Wednesday, February 26, 2020

Band of Outsiders Essay Example | Topics and Well Written Essays - 2000 words

Band of Outsiders - Essay Example The movie was one of the finest ever work by Jean-Luc Godard. It was a lyrical tragic comedy, perhaps was one of the Godard's most charming film. The screenplay was written by the director Jean-Luc Godard, and was based on the famous novel Fool’s Gold by Dolores Hitchens. The screenplay was the firm and strong base for the movie. The depth and contents of the movie supported the movie to became the Godard’s one of the best works. The scenes of the movie like the climax scene, a silence after the trio crowded in the cafe and many other scenes had made a significant and narrative effect on the viewers and the critics. These scenes created the essence of the brilliant direction and screenplay for turning the movie into an excellent work in all the fields like direction, screenplay, editing and others. The Band of Outsiders was known for its most superfluous work from the Jean-Luc, as compared to his other work like Breathless and others. From this movie, the Godard turned himself towards the low-scale movie which turned to be a fruitful step later in his film career. The direction made the haul for viewer to watch the long takes in the movie. The depth that had been created by the director in the movie was accordingly to synchronize the momentum of the movie. The long takes in the movie were outstanding creation work exactly from the director Jean-Luc Goddard. The dance scenes in Band of Outsiders were very much grand, although it was a playful and it came out of nowhere, it really did add a lot to the story. The strong point of the movie were the story, the scenes, the direction and these sorts of scenes. In the movie, the two men and the lady were dancing we heard the music cut off and a narrator come over. The narration produced a soothing effect on the viewer even at that time and also up to the present. The director Jean-Luc had tremendously worked out and described what each character was truly feeling as they looked like in the movie that they were having fun and dancing in a cafe. This small element made the viewers to think, what the characters were really thinking as they walked along and talked to each other for the rest of the film. In the movie, it was described simply that simple, but it added a lot of depths. The viewer would then add in the depth himself. This was some great stuff and was one of the many reasons, why Band of Outsiders was one of the excellent efforts from the direction point of view for putting the sensual effects in the movie. Band of Outsiders was the most poetic work from Godard's early films. This was due in large part to the voiceover narration, read by Godard himself, as the screenplay was written by the Godard himself. When the film's celebrated Madison scene, Godard cut out the music and relates the characters' thoughts, as the character Odile wondered if the men could see her breasts moving under the sweater. Arthur thought of Odile, dreaming of her

Monday, February 10, 2020

Long-Term Stability of Clay Slopes Essay Example | Topics and Well Written Essays - 1500 words

Long-Term Stability of Clay Slopes - Essay Example In order to describe "the long term stability of clay slopes", this paper will look at factors that make slopes become unstable overtime; the measurement of the instability; impact of long-term stability; and the prevention of instability of clay slopes. To begin with, long term stability of clay slopes is influenced by several causes which as are embedded in two major factors. These main factors, according to Price (1984) and Ritter (1986, p 121) are shear stress and shear strength. Shear stress refers to the forces that cause movement of materials down slope while shear strength is the force that resists materials from moving down the slope. These forces oppose each other in the sense that, while shear stress wants movement of material to commence, shears strength refuses. This means that movement will only occur when shear stress exceeds shear strength. Otherwise, like Sparks (1964, p 56) puts it, in uniform material, shear stress and shear strength may remain comparatively uniform. It is worth noting that shear stress has several intricate components that make it provoke movement of material down slope. Ritter (1986, p 121) outlines material internal friction characteristics; material normal stress and material normal cohesion as factors that determine stability of shear stress. Any drop or increase in these factors may alter shear stress. Internal friction is further broken down into plane friction (produced when one grain of soil slides past another) and interlocking friction (which originates when particles are required to move upwards and over one another. Secondly, Ritter (1986, p.122) further states that effective normal stress has the capacity to hold the material together, thereby increasing internal resistance to shear. It acts perpendicular to a shear surface and is absorbed by the underlying slab at the point of contact between grains. It should also be noted that some of the shear surface is usually occupied by openings which are filled with air or water. And since pore pressure exists in these interstitial spaces, it tends to support part of the normal stress. Thirdly, Ritter (1986, p.123) further states that clay soils have cohesion, which comes as a result of ions and water by clay minerals, thereby creating a binding structure among particles. Unfortunately though, cohesion decreases with increased water acquisition in the soil material. Clay cohesive strength very much depends on attractive forces between the particles and the lubricating action of the interstitial liquid. The more the clay acquires water, the more the slope becomes unstable. However, it should be noted that the rate at which the slope gains more water and the water drains away determines the time the slope should become unstable. For example, fast gaining and slow draining of water on a particular slope will make the slope fail very fast. On the other hand, slow gaining and fast draining of water will make the slope remain stable for some time. Where clay soils remains in an undisturbed normal cohesive strength, long-term slope stability will be evident. Sparks (1964, p 57) agrees with the above statement and adds that cohesive strength increases with depth thereby exceeding shear stress, hence surface mantle (slope material) is the one to be more unstable. As more water is added , cohesion decreases and when all pores are filled, any further input of water results in complete