Hypocritical Christianity Exposed in Bernard Shaws Major Barbara Essay

Hypocritical Christianity Exposed in Bernard Shaws Major BarbaraBernard Shaw reveals in his plays a type of religious standard that is non unlike Christianity but with what most people see as a stereotypical view of hypocritical Christianity. Shaws concept of Crosstianity , as he calls it, shows a organized religion in which the church preaches what the rich and powerful tell it, scoundrels are treated as equals, and punishment is concerned with prosecution rather than salvation. Poetic justice rules juridical retribution rather than redemption. Everyone is inherently the same. The scene in Major Barbara in which Bill perambulator is dealt with for his attack on the shelter is revealing about the concepts of Crosstianity. Walker expects that he should be punished equally to his crime and even desires this to relieve his guilt. If Barbara had allowed him to pay for his abuse of Jenny and the old woman monetarily or physically, that would have been Crosstianity. He would have relea sed his guilt and gone on his way without any real change in his moral character. However, Barbara does not ...

The Western Lawman :: American America History

The Western Lawman The west was filled with various characters ranging from cowboys, bandits, bar owners, and ultimately the law. The different attitudes towards men of authority during the Hesperian era can be seen through the national radio show of Gun smoke. The sexual, caring, and just sheriff of Dodge County named Matt Dillon portrays many societal roles as he is faced with perplexing situations. Through three chronological successions of Gunskmoke, the reoccurring theme is that Matt Dillon is the law, the judge, and often the jury. The rise of the west needed a figure of authority and Matt Dillon was that symbol. He was the first person the lawbreakers saw and in any case the last they wanted to meet. Yeah, weve met Throughout the three episodes of Gunsmoke it can be seen that Dillon is a really knowledgeable person. When a towns person comes and informs Dillon regarding a certain situation, he normally knows who they are or someone related to him. Not only is he aware of whom they are but also their tendencies, whether they are humanitarian in nature or just a plain drunk. During the three episodes of Gunsmoke, Dillon was faced with solving cases in which a murder took place. Dillon knew those who were convolute as well as the likelihood of that same person committing the crime at hand. It can be seen through this fortuity that the western lawman is knowledgeable about his surroundings as well as the various possible suspects. Pope was a good man, he wouldnt do this In the first episode of Gunsmoke, Dillon speaks to a frightened resident who fears the invasion of Indians on his property. Dillon advises the man named Pope to acquire a gun and shoot if they came to close. When the Indians came, Pope shot one dead. notwithstanding Dillon found out that it wasnt Indians but rather a group of drunken men playing a practical joke. Through this story it is evident that Dillon was very compassionate to Pope by listening to his problem and advising him. Dillon was also kind and patient to the men who played the wrongful joke. It can be seen through this incident that the western lawman is caring and understanding. Im still the law in Dodge Dillon was also very just when it come to the law. The main theme of these three episodes was the depiction of Dillon playing the role of investigator, judge, jury and lawman.

Nuggets of Wisdom :: essays research papers

Nuggets of WisdomMy family and I often take vacations during the summer for relaxation, or to visit family, etcetera. On one such vacation, I learned a valuable lesson. Parents were created to teach their children little nuggets of common sense, but it is up to the children to listen.We were visiting the Central American country of Honduras. It was a bright, sunny, and hot summer day. Taking a break from sight seeing, and the heat, we took refuge in a tropical style restaurant for lunch. It was a two-story restaurant over the ocean. Along the walls, there were beautiful greenish foliage that plump, colorful flowers sprung from. Also, throughout the restaurant were wooden poles, painted blue, that hammocks were hung on.The waiter escorted my family and I to our table on the second floor. My parents sat at the table, but I chose a nearby hammock. The hammock was next to the open side of the restaurant. As I lay there, I began to study the ocean. I looked down and watched as the waves rippled, broke, and crashed to the shore. A salt-water smell permeated through the restaurant. A nearby fan oscillated fundament and forth, blowing a refreshing breeze across my face. All these elements caused me to relax, and slowly I began to sway in the hammock.Soon after I got in that comfortable position, the waiter delivered the meal. My parents had ordered fish, and had begun nibbling. Since I was not hungry, I only ordered a drink, which I took adventure to the hammock to sip on. I began to sway, much vigorously than before, and I closed my eyes to enjoy the sounds. My father looked up from his meal and watched as I swung back and forth. He raised an eyebrow, and with a glint of humorous, wisdom in his eyes my father said, David, that hammock is loose. Rock too hard, and you will go flying. Of course, I gainful him no attention. I was thirteen years old, and thirteen year olds know everything.Acting as a typical teenager, I began to swing once more despite my fathers wa rning. My head was in the clouds, as I watched the waves, and the birds. How could something go wrong when everything was so perfect? I did not notice the screak noise the rope made as its knot came lose. Nor did I realize what was happening when my drink hit the floor causing the glass to break with a deafening sound.

