One of the worst natural disasters in United States history to this date occurred almost 109 years ago. On April 18, 1906 at 5:15am in San Francisco, California, the earthquake of San Francisco occurred hitting between 7.9 and 8.3M on the Richter scale. The San Andreas Fault, which is about 600 miles long, running from the Gulf of California to Cape Mendocino and is an active strike-slip fault, cut through the continental lithosphere to cause the San Francisco Earthquake of 1906. An earthquake is a trembling or shaking of the ground produced by movements along a fault (Strahler, 2012). After the tension is released at a critical point, the fault or tectonic plate slips and relieves the strain and creates the seismic waves, which radiates out in all directions causing the shaking of the surface.
Seismic waves are energy waves that are caused by the sudden breaking of rock in the earth’s crust, or because of an explosion caused by man; these waves travel through the earth and can be recorded by seismographs. There are many different types of seismic waves, but the two main types are surface waves, which can only move on the earth’s surface like a sort of ocean wave, and body waves, that travel through the earth’s innermost layers. Earthquakes make up both surface and body waves. Both surface and body waves can be broken down to two main
We will begin by discussing the land that is underneath the structures and its reaction to the earthquake. According to National Geographic there are three types of ground, Fault-zones, Landfills, and Bedrock. Even though each of those ground shakes during an earthquake, the building itself reacts differently to the terrains.
Earthquakes happen when two tectonic plates touch each other. When those plates experience tension and friction, they lock up, preventing any kind of movement. As soon as the pressure is suddenly released, an earthquake can occur. The phenomenon of rock breaking along a fault can cause the ground to shake because of the release of energy being given off in the form of seismic waves (“Earthquakes”).
Earthquakes are a natural part of the Earth’s evolution. Scientific evidence leads many geologists to believe that all of the land on Earth was at one point in time connected. Because of plate tectonic movements or earthquakes, continental drift occurred separating the one massive piece of land in to the seven major continents today. Further evidence supports this theory, starting with the Mid-Atlantic ridge, a large mass of plate tectonics, which are increasing the size of the Atlantic Ocean while shrinking the Pacific. Some scientists believe that the major plate moveme...
Mr. Adams describes the San Francisco earthquake as his most profound human suffering experience because the horror of shaking floors, parts of his mom’s house collapse to the floor, and got a broken nose from stumbling into a brick wall (Ansel Adams & The 1906 Earthquake 2008). Earthquakes are part of natural disasters of the earth and normally caused by shaking the ground and rapid movement of one block of rock slipping past another along fractures in the earth crust called faults. Faults are usually locked excluding abrupt movements with slippage that create earthquakes (Lutgens, F. & Tarbuck,
The earth is split into four layers, inner and outer core, the mantle and crust. The top of the mantle and crust make up what is like the skin of our earth (see source 2). The skin is split up like a puzzle and we call these puzzle pieces’ tectonic plates (see source 1). These plates are constantly moving and the plate boundaries (edges of the plates) move and slide past one another. Sometimes as the plates move the plate boundaries become stuck. Pressure builds up in the stuck area over time and eventually breaks. This is why earthquakes occur due to the sudden movement of the plate sliding and breaking creating a fault line to go off. The fault line is the line on which the
People will be relatively safe in buildings build since the 1970’s. However, this doesn’t mean everyone is safe. In fact the majority of buildings in the city today were built before then. Some businesses will be brought to a stand still for weeks, or even months. The economic impact will of a ’06 sized quake will be between $100 billion and $200 billion, and these effects will be felt worldwide. Chances our however that the next “big one” will be bigger than the 1906 earthquake. Ultimately, the impact of natural disasters, especially earthquakes, will be something we will always have to
An earthquake is a vibration of the Earths surface that follows a release of energy in the Earths crust. There are various ways this energy is released. Manmade explosions, dislocation of segments of the crust or volcanic eruptions are all triggers for an Earthquake; however, most are caused by a slippage of faults. A fault is a fracture in the Earths crust along which two blocks of the crust have slipped within one another. These faults are grouped into three categories (normal, thrust and strike-slip) and are located all over the Earth.
Earthquakes are caused by tectonic plates moving in the earth's crust. They either move apart or pull together at faults. Two forms of faults are normal faulting where the hanging wall moves downward causing rocks to be pulled apart by tension and reverse faulting, which is the opposite where the hanging wall moves upward casuing rocks to be forced together by tension. These movements cause tectonic plate boundaries called divergent boundaries, convergent boundaries and transform boundaries. Each boundary is different and play a
“Until fairly recently, geologists and other scientists were not totally sure what caused earthquakes. Now with swelling technology, the result of better monitoring, and an enhanced understanding of plate tectonics, they are able to give more solid explanations for them” (Briney 1). The first topic is what causes earthquakes but first let’s talk about the earth’s crust. The earth’s crust is comprised of massive rocks called tectonic plates. “There are a few handfuls of main plates and dozens of smaller, or minor, plates. Six of the majors are named for the continents embedded within them, such as the North American, African, and Antarctic plates. Though smaller in size, the minors are no less significant when it comes to shaping the Earth. The tiny Juan de Fuca plate is mostly responsible for the volcanoes that dot the Pacific Northwest of the United States. The plates make up Earth's outer shel...
The earth has four major layers: the inner core, outer core, mantle, and crust. The crust and the top of the mantle make up a thin skin on the surface of our planet. This skin isn’t all in one piece. It is made up of several pieces covering the surface of the earth, like a puzzle. These puzzle pieces keep slowly moving around, sliding past one another and bumping into each other. We call these puzzle pieces tectonic plates. The edges of tectonic plates are called plate boundaries. Plate boundaries are made up of many faults, and most of the earthquakes around the world occur on these faults. The edges of the plates are rough and get stuck while the rest of the plate keeps moving. Eventually the plate edges of a fault unstick and results in an earthquake.
Earthquakes can be very dangerous but what matters the most is that everybody is safe, and that we need to work together. One earthquake, in the Philippines, was truly devastating. It was classified as a 7.2 magnitude. The Philippines responded very well by gathering their resources, spreading the word, and giving donations. They bounced back very quickly.
The effects caused by earthquakes are devastating. They cause loss of human life and have effects on infrastructure and economy. Earthquakes can happen at any time anywhere. In January 12, 2010 an earthquake of a magnitude of 7.0 hit the nation of Haiti. An estimation of 316,000 people were killed, and more than 1.3 million Haitians were left homeless (Earthquake Information for 2010). Haiti was in a terrified chaos. After the earthquake, families were separated because many of the members were killed. Homes, schools, and hospitals were demolished. People lost their most valuable belongings. It will take time for the country to recover from this terrible disaster. The long damages are economic issues, health-state, and environmental issues that effect in the beautiful island of Haiti.
An earthquake is the shaking of Earth’s surface caused by rapid movement of the earth’s rocky outer layer. “Earthquakes occur when tension stored in rocks suddenly releases” (Vogt 12). Faults occur at these places where rocks on either side of the crack have moved. Oceans are very common places for major tectonic plates to shift. When two plates separate, new oceanic crust is made near the fault as magma rises and eventually sets on the sea floor. If the plates on either side of the fault continue to spread then the ocean slowly becomes larger in width. This is called seafloor spreading. Mid-ocean ridges are characterized by a crack like valley at the fault. This crack like valley is caused by the tension pulling the plates apart, causing normal faulting to occur a number of times in the divergent boundary.