earthquake essay on property damages

earthquakes. In all of these types of faults, the different blocks of rock push very tightly together, creating a good deal of friction as they move. If you come up with two spheres, based on evidence from two different seismographs, youll get a two-dimensional circle where they meet. These two ratings describe the power of the earthquake from two different perspectives. Geological research has shown that, possibly under the continuous impact of these disturbances, the western coast of the Japanese islands is settling, while the Pacific coast is rising. An earthquake is a vibration or oscillation of the surface of the earth caused by a transient disturbance of the elastic or gravitational equilibrium of the rocks at or beneath the earth the surface. According to the United States Geological Survey, more than three million earthquakes occur every year. Where did the recent earthquake occur. Such earthquakes are very severe good college admission essay and disastrous. (2) Mid-continental belt is also known as Mediterranean Belt or Alpine-Himalayan Belt which represents the collision or subduction zones of continental plates.

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They do this with a seismograph, a machine that registers the different waves. Meaning of earthquake, my earthquake experience essay, nepal earthquake essay. Sliding Plates, the biggest scientific breakthrough in the history of seismology the study of earthquakes came in the middle of the 20th century, with the development of the theory of plate tectonics. Which caused irreparable damage to human structures. If we look at the past seismic history of Gujarat, it appears that a severe earthquake occurs every 30 years.g., Bhawnagar earthquake, 1872; Kutch earthquake, 1903; Dwarka earthquake, 1940; Broach earthquake, 1970 and Bhuj earthquake, 2001. (4) Chilean tsunami: May 22, 1960, a strong earthquake of the magnitude.6 on Richter scale, generated Pacific-wide tsunamis and claimed 2,300 human lives in Chile. Moderate and intermediate earthquakes are also called as shallow focus and intermediate focus earthquakes respectively. Major tectonic events associated with these plate boundaries are ruptures and faults along the constructive plate boundaries, faulting and folding along the destructive plate boundaries and transform faults along the conservative plate boundaries. Where these plates meet, youll find faults breaks in the earths crust where the blocks of rock on each side are moving in different directions. With this information, they simply note how much time passed between the arrivals of both waves and then check a special chart that tells them the distance the waves must have traveled based on that delay. The lines where plates push toward each other are called convergent plate boundaries.