Plate tectonics Essay

Ever since the beginning on time, Humans believed the ground is solid and immobile. But this is not true whatsoever. The Earth is every-changing and continually in motion. The stability of the Earth is not at all what we think it is. Thinking about the rotational axis of the Earth, and possibly of what the Earth may become at a certain point in time, has a great influence on understanding all aspects of living things, either in the past, present, or future. The study of Plate tectonics is accredited to most of the creations of Mountain Ranges, the drifting of continents, earthquakes, and volcanic activity. Plate tectonics and mountains also play a big part in the geological features of our planet or any planet for that matter. Geophysics, which studies the physics of the Earth, has led to many important findings about the Earth and how it is made. Seismologic studies of planet Earth have revealed new information about the inside of the Earth that has helped to give new openings in understanding plate tectonics. The Earth is made of several significant layers. Each one of these layers has its own properties. The crust is the outermost layer of the Earth. The crust is made up of the oceans and continents. The crust has a fluctuating thickness, being thirty to seventy-five kilometres thick in the continents and ten to fifteen kilometres thick in the ocean basins. The crust is made up mainly of alumino-silicates (Fowler p472). The layer underneath the crust is the mantle, which is made up mainly of ferro-magnesium silicates. The mantle is approximately two thousand, nine hundred kilometres thick, and is separated in to the upper and lower mantle. It is in the mantle where most of the centralized heat of the Earth is located. Big convective cells in the mantle disperse heat and produce the plate tectonic processes. The core is the last layer of the Earth, which is broken down into the liquid outer core and the solid inner core. The inner core is about thirteen hundred kilometres thick and the outer core is about twenty-three hundred kilometers thick. A nickel-iron alloy mixture makes up the outer core, and the inner is almost all composed of iron. The Earth is separated in layers based on composition and mechanical properties. The top layer is the lithosphere, which is comprised of the solid upper mantle and the crust. It is divided into plates that move due to tectonic forces. The lithosphere floats on top of a semi-liquid layer that is called the asthenosphere. The asthenosphere allows the lithosphere to move around since it is much weaker (Tarbuck p605). Early scientist believed that one huge supercontinent existed over two hundred million years ago. The name for this supercontinent is Pangaea. Pangaea was broken in to several pieces, and each piece was a part of the lithosphere. They believed that the pieces of Pangaea formed the continents that we know of in present day geology. When Pangaea existed, the rest of the Earth was covered by an ocean called Panthalassa. Eventually, Pangaea split into two land masses, Laurasia to the north and Gondwanaland to the south. The theory of plate tectonics does in fact have an explanation for the movement of the Earth’s crust. The fact that Pangaea did exist could be quite plausible. Scientist also believes that as the Pacific Ocean is closing, a supercontinent may form in millions of years to come. In present day geology, we can consider Eurasia as a supercontinent because the Ural Mountains separate Europe from Asia and make a line of compression and change where the two continents smashed in to each other (Tarbuck p606). In 1620, Sir Francis Bacon wrote in his book Novan Organum and noted that the coasts of the Atlantic Ocean seemed to be parallel to one another. However, the plate tectonic theory really started to begin in 1915 when Alfred Wegener proposed the theory of continental drift. Alfred Wegener believed that the continents bulldozed through crust on the ocean basins, which would explain why most of the coastlines look like they could fit together. Wegener was not the first one to realize that the continents looked like they could fit together because Magellan and other early explorers noticed this also. However, he was the first person to realize that the Earth’s surface has changed over time, and that continents that are not together now could have possibly been joined together at some point in the past (Twiss p532). Many people were against Wegener’s theory because he did not really have an explanation for why the continents moved. During that time, geologist believed the Earth possessed these features because the planet went through periods of cooling and heating. Anti-mobilists were