (i.e., 7 for the 7th).Use the Hurricane Tracking Chart key (at the bottom of the page) and your colored pencils to connect the dots with the appropriate colors and/or patterns.When the storm dissipates, write its name or storm number (like in step #3 above) next to its final plot point.(Optional) You may also want to label the storms minimum pressure. (This tells where the storm was at its strongest.) Find the minimum pressure value and the date and time it occurred. Write this value next to the corresponding section of the storm track, then draw an arrow between them.Follow steps 1-8 for all storms forming during the season. If you miss a storm, visit one of these sites for past hurricane data: National Hurricane Center Tropical Cyclone Advisory ArchiveAn archive of advisories and storm summary information. (Click on the storm name, then choose the 00 and 12 UTC public advisories. Storm location and wind speed/intensity will be listed under the summary section at top of the page.) Unisys Weather Tropical Advisory Archive 404An archive of tropical cyclone products, advisories, and bulletins from season years 2005-present. (Scroll through the index to choose the desired date and time. Click on the corresponding file link.) Need an Example? To see a finished map with storms already plotted, check out the NHCs Past Track Seasonal Maps. Hurricane Tracking Chart Key Line Color Storm Type Pressure (mb) Wind (mph) Wind (knots) Blue Subtropical Depression 38 or less 33 or less Light Blue Subtropical Storm 39-73 34-63 Green Tropical Depression (TD) 38 or less 33 or less Yellow Tropical Storm (TS) 980 + 39-73 34-63 Red Hurricane (Cat 1) 980 or less 74-95 64-82 Pink Hurricane (Cat 2) 965-980 96-110 83-95 Magenta Major Hurricane (Cat 3) 945-965 111-129 96-112 Purple Major Hurricane (Cat 4) 920-945 130-156 113-136 White Major Hurricane (Cat 5) 920 or less 157 + 137 + Green dashed (- - -) Wave/Low/Disturbance Black hatched (+++) Extratropical Cyclone

Childhood Protection and Child Rights; Lex ferenda; Breaking the Cycle Essay

Childhood Protection and Child Rights; Lex ferenda; Breaking the Cycle of Violence within the Child Phd Thesis - Essay Example According to the World Health Organization (WHO), there is no one "official" definition of mental health. To define Mental Health academicians rely on various theories from cultural differences, subjective assessments, and competing professional.1 This research project has sought its backing in principles of child psychology. By matching and comparing the definition of a â€Å"child† in law and psychology, one realise the emerging truth of a lack of understanding in law-making, judiciary and legal pronouncements as to concepts, such as child vulnerability, child needs, and child resilience. In concrete words, what changes for a child who has been victim of sexual violence? What changes for a child who is working day and night in a factory? What changes for a child who is living on the streets? What changes for a child arrested? What changes for a child beaten up by police? Well, the first and foremost change is at the level of mental health. The way she thinks, the way she fee ls. Mental health of children is an important aspect of child-right study discourse. Through the understanding, one can assure the child is able to ‘bounce back’ and recover from a difficult situation. What is important to realise is that the mental health promotion dealt with in this research is actually a promotion and prevention in the aftermath of a severe incident or process, in the child’s life. These are the promotion of a child’s special needs, and the prevention of long-term violent impacts on the society. The later chapters deal with the reactions and risks of un-dealt trauma, and societal progress linked to the wellbeing of its children. The research study does not per se differentiate between categories of children. The categories presented here are neither exhaustive nor exclusive. Mostly vulnerable children fall into many of the categories. For instance, street children can also be child labourers, and sexually abused. My

Assignment for Art Humanities class Example | Topics and Well Written Essays - 750 words