Ecommerce :: Essays Papers

Ecommerce The Internet has caught on like wild fire. No one ever intended for it to be so commercially successful. In the beginning, its main purpose was to send and receive messages no one anticipated that one-day people could buy books and cars over a computer. Though with the advancement of original technologies, this has happened. E-commerce is a worldwide commodity that has taken the place of trips to the supermarket and has given us the freedom to conduct business at out ho intent in our pajamas.To fully understand what e-commerce is, you must first understand where it came from. It all commencement exerciseed with the DOD (Department of Defense) in 1996. After the Cold War the Government wanted a reliable melodic line of communication. If a network link became damaged by enemy attack, the information on it could be rerouted automatically to other links. This was the birth of the Internet. In order to use anything on the Internet, it is required that you lear n to operate a separate program, one for the mail, one for news groups, and several different programs for accessing databases.This all changed in 1989. A police detective at CERN (a big European physics laboratory) named Tim Berners-Lee started to work on hypertext. By victimisation hypertext he could link together all the different kinds of information in stock(predicate) on the Internet.Berners-Lee called the software pack the World Wide Web.For the World Wide Web to work, each page has its own address that the web recognizes using a system called HTTP (Hypertext Transport Protocol). Each page has to be written with a special language called HTML (Hypertext Markup Language). This language tells the computer how to display a page. Now with the invention of the web, Businesses faeces use pictures to help sell their merchandise online, And now that the Internet is everywhere- in schools, libraries, and even cafes anyone can order just about anything from anywhere.It is no w easier than ever to have and start your own web page anyone form a big corporation or even the average joe can build his for her own web page. Just like Jeff Bezos, Time magazines Person of the Year of 1999. With a loan from the bank, Jeff founded Amazon.com in his garage and helped start e-commerce, as we now know it.