people that were against Wegener’s theory. People who were in favor of Wegener were known as mobilists because they had seen proof of continental movement in the Alps (Fowler p475). In a few short years, Wegener’s theory was denied. However, his theory was the first time the idea of continental movement was announced to the science community. His theory laid the foundation for the advancement in twenty-first century plate tectonics. Years would pass and more evidence became available to support the idea that plates were in fact in motion and changed over a period of time (Fowler p476). After the Second World War, more information was discovered which supported the theory of plate tectonics. In the sixties, a bunch of seismometers were installed to collect data on nuclear bombs, and these instruments sparked curiosity among geologists. It showed that volcanoes, earthquakes, and other features were along the Pacific Ocean and ran along the continents edges for the most part. It turned out that all of these edges became known as tectonic plates (Kearey 2009). Further studies showed a pattern of magnetic fields in the ocean basins. The rock basalt contains a lot of magnetic minerals called magnetite. The lava forms and cools and the magnetic minerals align with the North Pole. This proves that the Earth has gone through several magnetic reversals; this would not be possible if the lithosphere was not in motion. Since all of this has been discovered, plate tectonics has gained acceptance as the Earth processes (Kearey 2009). Plate tectonics is made up of the study the motion and change in the Earth’s crust. This is based on the theory that the lithosphere is divided into seven major plates and several minor plates, and they all move in accordance with each other. They also move in relation to hot spots, which is where mantle material comes up. The plate tectonic theory tries to tell us that the Earth’s crust moves over a period of time. The crust moves in a rigid way, which explains the change that we see. The theory is based on a few beliefs. New material is made by the spreading of the ocean floor and eventually become part of a plate, and motion of plates occurs only at plate boundaries. Plates are rocks that pretty much float on top of the asthenosphere. The crust has two types, the oceanic and continental; they both differ because of composition. The continental crust is made up of mostly granite. This brings us to the conclusion that the rocks have a lot of quartz and feldspars. However, most of the oceanic crust is made up of basalt. Basalt usually has other minerals like olivine and mafic minerals (Fowler p477). There are three types of plates, divergent, convergent, and conservative. Wide places of change are usually around plate boundaries because of the two plates colliding. We know that these boundaries exist because of their motions. One sort of plate is the divergent boundary. At this boundary two plates move apart. As they move apart it creates a crack in the crust and magma comes in to the ocean and cools. When the plates move, more and more crust is formed. Divergent boundaries are believed to be the reason for the plates moving. The formation of the new crust pushes the two plates apart, this is apparent in the mid-ocean ridge, which helps to move Europe and North America further and further apart. Mid-ocean ridges are mountains under water. They can even be as tall as mountains that are on land, this process is known as convection. Magma is pushed up by convection currents. Some magma erupts through the crust and some moves under the crust away from the ridge crest. The magma flows and helps move the plates away from each other to allow more crust to be created and to grow; this is called convection cells. We know this to be sea-floor spreading. The mid-ocean ridge plays a big part in the plate tectonic theory because of the minerals uniqueness within the basalt. It contains a lot of magnetic minerals that align with the Earth’s magnetic field when it crystallizes. In the past, scientist has known the Earth’s magnetic field to change. When the magnetic minerals align scientist can use it to date the crust. This plays an important role in the theory because it is first proof that plates were in fact moving and have been for almost Earth’s existence. We can use the magnetic information to prove that the plates are moving, and we can also determine that new crust is being formed and that the old crust was erased in a continuous process that has been going on for all of Earth’s past. The oldest crust ever dated is approximately one hundred million years old, which is quite recent in geologic time. This may lead you to question, where did all of the