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tectonic forces

The longer the time between the arrival of the P-wave and S-wave, the farther away is the epicenter. Each year about 18 earthquakes are major with a Richter magnitude of 7.0 to 7.9, and on average one earthquake has a magnitude of 8 to 8.9. Describe the causes of tectonic stress and how they influence earthquakes and volcanoes. Mostly these anecdotes are told after the earthquake. This chapter has several goals and objectives: Describe the causes of tectonic stress and how they influence earthquakes and volcanoes. The 2001 Gujarat earthquake in India was responsible for about 20,000 deaths, and many more people became injured or homeless. Earthquake effects on buildings are seen in this animation. This may either create a series of small earthquakes or potentially create a large earthquake. Sudden stress, such as a hit with a hammer, is more likely to make a rock break. The two types of seismic waves described in “Plate Tectonics,” P-waves and S-waves, are known as body waves because they move through the solid body of the Earth. Massive earthquakes are the hallmark of the thrust faulting and folding when two continental plates converge. The scientist then draws a circle with a radius equal to the distance from the epicenter for that seismograph. Surface waves are the slowest of all seismic waves, traveling at 2.5 km (1.5 miles) per second. However, it is the epicenter of an earthquake that is reported by scientists and the media.

Stress applied over time often leads to plastic def. Tectonics, scientific study of the deformation of the rocks that make up the Earth’s crust and the forces that produce such deformation. Called the, http://www.youtube.com/watch?v=QzdBx9zL0ZY, http://www.opengeography.org/ch-5-tectonic-forces.html. This is also an uncertain predictor of large earthquakes.

Since stress on a fault builds up at the same rate over time, earthquakes should occur at regular intervals. Along the middle of the two mountain ranges, between the Wasatch Mountains and the Oquirrh Mountains, is the Jordan River which flows from Utah Lake northward to the Great Salt Lake. Earthquake-prone communities should always be prepared for an earthquake. Elastic deformation occurs when the rock returns to its original shape when the stress is removed. P-waves travel through solids, liquids, and gases. referring to the forces or conditions within the earth that cause movements of the crust. The energy from earthquakes travels in seismic waves, which were discussed in the chapter “Plate Tectonics.” The study of seismic waves is known as seismology. When an earthquake will occur is much more difficult to predict. Using data from two seismographs, the two circles will intercept at two points.

The epicenter is somewhere along that circle. In San Francisco, water and gas pipelines are separated by valves so that areas can be isolated if one segment breaks. An earthquake is sudden ground movement caused by the sudden release of energy stored in rocks, called the elastic rebound theory. Is it more likely to break deep within Earth’s crust or at the surface?

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