For Art Humanities class - Assignment Example Other images show kissing between married people as unclean, even when legalized by the matrimony. Though kissing can have other meanings, such as the kiss of peace and the mythical kiss, the Church related kissing to immorality because of its physical gratification aspect. The author presents a compelling argument regarding the treatment of desire in the medieval times. His use of descriptive language specifically helped understand the meaning of kissing images in art and literature. His analyses offer insight on how the Church used the dichotomy between right/wrong, and spirit/body, to further divide the male and female gender and ascribe inferiority to the latter. Thus, kissing has been connected to sin, where the female sex invokes sin among men. This shows that women were characterized as temptresses, whose whorish abilities must be controlled and fought. The Production of the Orient in Said’s â€Å"Orientalism† In â€Å"Orientalism,† Said argues that the Or ient is a product of European imagination and demand for domination through imperialism. He stresses that Europe gains from defining the Orient as â€Å"the Other† because it justifies its control over its people and resources. Furthermore, when Said talks of Orientalist discourse, he pertains to socio-economic and political institutions that reinforce Eurocentricism. Orientalist discourse is not about the Orient as its natives believe it to be, but how Britain, France, and America want to see and discuss the Orient. The difference between what is and what the powers want something to be is related to Camille’s analysis of the Kiss. The Church thinks that the Kiss is inherently evil because of its sexual consequences. In the same line of thinking, Said sees Orientalism as man-made, specifically, produced by imperialist rulers. They manufactured Orientalism for their own purposes, in the same way that the Church generates images of the kiss for its own intentions. The C hurch and the white empires both want to control people through their literature and arts. They similarly impose their will on the powerless, so that the former can maintain and expand their powers. Like Camille, Said performs a visual analysis on Orientalist literature. These images indicate the loss of the Orient to the much more powerful and superior West. Thus, Said argues that the West did not only control the Orient through its political structures, but more so, through shaping its cultural norms and symbols. Not Fury, but Calmness in Freud’s â€Å"The Moses of Michelangelo† In Totem, Taboo, and other Works, Freud interprets the Moses statue of Michelangelo in his essay, â€Å"The Moses of Michelangelo.† He disregards common artistic interpretations that Moses is about to spring into action and the tablets are almost slipping from his left hand. Instead, he believes more in the analysis of Thode, that by virtue of Moses’s position in an array of scu lptures and the actual muscle tensions in his body, Moses is in a state of perpetual wrath, but not ready to perform any immediate action. Freud thinks that Moses is not preserved for a historical event, but as a character whose experiences have aroused inner feelings of anger and

Relationship(s) between leadership and management 311 Essay

Relationship(s) between leadership and management 311 - Essay Example On the other hand, with the rapid growth of the business sector and constant changes in the nature of markets, the theories, concepts and practices of leadership and management have also evolved (Baker and Desjardins, 2013). Relating to these changes, this essay focuses on analyzing the contribution and use of leadership and managerial concepts in ensuring sustainable business practices and growth. As stated by Brown, Trevià ±o and Harrison (2008), selection of the managerial process in a business is dependent upon the style of leadership being applied. On the other hand, Bogardus (2009) mentioned that the management practices of a firm define the leadership styles that can be implemented. Both of these notions can be analyzed in an in-depth manner by reflecting their characteristics and objectives of utilization. As highlighted by Morgan (2009), the key objective of management is to enhance that the aims of the organization can be fulfilled while leadership establishes the mission and vision that provides direction to a company. Supporting this notion, Kim and Brymer (2011) further added that as an organization is structured and the work culture is established, the style of leadership among the various operational variables of the business differ. In the business sector, this sort of alignment between leadership and management can be often observed. As an evidence for the above stated concept of alignment of leadership and management, the managerial process of Google Plc can be taken into consideration. The mission of Google is to help in spreading knowledge by innovating new platforms for sharing information all over the world (Day, Harrison and Halpin, 2012). Based on this mission, the managerial and leadership aspects of the company are developed. Lunenburg (2011) highlighted that Google being a technology firm depends on innovation and thus have created a participative managerial and leadership culture