old crust go (Fowler p478). This brings me to my next discussion which is convergent boundary. A convergent boundary is when another plate overrides another plate, causing one plate to go underneath it. Most of the boundaries can be found in island systems and trenches. Most of the old crust goes in to these systems as new crust is formed at spreading centers. This explains why scientist cannot find any crust that date past the Cretaceous period. The old crust was destroyed by the process of subduction. Earthquakes are very active in subduction zones. The earthquakes occur because one plate slides under another. Although this movement is not visible, it has very strong effects on the Earth. The outer edges of the Pacific Ocean are referred to as the â€Å"Ring of Fire† because the subduction zones go all around the Pacific Ocean. Volcanic activity is also caused by subduction zones because when one plate goes under another it gets hotter. The reason it gets hotter is because it is closer to the mantle. When the old crust gets close to the mantle, it melts and forms in to magma. The magma eventually runs up through the crust and forms volcanoes. One good example of a subduction zone surfacing is the Aleutian Islands off the coast of Alaska (Twiss p536). When two plates collide, subduction zones do not always occur. Continental crust is less dense than oceanic crust, and when they collide, they do not run over each other. Instead, they kind of plow in to each other and create mountains. This type of boundary is called a collisional boundary. An example of two plates colliding is the Himalayas in India. The third type of boundary is the transform boundary. It is called this because plates are not destroyed or created, but they slide past each other. A good example of a transform boundary would be the San Andreas Fault in California. In California, the Pacific Plate and the North American Plate are sliding past each other. This is why many earthquakes occur in that region. The earthquakes occur because of the strain that the two plates exert as they slide past each other (â€Å"Historical perspective). The Earth changes in many ways, however there are three forces the cause change within the Earth. When these forces act, they create stress and they change the volume and shape of a material. The three main types of stress are shear, compressional, and tensional. Stress puts a lot of strain on the Earth which causes the change in rocks and the Earth’s crust. Compressional forces may cause a rock to compress or shorten. Tensional forces may cause a rock to become longer and pull apart. Shear forces can cause rocks to slip past each other (â€Å"Historical perspective). Faults are places where rocks have been broken and have been changed. There are three big types of faults. These are strike-slip, normal, and reverse. The stresses caused by motion of the plates build up over a course of time and ultimately cause the Earth’s crust to break when the rocks rub past each other. Usually when a fault happens, an earthquake occurs. Every plate boundary has some characteristic of a type of fault. Normal faulting can be affiliated with crustal extension. Normal faults can usually be found at divergent boundaries. Crustal shortening can be affiliated with reverse faulting. Reverse faults can usually be found at convergent boundaries. Strike-slip faulting is affiliated with sideways movement of the crust. These faults usually form at transform boundaries (Twiss p538). Even today, we are constantly reminded that the plates are in motion. One recent catastrophe caused by plate tectonics was the earthquake that happened in Haiti. Studies suggest that the earthquake occurred due to a strike-slip fault. The Caribbean sits on its own little plate and is surrounded on three sides by the bigger North and South American plates. Scientists believe that the North and South American plates are moving westward at approximately two to three centimeters per year. Based on the recordings of the earthquake, the Haitian quake seems to have occurred close to the Enriquillo Fault. The Enriquillo Fault is a big strike slip fault that runs across the southern border of Haiti. Scientists presume this is the fault that most likely ruptured because it is closest to the epicenter of the rupture. Although this was a big catastrophe for human life on the island of Haiti, it was not really unusual given the plate tectonic activity in that area. Unfortunately for Haiti, it is one of the most poorest and underdeveloped countries in the world. Its government was not really in the position to have any preparations in line for such a huge earthquake, and this caused thousands of people lost their lives (Kearey 2009).

