* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
Download Getting to Know: Why Earthquakes Occur
Physical oceanography wikipedia , lookup
Geochemistry wikipedia , lookup
Age of the Earth wikipedia , lookup
History of Earth wikipedia , lookup
Great Lakes tectonic zone wikipedia , lookup
Earthquake engineering wikipedia , lookup
History of geology wikipedia , lookup
Post-glacial rebound wikipedia , lookup
Seismometer wikipedia , lookup
Getting to Know: Why Earthquakes Occur You’ve probably seen the devastation caused by large earthquakes in photographs or on the news. Dramatic images of collapsed buildings, injured people, and widespread destruction are hard to forget. When we begin to talk about earthquakes, those are the images that often come to mind. These disturbing images may lead people to believe that earthquakes are rare and incredibly destructive. The first thing that people may not realize is that earthquakes are not rare. Small earthquakes happen every day. In fact, some earthquakes are so small that people cannot feel them. These minor earthquakes are only “felt” by sensitive instruments that can detect seismic waves. Seismic waves are waves that transmit the energy of the earthquake. What are earthquakes? To answer that question, you need to recall what you have learned about Earth’s structure. If you remember, Earth is made up of layers. Earth’s center, the inner core, is surrounded by the outer core. The outer core is surrounded by the mantle, which contains molten rock. On top of this molten rock layer is the crust—the layer on which we live! Large earthquakes damage structures such as roads, buildings, and bridges. The crust is made up of many large pieces, called tectonic plates. Tectonic plates fit together like a giant jigsaw puzzle. Some parts of this puzzle are above sea level and form the continents, and other parts are below sea level, comprising the ocean floor. Because tectonic plates rest on partially molten mantle rock, they are always in motion and their boundaries interact with each other. Convergent boundaries form when plates are moving toward one another, divergent boundaries form when plates move away from each other, and transform boundaries form when plates slide sideways past one another. This movement can cause earthquakes. Earth is made up of layers, including the crust, mantle, outer core, and inner core.Tectonic plates are parts of Earth’s crust that move on the mantle. Concept: Why Earthquakes Occur Getting to Know www.discoveryeducation.com 1 © Discovery Education. All rights reserved. Discovery Education is a subsidiary of Discovery Communications, LLC. Are tectonic plates the same as continents? Tectonic plates and continents are not the same. The continents are the parts of tectonic plates that are above sea level. However, tectonic plates also make up the ocean floor. For example, the North American Plate, which is the tectonic plate that the United States rests on, does not end at the shoreline—it continues far out into the ocean. In fact, the edge of the North American Plate is on the sea floor in the middle of the Atlantic Ocean! Sometimes people mistakenly think that continents and islands float on top of the oceans. The truth is that both the oceanic crust and the continental crust “float” on top of the mantle. How is tectonic plate motion related to earthquakes? Seismic waves carry energy away from an earthquake’s focus. Tectonic plate movement is the primary cause of earthquakes. As tectonic plates move, they grind against each other or push into each other. The edges of the plates rub against each other with a lot of friction, and the edges can become stuck for awhile. If this happens, pressure builds up in the crust. Sometimes this pressure is released in a burst of seismic waves that we call an earthquake. An earthquake’s focus, which occurs at the point where the pressure is released when the two plates break loose again, can be near the surface or deep in Earth’s crust. Seismic waves carry energy out in all directions from an earthquake’s focus. Earthquakes can occur anywhere in Earth’s crust. Many earthquakes are so small that they can only be detected using sensitive scientific instruments. Large earthquakes that damage buildings and change the landscape are more common in areas near tectonic plate boundaries. Misconception: I saw an earthquake on TV, and it seemed like the earthquake made cracks in Earth’s crust. Earthquakes can cause smaller areas of ground to crack. However, these cracks do not go through the entire thickness of Earth’s crust and they are different from the large cracks in Earth’s crust, called faults, which are the focus of earthquakes. If the crack formed by an earthquake broke through the entire depth of Earth’s crust, magma would pour out and a volcano would form. Concept: Why Earthquakes Occur Getting to Know www.discoveryeducation.com 2 © Discovery Education. All rights reserved. Discovery Education is a subsidiary of Discovery Communications, LLC.