Subsurface Layer Characterisation Research

Subsurface Layer Characterisation Research SUBSURFACE LAYER CHARACTERISATION FOR ENGINEERING PURPOSES USING VERTICAL ELECTRICAL SOUNDING IN BANANA ISLAND, LAGOS, NIGERIA OLADUNJOYE, H.T., 2OLALEYE, A.O. ABSTRACT Seven (7) vertical electrical sounding stations along two traverses were used to study the depth to competent formation for foundation of engineering structures in Banana Island of Lagos. The study is meant to unravel the presence of problem soils that can be inimical to structures.   The sounding data used in this study was acquired using Schlumberger Electrode Configuration. The VES data were interpreted into a model curve using forward modelling software called Winglink. The interpretation parameters (layer resistivities and thicknesses) for each VES point were grouped into three geo-electric sections to represent the 2-D models of the subsurface layers in the study area. The final interpretation results (resistivities and depths) modelled as geoelectrical sections and pseudosections were compared within the surveyed area and correlated with the borehole log-derived depths to determine a probable depth for foundations of high rise building. The study concluded that the geophysical investigation is of great significance in partial curve matching interpretation technique gives the most consistently low percentage deviation error margins amongst the three VES preliminary interpretation techniques. There is consistent increase in depth prediction error, with depth, in all the interpretation techniques. INTRODUCTION Geophysical resistivity techniques are based on the response of the earth to the flow of electrical current. In all methods, an electrical current is passed through the ground and the resulting potential electrodes allow us to record the resultant potential difference between the current electrode is measured. The apparent resistivity is then a function of the measured impedance (ratio of potential to current) and the geometry of the electrode array. Depending upon the survey geometry, the apparent resistivity data are plotted as 1-D soundings, 1-D profiles, or in 2- D cross-sections in order to look for anomalous regions. In the shallow subsurface, the presence of water controls much of the conductivity variation. Measurement of resistivity (inverse of conductivity) is, in general, a measure of water saturation and connectivity of pore space. This is because water has a low resistivity and electric current will follow the path of least resistance. Increasing saturation, increasing salinity of the underground water, increasing porosity of rock (water-filled voids) and increasing number of fractures (water-filled) all tend to decrease measured resistivity. Resistivity measurements are associated with varying depths depending on the separation of the current and potential electrodes in the survey, and can be interpreted in terms of a lithologic and/or geohydrologic model of the subsurface. The choice for Direct Current (DC) resistivity survey in this project is as a result of its ability to provide a quick synoptic picture of lithological and groundwater characteristics in terms of its apparent resistivity contrast. In this work the electrical resistivity character collected were model with Winresist and Winglink inversion software. The layers parameters (resistivities and thicknesses) obtained from data processing were then inverted with Winglink to provide two-dimensional images of the subsurface apparent resistivity variation (Pseudosection). However, knowledge on the geology of the area from acquired borehole log has played a vital role in determining the best fit model. MATERIALS AND METHOD OF STUDY The vertical electrical resistivity is used to determine the subsurface resistivity distribution and depth of the sub-surface layers with the aid of electrical resistivity meter. In this study, Schlumberger array of electrical resistivity method was adopted because of the low cost of the field operation, reduced logistics man power and also faster. A total of Six (6) vertical electrical sounding (VES) were measured within the area. The resistivity measurement is taken by introducing small portion of electricity through two current electrodes (A and B) and measuring the resultant voltage drop between a pair of potential electrodes (M and N). A simple calculated value of apparent resistivity is the parameter bearing the information for the characteristics of the subsoil (Tonkov, 2008). From the foundation of electrical resistivity theory is the ohms law (Grant and West, 1965; Dobrin and Sarvit, 1988):            Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚   (1) Where Ï  is the resistivity, R is the resistance, L is the length of the conducting cylinder and A is the cross sectional area. For the solid earth, whose material is predominantly made up of silicates and basically non conductors, the presence of water in the pore space of the soil and in the rocks fractures enhances the conductivity of the earth when an electrical current I is passed through it, thus making the rocks a semi conductor.   Since the earth is not like a straight wire and it is not an anisotropic, then Equation 1 can be customized as:   Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚   (2) Where change in voltage and r is is the radius of current electrodes hemisphere. Since the earth is not homogeneous, Equation 2 is used to define an apparent resistivity which is computed as the product of the geometric factor and the resistance recorded in the electrical resistivity meter and resistivity the earth would have if it were homogeneous (Grant and West, 1965;):   Ã‚  Ã‚  Ã‚     Ã‚  Ã‚     Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚  Ã‚   (3) Where, 2Ï€r is then define as the geometric factor (G) fixed for a given electrode configuration and is dependent on the electrode arrangement. The Schlumberger electrode configuration was used for this study. The geometric factor is thus given as:   Ã‚  Ã‚   (4) Where AB is the distance between two current electrodes, MN is the distance between two potential electrodes. LOCATION AND GEOLOGY OF THE STUDY AREA The study area is located in the south-eastern part of Lagos State between Latitudes 6 ° 25 to 6 ° 28 North of the Equator and Longitudes 3 ° 24 to 3 ° 30 East of the Greenwich Meridian (Fig.1.1). The study area Lekki and its environ issituated within the western Nigeria coastal creeks and lagoon developed by barrier beaches associated with sand deposition (Pugh, 1954). It forms part of the Lagos lagoon system known as the largest of the four lagoon system in the gulf of guinea coast (Adepelumi and Olorunfemi, 2000). Banana Island is an artificial island in Lagos State, Nigeria. It is located in the Lagos Lagoon and attached to the North-Eastern Ikoyi Island by a dedicated road strip which is linked to the existing road network. The banana-shaped Island is approximately 1,630,000 square metres in size (less than a square mile) and is divided into 536 plots (of between 1000 and 4000 square metres in size) mainly arranged along cul-de-sacs, so designed to enhance the historically residential nature of Ikoyi. Banana Island is an artificial island reclaimed from portions of the Lagos Lagoon, topographic elevation obtained at the site averaged 4 metres above mean sea level. The study area is located within the coastal region of Nigeria with a climate of long wet season (April to October) and short dry season (November to March). Average annual precipitation is above 2000mm and serves as a source of groundwater