Why do people watch reality TV

Why do people watch reality TV Are people dangerously disillusioned with their livelihoods such that they have to keep watching others on TV? This is a question that many scientific papers try to unravel as these programs continue to undo our civilized society. The shows are continuously attracting a large audience every new day. There are mixed reactions that explain such a rise. Advertising We will write a custom essay sample on Why do people watch reality TV? specifically for you for only $16.05 $11/page Learn More The great quantity of the programs looks like they are as reliable as the seasons, with shows like the â€Å"American Idol† and some Soap Operas being more popular than any other time ever. Their imitations are proliferating the cable channels at an alarming rate. In the entire world, people are fascinated by the rising popularity of reality TV programs. This paper explores the reasons behind the popularity of reality TV programs. Advantages of reality TV programs To understand the reason why many people watch reality TV, it is imperative to analyze the advantages of these programs. Firstly, these programs can be informative and thought provoking (Hill, 2005). For instance, programs that deal with crime can educate people on the dangers that policemen deal with on a daily basis. Other programs that deal with health issues can help people, especially pregnant women, depict early signs of complications. It is possible for viewers to learn of the disease symptoms through the information gotten from some of the reality programs like Dr. OZ, for example. In these programs, viewers also identify themselves with the celebrities in the view that they will one day become ones. These programs provide people with an opportunity to showcase their natural gifts and make people aware of social causes. What is so appealing about reality TV programs? The greatest appeal that makes these programs so popular is that viewers feel as though they are real participan ts. Secondly, the suspense created by these programs makes viewers anticipate the next episodes. Especially the Soap Operas create a high level of suspense that makes viewers remain glued to their TV sets wishing to see the next move. Other programs, such as the American Idol, give their viewers toll-free numbers to participate by making their remarks. This has a great appeal to the viewers who would always want to make recommendations. Thirdly, most of these programs deal with the real life situations that people are facing. Thus, other individuals watch them as a way of trying to find means to come out of their flabbergasting circumstances in life (Hill, 2005). For instance, married men may watch reality programs that deal with cheating to find out tactics to deal with their cheating wives. Another appeal is that viewers are given a chance to compare their lives with those of the shows’ protagonists (they are able to blend fantasy with reality).Advertising Looking for essay on social sciences? Let's see if we can help you! Get your first paper with 15% OFF Learn More However, some reality shows promote poor behavior such as emphasizing just sexual aspects of dating as opposed to developing mature and loving relationships. This is a detrimental effect of the programs. At times such detrimental aspects can contribute to some social problems in the society. Conclusion Different people watch reality programs for various reasons, but the greatest of all seems to be the fact that these programs make the viewers feel as if they are part of the action. The above article explores the peoples behavior and the manner in which the programs affect their livelihoods, either positively or negatively. Reference Hill, A. (2005). Reality TV: Factual Entertainment and Television Audiences. London: Tailor Francis group.

Love in essays

Love in essays Love is defined as when you seek and foster the goodness of others in the context of their concrete situations. That statement can be interpreted in many different ways. There are many different types of love: self-love, friendship love, erotic love, parental love, love of nature, romantic love, and Gods love. Self-love is when you love yourself, not vainly, but just caring about yourself and you well being. Friendship love is when you and another person love each other in a platonic way. Erotic love happens when two people want to join together in union in both body and mind. Parental love is the affirmation parents make about their kids. Its an unconditional love because parents love their kids no matter what bad things they do. Love of nature is when you respect all of Gods creations, and nurture them. Romantic love is friendship love only on a much deeper level. The two people care about each other so much that they only want to be with each other. Gods love is the lo ve that God has for us. God made everything in his image and likeness, so obviously he loves everything on earth. The movie Forrest Gump depicts all of these types of love, some more obviously than others. Friendship love can be seen in Forest Gump most easily between Forest and Jenny. From the time they first met on the school bus, when Jenny let Forest sit next to her, they became friends forever. They grew up as best friends. They helped each other out when they needed it. They cared about each other. An example is when some local bullies were making fun of Forest and throwing stones at him, Jenny told Forest to run, he did, and then was free from the bullies harm. An example of when Forest was there for Jenny when she needed it was when Jenny was trying to get away from her abusive father. Jenny left her house and with Forest, went into the corn field. He was there to give her support and to try to make her...