relationships :: essays research papers

The position of thrust rag weeks aroundthe margins of landslide walk forfends, and theirmorphology and direction of thrusting, suggests thatthey were formed as a proceeds of walk block pressure sensation and performance in the surrounding rachis. Toe-thrust sheets thus can be considered as the morphologicalexpression of ongoing instability at the landslidetoe. The upthrust nature of these sheets at WestRunton suggests that rotation of toe blocks,generating forward movement of the surrounding loosebeach gritstone, is the principal process of toe-thrustsheet formation (fig. 6). Passive crush of toeblocks into the surrounding common sense under gravity isunlikely to result in either brittle failure of thesand or differential movement of the sand away fromthe toe blocks (i.e., different thrust sheet widths).The presence of thrust sheets therefore suggests thatlandslide blocks are actively excavating into thesofter and unconsolidated beach sand that is displacedoutward as a re sult of this process. The size and extent of the thrust sheets can be usedas a proxy for the scale, rate, and timing of blockmovement. For example, the bigger landslide blocks areassociated with more extensive thrust sheets, andsheet width is likely associated with excavationdepth. The presence of aggregate and overlapping thrustsheets that digress in extent along the front oflandslide blocks (figs. 4, 5) also suggests thatdifferent parts of the toe are active at differenttimes and therefore that sliding rates and volumesaveraged across the entire landslide (Waltham andDixon 2000) likely conceal wide spatial and temporalvariations. Graphic omitted The presence of fragile toe-thrustsheets in spite of appearance the intertidal geographical zone at West Runton is ofinterest because these features are easily destroyedby waves and will be wiped out by every(prenominal) high soar upwards.Figure 6 is a schematic cartoon illustrating apossible formation mechanism for these features.Du ring high tides, the elevated position of the outer weewee plane (mean high weewee level) againstthe landslide toe means that there is a smalldifference in head, and low hydraulic potentialgradient, amongst the landslide toe and its externalenvironment (fig. 6a). The depth of marine wet alsolikely increases interstitial pore water pressure bothwithin the submerged beach sand and within thefine-grained landslide sediments and influenceseffective pressure (cf. Dixon and Bromhead 2002).Elevated external water pressure at high tide helps tohold back toe advance (Hutchinson 1988). At low tide, when the ground water table is locatedwithin the beach sand and is under impose (atmospheric)interstitial pore water pressure, a large differencein head and therefore steepened hydraulic potentialgradient exists between the landslide toe and theexternal environment (sea level) (fig. 6b). netherthese conditions, sliding and the formation ofrelationships essays research papers The position of thrust sheets aroundthe margins of landslide toe blocks, and theirmorphology and direction of thrusting, suggests thatthey were formed as a result of toe block pressing andmovement in the surrounding sand. Toe-thrust sheetstherefore can be considered as the morphologicalexpression of ongoing instability at the landslidetoe. The upthrust nature of these sheets at WestRunton suggests that rotation of toe blocks,generating forward movement of the surrounding loosebeach sand, is the principal process of toe-thrustsheet formation (fig. 6). Passive pressing of toeblocks into the surrounding sand under gravity isunlikely to result in either brittle failure of thesand or differential movement of the sand away fromthe toe blocks (i.e., different thrust sheet widths).The presence of thrust sheets therefore suggests thatlandslide blocks are actively excavating into thesofter and unconsolidated beach sand that is displacedoutward as a result of this process. The size and extent of the thrust s heets can be usedas a proxy for the scale, rate, and timing of blockmovement. For example, the bigger landslide blocks areassociated with more extensive thrust sheets, andsheet width is likely associated with excavationdepth. The presence of multiple and overlapping thrustsheets that vary in extent along the front oflandslide blocks (figs. 4, 5) also suggests thatdifferent parts of the toe are active at differenttimes and therefore that sliding rates and volumesaveraged across the entire landslide (Waltham andDixon 2000) likely conceal wide spatial and temporalvariations. Graphic omitted The presence of delicate toe-thrustsheets within the intertidal zone at West Runton is ofinterest because these features are easily destroyedby waves and will be wiped out by every high tide.Figure 6 is a schematic cartoon illustrating apossible formation mechanism for these features.During high tides, the elevated position of theexternal water plane (mean high water level) againstthe landslide toe means that there is a smalldifference in head, and low hydraulic potentialgradient, between the landslide toe and its externalenvironment (fig. 6a). The depth of marine water alsolikely increases interstitial pore water pressure bothwithin the submerged beach sand and within thefine-grained landslide sediments and influenceseffective pressure (cf. Dixon and Bromhead 2002).Elevated external water pressure at high tide helps tohold back toe advance (Hutchinson 1988). At low tide, when the ground water table is locatedwithin the beach sand and is under lower (atmospheric)interstitial pore water pressure, a large differencein head and therefore steepened hydraulic potentialgradient exists between the landslide toe and theexternal environment (sea level) (fig. 6b). Underthese conditions, sliding and the formation of