recharge. The area is susceptible to flooding after heavy rainfall during the wet season. Nigeria lies in an extensive Pan-African mobile belt which separates the West African and Congo Cratons. The belt is interpreted to have evolved from the continental collision between the West African craton and the Pan-African belt (Black et al., 1979; Caby et al., 1981). Geochronologically, the Precambrian rocks of Nigeria can be grouped into four major classes (Liberian Orogeny 2800  ± 200 Ma, Eburnean Orogeny 2000  ± 200 Ma, Kibaran Orogeny 1100  ± 200 Ma and The Pan-African Orogeny 600  ± 150 Ma). These classes correspond with the four orogenic events that have punctuated the Precambrian history of Africa (Odeyemi, 1979). Figure 2.1: Regional Geological Map of Nigeria (Modified after Ajibade et al., 1988) Coastal Nigeria comprises two sedimentary basins: The Benin-Dahomey basin and the Niger Delta basin separated by the Okitipupa ridge. The rocks of the Benin basin are mainly sands and shales with some limestone which thicken towards the west and the coast as well as down dips to the coast. Recent sediments are underlain by the Coastal Plains Sands which is then underlain by a thick clay layer the Ilaro Formation and other older Formations (Jones and Hockey, 1964). The Coastal Plains Sands aquifer is a multi-aquifer system consisting of three aquifer horizons separated by silty or clayey layers (Longe et al., 1987). It is the main aquifer in Lagos Metropolis that is exploited through boreholes for domestic and industrial water supply. The sedimentary rocks of Lagos State are composed of five (5) sedimentary formations (Jones and Hockey, 1964) viz: Abeokuta Formation, Ewekoro Formation, Ilaro Formation, the Coastal Plains Sands and the alluvial deposits. The coastal plains sand also known as the Benin Formation stretches across the Dahomey basin into the Niger Delta Basin. The geological formations of the study area composed of sediments laid down under fluviate, lascustrine and marine environments. These sediments grade into one another and vary widely in lateral extent and thickness (Adepelumi and Olorunfemi 2000). Longe et al., (1987) classified the aquifer into three types. Quantitative interpretation of the curves involved partial curve matching using two-layer Schlumberger master curves and the auxiliary K, Q, A and H curves. Output from the quantitative interpretation was modelled using computer iteration. The Resist Version 1.0 interpretation software was used for iteration and presentation of the curves (see Figures 3a f). RESULTS AND DISCUSSIONS The apparent resistivities from the field plotted on a log-log graph survey against the corresponding half Schlumberger electrode spacing was interpreted using the computer iteration technique. The initial model was deriving by winresist software by entering layer parameters from partial curve process as the starting parameters. The resulting models were then iterated till the best fit curve as attained. In all, there was a large value for root mean square (r.m.s) error resulting mostly from the scattered point data observed where half Schlumberger electrode spacing is greater than 32m. In order to view the resistivity distribution of the whole surveyed area, the result of the soundings data linearly and vertically interpolated into two dimensional pseudosections. The borehole records from the geo-technical investigation were used as a control in interpreting the VES data acquired in this study. Interpretation of the geo-electric curves was essentially based on the fact that resistive materials constitutes zones of interest for engineering construction, considering that clay and organic materials are conductive and typified by low resistivity values(reference). The outputs from the manual interpretation were modelled using computer iterations. Resist Version 1.0 software was utilized for the iterations. The curve types obtained are 3 layer H (VES 1), 4 layer QH (VES 2, VES 3 and VES 6) and 5 layer QHK (VES 4 and VES 5), as shown in Figures 3a f. VES 1 and VES 6 with RMS-error (Root Mean Square) of 11.7 and 10.4 respectively present better quality data than VES 2 to VES 5 with RMS-error ranging from 12.7 to 20.8, thus the interpretation of the geo-electric curves at VES 1 and VES 6, present more reliable results. From the iteration of VES 1, depth to competent bedrock (sand) is 39.6 metres, while depth to competent (sand) layer at VES 6 is 39.8 metres, this is signified by the rising segment of the curve at both VES stations, typified by a relatively resistive material (5 105 à ¢Ã¢â‚¬Å¾Ã‚ ¦-m). CONCLUSION This paper describes the possibility of locating a competent formation for high rise building in area around Banana Island Ikoyi using Schlumberger array. The results of the interpretation of field survey reveal only the presence such formation in depth close to 10m. At this depth saturated sandy clay can be obtain virtually for all the VES stations. This saturated sandy clay formation provides good foundation support for any high rise due to the fact that the liquefaction potential is very low compare to all other formation inferred from geologic section. REFERENCE Alile, M.O., S.I. Jegede and O.M. Ehigiator, 2008. Underground water exploration using electrical resistivity method in Edo State, Nigeria. Asian J. Earth Sci., 1: 38-42. Anderson, N. L. Selection of Appropriate Geophysical Techniques: A Generalized Protocol Based on Engineering Objectives and Site Characteristics. Proc., 2006 Highway Geophysics- NDE Conference, 2006, pp. 29-47. Available at http://2006geophysics.mst.edu/. Anderson, N. L., A. M. Ismail, and T. Thitimakorn. Ground-Penetrating Radar: A Tool for Monitoring Bridge Scour. Environmental and Engineering Geoscience, Vol. 13, 2007, pp. 1-10. Dobrin, M.B. and C.H. Savit, 1988. Introduction to Geophysical Prospecting. 4th Edn., McGraw Hill Book Co., New York. Dogara, M.D., B.M. Dewu and C.O. Ajayi, 1998. Groundwater potential of Romi, Kaduna. Nig. J. Physics., 10: 85-90. Grant, F.S. and G.F., West, 1965. Interpretation Theory in Applied Geophysics. McGraw-Hill, New York. Nwankwo L.I., P.I. Olasehinde and E.B. Babatunde, 2004. The use of electrical resistivity pseudo-section in elucidating the geology of an east-west profile in the basement complex terrain of Ilorin, West-Central Nigeria. Nig. J. Pure Applied Sci., 19: 1672-1682. Olasehinde, P.I., 1999. An integrated geological and geophysical exploration for groundwater in the basement complex of west central Nigeria. Water Resourses, 10: 46-49. Olasehinde, P.I., A.E. Annor and P.C. Pal, 1986. A geological evaluation of a prospective site for a weir on river Oyun, Ilorin, Nigeria. 7. Angew Geowiss, 8: 83-90. Olorunfemi, M.O and S.A. Fasoyi, 1993. Aquifer types and the geoelectric/hydrogeologic characteristics of part of the central basement terrain of Nigeria (Niger State). J. Afr. Earths Sci., 16: 309-317. Plummer, C.C., D. McGeory and D.H. Carlson, 1999. Physical Geology. 8th Edn., McGraw Hill Co. Inc., New York, pp: 48-56. Rabiu, A.B, I. A. Adimula, K. Yumoto, J. O. Adeniyi and G. Maeda, 2009. Preliminary results from the magnetic field measurements using MAGDAS at Ilorin, Nigeria. Earth Moon Planets, 104: 173-179. Rahaman, M.A., 1973. Review of the Basement Geology of South Western Nigeria. In: Geology of Nigeria, Kobe, C.A. (Ed.). 2 Edn., Rockview Publishers, Jos, Nigeria. Singh, K.K.K., A.K.S. Singh, K.B. Singh and A. Sinha, 2006. 2D resistivity imaging survey for siting water-supply tube wells in metamorphic terrains: A case study of CMRI campus, Dhanbad, India. The Leading Edge, 25: 1458-1460