Standards of Practice Coursework Example | Topics and Well Written Essays - 250 words

Standards of Practice - Coursework Example These laws and standards include maintaining of professional competence in practice, meeting educational qualifications and avoidance of engaging in professional misconducts such as practicing fraudulent activities, practicing without proper licensing and abusing patients. These studies will continuously update nurses on these issues concerning the legal requirements and put them in a better position to adhere to them. This will facilitate safer practice in nurses (Malloch & Porter-OGrady, 2006). Enabling nurses to get access to further studies puts them in a position to work as team leaders in their various departments in the healthcare system. The giving of nursing care to patients is a challenging task that involves a team effort. The healthcare sector is very dynamic since the diseases and other issues change rapidly depending on various factors such as climate and geographical locations. Furthering of learning by nurses will equip them with the relevant expertise to tackle these emerging

Hardware and Software Standardisation Essay Example | Topics and Well Written Essays - 750 words

Hardware and Software Standardisation - Essay Example From a recent survey done by Symantec involving 500 global companies, it was observed that nearly 50% of those companies "still struggle to manage complex infrastructure built on different hardware and software from different vendors". (Courtney) Upgrading and troubleshooting can be much easier with a standardised set of hardware. Configuring and installing patch upgrades to software also becomes simpler, easing the burden on network administrators. In a heterogeneous environment (i.e. one with many different hardware and software platforms) different expertise will be required for configuration and administration, thus increasing the complexity of administration. Cost reductions are possible due to bulk purchasing. Hardware can be purchased at discounts when buying in multiple units. Software licensing costs can be reduced by applying for volume licensing. Instead of getting per-seat licenses, companies can negotiate for flat licensing schemes which do not depend on the number of seats. (Schweitzer) End user training becomes much simpler with a standard set of software. The support staff finds it easy to troubleshoot queries from end users resulting in minimum disruption for work. Moving within divisions and branches will be without the pain of learning a new set of applications every time an employee changes location. Quick troubleshooting turnar... Installation of licensed software eliminates most problems caused by defective pirated software, lack of documentation and technical support. (Why a License Matters). These benefits indirectly increase the stability of the network. However, standardization is not without its drawbacks. Single vendor lock-in, vulnerability to buyouts of vendors and inability to support varied needs and platforms of certain staff such as designing and publishing staffs are the possible drawbacks. (Schweitzer) The last drawback of not being able to support varied requirements of end users can be reduced to a certain extent by having multiple load images. A load image (or a boot image) is a type of disk file which typically "includes the operating system, utilities and diagnostics, as well as boot and data recovery information" (Boot image). Different boot images can be bundled together with specific application requirements of different user groups. As such, maintaining multiple load images as apposed to a single image can be advantageous. (III) Licensing As noted earlier, software standardisation helps companies to manage their software licensing. The benefits are two fold; cost reductions and ease of administration and liaison. As a result, organisations can fulfill their ethical obligations by abstaining from software piracy and can also guard against severe penalties enforced by stringent piracy laws. Abiding to software piracy laws and proper licensing of all software applications helps a company to become a member of the Federation Against Software Theft (FAST), a professional body formed to combat software piracy. FAST is very strict about its members adhering to the code of conduct put forward by them. Members get a range of benefits including education,

Development task 2... assignment with label sketch - 3

Development task 2... with label sketch - Assignment Example The depth of the concrete has to be greater than 500 millimeter. From ground level, the depth of the concrete must be greater than 1500 millimeter (Cyril, 2003: 110). Since the ground condition has firm clay, therefore there is a need to consider the depth of foundations. Clay exhibits the property to shrink or contract depending on the moisture content present in it (Kenneth, 1993:25). At the same time, if the surrounding area has trees, there is a possibility that the trees would absorb the moisture from the clay and hence, the foundation may experience settlement to a significant level. For this case, it is essential to consider the depth of the foundation. A trench fill foundation is thus ideal for this type of site condition. Research suggests that â€Å"trench fill foundations are quicker to prepare than deep strip foundations. This means that there is less disruption once the building work starts and not as much labour time will be needed. It is less likely that subsidence will occur in cases where there may be changes in the soils substrata† (Mosley & Bungey, 2000, 48). The site has different ground conditions and has different soils. Thus, it has a weak bearing capacity. For this purpose, the ideal foundation would be strip, grid or mat foundation. In this case, the suggested foundation is mat foundation. Because of varying ground conditions, majority of the isolated footings would have large areas and thus, it would become uneconomical (Terzaghi et.al, 2006, 256)l. According to the British Code, â€Å"Where the subsoil is very weak the load needs to be spread over a greater area. This is achieved by casting a slab of concrete over the whole ground area and thickening the slab where walls are to be placed†(Perry & Perry, 2009, 118). The design of any reinforced concrete structure aims at a suitable and economical design and for this purpose, mat foundation is ideal. A mat foundation is often used by designers when isolated footings may

