It … Get in touch with us and we'll talk...However, their boundaries can be mapped accurately from outer space, via measurements from GEOSAT satellites. The rocks still push against each other but are not moving. The devastating 7.0 earthquake hitting Haiti in January 2010 and took away more than 200,000 precious lives, the Would you like to write for us? Whenever a tectonic plate moves suddenly, this causes an earthquake.The sudden release of friction and pressure between tectonic plates causes an earthquake. When these plates underline the oceans, they are termed as oceanic plates, whereas, when they underline the continents, they are referred to as continental plates.As the mantle within the earth’s crust moves, the plates also begin to move and start pulling away from each other. Sign up to receive the latest and greatest articles from our site automatically each week (give or take)...right to your inbox. When the unstuck part of the plate has moved far enough, the force exerted by it pulls the stuck regions apart. While they are far more common in some regions than others earthquakes can occur anywhere. An earthquake is a shock wave that radiates to the Earth's surface from underground. These cookies will be stored in your browser only with your consent. Let's take a look at how it happens.The world has encountered a series of earthquakes of high magnitudes. Earthquakes happen when these plates move under, slide past one another, or collide into one another.The surfaces where these plates slip are termed as fault planes or faults, and the plate boundaries are made up of several such faults or slipping zones.Since the edges of these plates are rough, the sliding process is not very smooth.
Land can also collapse or pull apart, causing more buildings to fall.
The plate boundaries mostly lie beneath the oceans and cannot be seen.Would you like to write for us? These plates also converge over a period of thousand years by slowly positioning them one beneath the other.Earthquakes occur at the edges of the plates, and more commonly at the edges of large plates. Thus, the earth’s crust is not actually one solid layer, instead is like a puzzle, with pieces coming together to form one big picture.The size of these puzzle pieces or plates can vary from a few hundred to thousands of kilometers, while their thickness may vary from less than 15 km to 200 km. Aftershocks follow and can continue for weeks, months or even years.Fault lines are the areas where two or more tectonic plates join, and it's in these areas most earthquakes occur. If you are lucky, you might get a little bit of advance warning in the form of tremors or smaller, less-damaging quaking, but as a rule they will occur without warning. The Earth is made of an inner core, an outer core and a mantle, and the final layer is a thin crust covering the mantle, which is the surface of the Earth including all the oceans and continents. These cookies do not store any personal information.Any cookies that may not be particularly necessary for the website to function and is used specifically to collect user personal data via analytics, ads, other embedded contents are termed as non-necessary cookies. You also have the option to opt-out of these cookies.
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