relationships :: essays research papers

The position of energy planing machines more than or lessthe margins of landslide walk blocks, and their sound structure and direction of thrusting, suggests thatthey were formed as a reply of toe block pressing andmovement in the environ sand. Toe-thrust sheets in that locationof can be considered as the morphologicalexpression of ongoing instability at the landslidetoe. The upthrust nature of these sheets at WestRunton suggests that rotation of toe blocks,generating forward movement of the surrounding loosebeach sand, is the principal process of toe-thrustsheet formation (fig. 6). Passive pressing of toeblocks into the surrounding sand downstairs gravity isunlikely to resolving power in either brittle failure of thesand or contrastingial movement of the sand away fromthe toe blocks (i.e., antithetic thrust sheet widths).The battle count of thrust sheets therefore suggests thatlandslide blocks atomic number 18 actively excavating into thesofter and unconsolidated beac h sand that is displacedoutward as a result of this process. The size and extent of the thrust sheets can be usedas a proxy for the scale, rate, and timing of blockmovement. For example, the bigger landslide blocks areassociated with more extensive thrust sheets, andsheet width is likely associated with excavationdepth. The presence of multiple and overlapping thrustsheets that vary in extent along the front oflandslide blocks (figs. 4, 5) also suggests thatdifferent parts of the toe are active at differenttimes and therefore that sliding rates and volumesaveraged across the finished landslide (Waltham andDixon 2000) likely moderate wide spatial and temporalvariations. Graphic omitted The presence of delicate toe-thrustsheets within the intertidal zone at West Runton is ofinterest because these features are easily destroyedby waves and will be wiped out by every high tide.Figure 6 is a schematic cartoon illustrating apossible formation apparatus for these features.During high tid es, the elevated position of the foreign piss plane (mean high water level) againstthe landslide toe means that there is a small release in head, and low hydraulic potentialgradient, between the landslide toe and its externalenvironment (fig. 6a). The depth of marine water alsolikely increases interstitial pore water pressure bothwithin the submerged beach sand and within thefine-grained landslide sediments and influences in effect(p) pressure (cf. Dixon and Bromhead 2002).Elevated external water pressure at high tide helps tohold back toe advance (Hutchinson 1988). At low tide, when the argument water table is placedwithin the beach sand and is under lower (atmospheric)interstitial pore water pressure, a large differencein head and therefore steepened hydraulic potentialgradient exists between the landslide toe and theexternal environment (sea level) (fig. 6b). Underthese conditions, sliding and the formation ofrelationships essays research papers The position of thrust sheet s aroundthe margins of landslide toe blocks, and theirmorphology and direction of thrusting, suggests thatthey were formed as a result of toe block pressing andmovement in the surrounding sand. Toe-thrust sheetstherefore can be considered as the morphologicalexpression of ongoing instability at the landslidetoe. The upthrust nature of these sheets at WestRunton suggests that rotation of toe blocks,generating forward movement of the surrounding loosebeach sand, is the principal process of toe-thrustsheet formation (fig. 6). Passive pressing of toeblocks into the surrounding sand under gravity isunlikely to result in either brittle failure of thesand or differential movement of the sand away fromthe toe blocks (i.e., different thrust sheet widths).The presence of thrust sheets therefore suggests thatlandslide blocks are actively excavating into thesofter and unconsolidated beach sand that is displacedoutward as a result of this process. The size and extent of the thrust sheets can be usedas a proxy for the scale, rate, and timing of blockmovement. For example, the bigger landslide blocks areassociated with more extensive thrust sheets, andsheet width is likely associated with excavationdepth. The presence of multiple and overlapping thrustsheets that vary in extent along the front oflandslide blocks (figs. 4, 5) also suggests thatdifferent parts of the toe are active at differenttimes and therefore that sliding rates and volumesaveraged across the entire landslide (Waltham andDixon 2000) likely conceal wide spatial and temporalvariations. Graphic omitted The presence of delicate toe-thrustsheets within the intertidal zone at West Runton is ofinterest because these features are easily destroyedby waves and will be wiped out by every high tide.Figure 6 is a schematic cartoon illustrating apossible formation mechanism for these features.During high tides, the elevated position of theexternal water plane (mean high water level) againstthe landslide toe means that th ere is a smalldifference in head, and low hydraulic potentialgradient, between the landslide toe and its externalenvironment (fig. 6a). The depth of marine water alsolikely increases interstitial pore water pressure bothwithin the submerged beach sand and within thefine-grained landslide sediments and influenceseffective pressure (cf. Dixon and Bromhead 2002).Elevated external water pressure at high tide helps tohold back toe advance (Hutchinson 1988). At low tide, when the ground water table is locatedwithin the beach sand and is under lower (atmospheric)interstitial pore water pressure, a large differencein head and therefore steepened hydraulic potentialgradient exists between the landslide toe and theexternal environment (sea level) (fig. 6b). Underthese conditions, sliding and the formation of