Breathless Reaction Paper Essay Example for Free

Breathless Reaction Paper Essay Katherine Paler- Rivera According to the many articles and film history that I read, this is the first feature film directed by Jean- Luc Godard who was considered the influencial director that started the French New Wave. And based on our lectures, what makes the French New Wave famous was the technique like jumpcuts, shooting on location, using handheld cameras, loose narrative form or improvised dialogue. Godard also uses the history of cinema art and music. He also includes pictures in posters of famous artists like Picasso and Renoir women. The music in the soundtrack also includes Mozart’s clarinet concerto and French pop radio. The entire story started when the character of Michel Poiccard which Jean Paul Belmondo portrays, has stolen a car. While he was driving he passed by two hitch hikers and decides to decline for the thought they were far too ugly for him. Then suddenly, he realized that the cops was behind him. He hid on the side of the street. Thinking he got away he feels relieved. But suddenly a cop found him. He was shocked and unconsciously because of his instinct killed the cop. It was not shown how he shot the cop, it was suggested because the next scene, the cop falls down in the bushes. Then he runs away in an open field. In Paris, he called up somebody on the phone but no one is answering. Then he bought a newspaper from a boy in a bicyle, browse it a bit then head to an apartment employee asking for that somebody. He just took the keys when the man was not looking. Next scene he was inside the room. He just had a quick time in the wash room to freshen up. He was looking for money in the drawer but he was disappointed. He took a newspaper, read a bit then rubs in in his shoes. Then a some girl opens the door and let him in. The room was full of posters of girls. He was asking for money. While the girl was changing, Michel easily took the money in her wallet. Then in the next scene he was on the streets looking for a girl. It was Patricia Franchini who was portrayed by Jean Seberg. She was studying journalism whom he had met in Nice a few weeks earlier. She was selling New York Herald Tribune. Michel was having a conversation with him about what had happen in their stay in Nice, his women and their plans. He asks for a copy of the newspaper but return it once he realized it had no horoscope. They were planning to see each other on the same same street when the day ends. When they parted, he saw a newspaper stand, bought a copy. Patricia rushed through him and gave him a quick smack on the cheek. Right then and there I observed that these two were an item. In the building where he got inside, he was looking for a guy friend named Tolmachov.. They talked about certain guys common to them. Then his friend handed him an envelope which he was not please. He was given a certain phone number that he called. Then he bid goodbye. Two gentlemen came inside the building, the bigger man I knew was an inspector. He was asking for Michel or a certain other name. At first Tomalchov denied he saw Michel but they were busted when a girl passed by and the detective asked her if he saw Tomalchov with a man 5 minutes ago. He was also reminded that accessory of a murder is a crime. I find Michel’s character rude, proud, dishonest and self centered. He likes to have everything easy without trying to work on it. Examples are the cars he stolen, the man he beat up in the comfort room so he can have money. I don’t think the respect Patricia. He â€Å"uses† people and loves to use the word â€Å"louse†. He almost always has a cigarette on her mouth which makes me annoyed. Some critic said he made it sexy but I don’t find it appealing. As usual he always has a newspaper but I don’t think he paid for it. He wore sunglassed even if its late in the afternoon which I find truly absurd. Patricia’s character gets into my nerve. I hate movies that shows women they are like a â€Å"thing to be used†. I don’t like if someone used bad words to a woman. Good for him that he told the police about Michel. The background music also bores me. They keep on using it again and again. Except for the classical music they played when they were inside Patricia’s room. There was also this scene when Patricia was interviewing a man alongside other journalist. When she asked â€Å"What’s your greatest ambiton? † The man replied, â€Å" To become immortal and then die. † Patricia