Earthquakes in General
By: Jonathan Levron
“Earthquakes are one of the most potent natural powers on earth and regularly affect people around the world. Unlike often equally destructive severe weather events such as hurricanes and tornadoes, earthquakes can hit at any time. Earthquakes can also have a array of magnitudes with the strongest having disturbing consequences for the zones where they are concentrated, nearby areas, and even some far away in the instance of earthquake-generated tsunamis” (Briney 1). We think that the ground beneath us is unmoving but the earth’s crust is constantly moving and the destructive forces caused by this moving are called earthquakes. I will be talking about several topics: What causes earthquakes, two types of earthquakes, what their affects are, and what we are doing to predict future earthquakes.
Major Earthquakes are Inevitable in Indiana’s Future
An earthquake felt throughout the Midwest on June 18 was a shaky reminder that earthquakes can occur anywhere.
The earthquake, whose epicenter was located north of Evansville, was felt through most of Indiana and surrounding states, as reported by the Indianapolis Star. The quake was not the largest in Midwestern history, only registering a 5.0 on the Richter scale, nor did it do much damage.
Earthquakes occur almost all over the world and often cause many casualties and injuries, but it is a common misconception to think that all earthquakes or even most of them cause destruction. In fact, most earthquakes aren’t even strong enough to be felt by humans and most animals, and can only be recorded by seismometers that are strategically placed in all corners of the world in order to get a reliable and precise reading on the earthquakes strength. Another common misconception about earthquakes is that people believe that the injuries and deaths that result from earthquakes are because of the earth’s shaking itself, whereas it is in fact usually because of heavy items falling from the incessant vibrations. Earthquakes can be defined as
Report on Earthquakes by Zeta Stevens
Why Do Earthquakes Occur?
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).
An earthquake can be defined as vibrations produced in the earth's crust. Tectonic plates have friction between them which
An earthquake is the shaking of the ground caused by sudden release of energy inside the earth's crust. It's the breaking and moving of tectonic plates along a fault line. Earthquakes can range in size from weak where we don't feel them to extremely violent where they actually thow people around and destroy cities. They may be a result of geological faults or other activites such as volcanoes, landslides, mine blasts and nuclear tests. An earthquake is not always naturally caused.
On March 11, 2011 at 2:46 PM, Japanese time, an 8.9 magnitude earthquake hits, but was later upgraded to a 9.0 magnitude earthquake, happens 231 miles northeast of Tokyo, Japan, at a depth of 15.2 miles. The pacific tsunami-warning centre sends out a warning to the Pacific Ocean from Japan all the way to The United States of America. Around an hour later after the earthquake the waves hit. The waves got up to 30ft high when they hit the Japanese coast. The waves caused widespread devastation washing away cars like they were sticks, collapsing buildings and destroying roads and highways.
The word tsunami comes from a Japanese word meaning “Long harbor waives”. Tsunami is much known and very common in Japan because thousands of Japanese have been killed and some suffered in recent centuries. Tsunami waves generally speaking cause a lot of damages such as, killing people, destroying building, and costing million of dollars. Moreover, a tsunami is a series of great sea waves caused by an underwater earthquake, landslide, or volcanic eruption. The 2004 Indian Ocean earthquake that is located on epicenter off the west coast of Sumatra, Indonesia, is actually one of the worst disasters in the history of Indian Ocean that generated by the most powerful 9.0 magnitude earthquake. An aggressive movement of the Earth's tectonic plates creates an enormous amount of water (probably 30 feet long), sending powerful shock waves in every direction.
...ct so many people per year. In knowing what earthquakes are, people can learn to recognize the signs, and better educate themselves. Through grasping how an earthquake occurs, and where they happen in the world can better help people understand earthquakes as a whole. Also, in being mindful on how earthquakes are measured and their magnitude can help someone become better educated on the topic of earthquakes since they could happen at any time. Besides the fact, learning about the causes, foreshocks, mainshocks, and aftershocks are also vital in sensing earthquakes. Not only is it fundamental to know the facts behind earthquakes, it is also crucial to know where they occur, such as in places like Haiti, Japan, and Mexico. Earthquakes are not preventable, but in knowing the workings behind them, people can learn to cope with them to a greater degree.
Tsunamis are series of waves, generated by earthquakes, landslides, volcanic eruptions, explosions, or even impact of cosmic bodies, that travel across the ocean and have extremely long wavelengths. A tsunami can be created when a disturbance displaces a large water mass from its equilibrium position. In earthquake-generated tsunamis, the water column is disturbed by the uplift or subsidence of the ocean floor. Submarine landslides, which often come with large earthquakes, as well as disintegration of volcanic edifices, can also disturb the overlying water column as sediment and rock slump downslope and are redistributed across the sea floor. Similarly, a violent submarine volcanic eruption can create an impulsive force that uplifts the water column and generates a tsunami (Ruff, 2003, Yalciner, 2003). Conversely, terrestrial landslides and cosmic-body impacts disturb the water from above, as energy from falling debris is transferred to the water into which the fragments falls (Murty, 1977, Bryant, 2001, Clague et al., 2003, Yalciner, 2003).