Because of the fault line
Seimsic Lines
Well verbs for earthquake would be: shake, roll, move, tremor, wave, and aftershock to name a few.
No it isn't. There are several factors which contribute to earthquake fatalities: the size of the earthquake, the amount of population in the affected area, and the quality of construction of the buildings in that area. So, a huge earthquake taking place in an unpopulated region of Alaska, for example, would cause few if any fatalities, whereas a much small earthquake in Haiti caused lots of fatalities, due both to density of population and to poor construction standards.
It wasn't hit directly by the earthquake. It did however, experience tremers and a surge from the ocean that destroyed a few things.
The most earthquake prone part of the US is Alaska. California is the second most earthquake prone state and Hawaii third. According to the USGS National Earthquake Center, there is an earthquake of magnitude 7.0 or greater in the US once every few years.
The effect of the earthquake as it spreads from the epicenter gets weaker and weaker the farther you go from the epicenter. When you experience aftershock, you feel a second or third minor vibration from the original earthquake.
Injury and death to people. Wreckage to the environment and a weaker economy.
The Richter and Moment Magnitude scale are both logarithmic scales so that a scale 1 earthquake would be 10 times weaker than a scale 2 earthquake and 100 times weaker than a scale 3 earthquake, so mathmatically I would say that it increases by a tenth of a scale 7 earthquake.
An aftershock is a smaller earthquake that follows the main earthquake, usually occurring in the same area and caused by the shifting of rock underground. Aftershocks can happen within hours, days, or even months after the initial earthquake. These can be as strong as or weaker than the main earthquake.
Which earthquake, there have only been about a few thousand recorded.
It depends! Depending upon the built-in energy at the epicenter before and after the earthquake (main shock), and/or the energy (especially stored at some weaker places) generated after the earthquake, aftershocks of an earthquake range in their time.For more details, refer: http://www.answers.com/library/Wikipedia-cid-1349 Aftershock
An earthquake gets weaker as you move away from the epicenter because the seismic waves spread out in all directions, losing energy as they travel through the Earth's layers. The farther you are from the epicenter, the more the energy of the seismic waves is spread out over a larger area, resulting in weaker shaking.
Earthquakes are very short, almost never longer than 1 minute, usually around 30 seconds. Weaker aftershocks occur afterward, these are around 10 seconds. The aftershocks are also very short, usually shorter than the initial earthquake. But in that small amount of time, earthquakes can cause massive damage.
An earthquake can happen anywhere. But some places are more active than others.
NewOrleans, (hurricane), Haiti, (earthquake),Japan (earthquake)Srilanka(tsunami), Turkey (earhquake), Chile (earthquake)
Earthquakes are stronger at the epicenter because that is where the earthquake originates and where the release of energy is most intense. As seismic waves propagate outwards from the epicenter, they decrease in intensity and strength. At the edge of the earthquake, the seismic waves are weaker compared to those at the epicenter.
Yes it has. It had a few earhtquakes.