took off her sunglasses, think deeply and face the camera as if connecting to the viewers. In the scene where he called the cops about Michel, she even talked to him hear to heart. She love him that’s why she gave him away which made him furious. According to Wikipedia, â€Å"Godard envisaged Breathless as a reportage (documentary), and asked the Cinematographer Raoul Coutard to shoot the entire film on a hand- held camera, with next to no lighting. In order to shoot under low light levels, Coutard had to use liford HPS film, which was not available as motion picture film stock at the time. He therefore took 18 metre lengths of HPS film sold for 35mm still cameras and spliced them together to 120 metre rolls. During development he pushed the negative one stop from 400 ASA to 800 ASA. The size of the sprocket holes for motion picture film and the Cameflex camera was the only camera that would work for the film used. † â€Å"The production was filmed on location in Paris during the months of August and September in 1959, using an Eclair Cameflex. Almost the whole film had to be dubbed in post- production because of the noisiness of the Cameflex camera and because the Cameflex was incapable of synchronized sound. † â€Å"Filming began in August 17, 1959. Godard met his crew at the Notre Dame cafe near the Hotel de Suede and shot for two hours until he ran out of ideas. Coutard has stated that the film was virtually improvised on the spot, with Godard writing lines of dialogue in an exercise book that no one else was allowed to look at. Godard would give the lines to Belmondo and Seberg while having a few brief rehearsals on scenes involved, then filming them. No permission was received to shoot the filmin its various locations (mainly the side streets and boulevards of Paris) either, adding the spontaneous feel that Godard was aiming for. However all locations were picked out before shooting began and Assistant Director Pierre Rissient has described the shoot very organized. Actor Richard Balducci has stated that shooting days ranged from 15 minutes to 12 hours, depending on how many ideas Godard had that day. Producer Georges de Beauregard wrote a letter to the entire crew complaining about the erratic shooting schedule. Coutard claims that on a day that Godard had called in sick de Beauregard bumped into the director at a cafe and the two got into a fist fight. † â€Å"Godard shot most of the film chronologically, with the exception of the first sequence which was shot towards the end of the shoot. Filming at the Hotel de Suede for the lengthy bedroom scene between Michel and Patricia included minimal crew and no lights. This location was difficult to secure, but Godard was determined to shoot there after having lives at the hotel after returning from South America in the early 1950’s. Instead of renting a dolly with complicated and time- consuming tracks to lay, Godard and Coutard rented a wheelchair for the film that Godard often pushed himself. For certain street scenes Coutard would hide in a postal cart with a hole in it for the lens and stamped packages piled on top of Coutard. Shooting lasted 23 days and ended on September 12, 1959. The final scene where Michel is shot in the street was filmed on the rue Campagne- Premiere in Paris. † It left me hanging where Michel was shoot and Patricai catched up with the detective. Their dialogue had me thinking what was the meaning of their conversation especially the word â€Å"louse†. In my research it means a plural of â€Å"lice†, a wingless usually flattened blood sucking insect parasitic on warm- blooded animals or a person who has a nasty or unethical character underserving of respect. Michel for me is the big â€Å"louse†! Frankly speaking I was not really into the film. The very first time I watched it, it was all in French with no subtitles. I tried myself to be interested with it but I just found myself bored. Good thing our teacher shared a copy with subtitle. Being a student I was diligent in all the dialougues and scenes. I was carefully observing the techniques that I’ve learn in French New Wave. I find it fascinating that during that time, Godard was a young director who was thinking outside the box. I love the confidence and the guts he puts into his film. He was even part of the film. So I tried to know him more. His most influential innovations was to design shots that seem astonishingly flat. He is the most widely imitated director of the entire post war era.