We are the Plague, We are the Cure :: Exploratory Essays Research Papers

We are the Plague, We are the Cure Why is it that the fate of our nation seems to be in a downward spiral of despair? It seems as if everywhere you turn, you are greeted with grim visages of violence and misery. What is this plague which afflicts our society and has taken away the innocence and happiness of past generations? Our society is condemned to its current state due to its individualistic desires. If man is the downfall of himself, then is he also the plague of his society? You might believe that only recently with the advent of the Internet are we pushing ourselves too far, but this is far from the truth. This problem has hung as a spectre over society since its origin. In Genesis 3, we are first introduced to this plague on society. As Adam and Eve wandered the Garden of Eden, they were tricked by the serpent into eating from the Tree of Knowledge. After condemning all three for their disobedience God commented that, "the man has now become like one of us, knowing good and evil." (Genesis 3:22) This plague continues to today. If you think about it, we are all becoming increasingly dependent on technology. In a recent work by Bill Joy, this thought really hit home. To think that soon, "People won't be able to just turn the machines off, because they will be so dependent on them that turning them off would amount to suicide." This is what our dependence will cause, and this dependence is cause by our desire to push ourselves harder than is necessary. (Joy 2) As you can see this problem began when society did, and will not end until society does also. Technology and history are not the only fields in which society's plague are present, however. Recently, it seems as if every time you open the newspaper you are greeted with a declaration of 'breaking' news on the Presidential election. For hundreds of years, this process seemed so simple. Of course, there were times when society's little evil would spring up and try to do damage.