The world has encountered a series of earthquakes of high magnitudes. The devastating 7.0 earthquake hitting Haiti in January 2010 and took away more than 200,000 precious lives, the massive 8.2 magnitude earthquake in Fiji in August, the 7.5 earthquake in Indonesia in September, and a 7.9 magnitude earthquake in Fiji during September, all make us shudder.
How Does an Earthquake Occur?
This strong lithosphere is further broken down into plates called tectonic 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. 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.
There are three main tectonic movements: extensional, transform, and compressional, all of which result in different types of earthquakes. The movements of these plates is usually very slow, usually the same speed our fingernails grow! It's when these plates collide against each other, that rock layers are forced upwards in the form of mountains.
When these plates move away from one another, lava from the mantle fills the gap and forms a new crust. These plates also converge over a period of thousand years by slowly positioning them one beneath the other.
Science Behind Earthquakes
Earthquakes occur at the edges of the plates, and more commonly at the edges of large plates. The plate boundaries mostly lie beneath the oceans and cannot be seen.
However, their boundaries can be mapped accurately from outer space, via measurements from GEOSAT satellites. Earthquakes happen when these plates move under, slide past one another, or collide into one another.
Since the edges of these plates are rough, the sliding process is not very smooth. As the plates slide past one another, parts of the plate get stuck, while the rest continues moving. So, one portion of the plate clings on to opposing portion of the other plate, while the rest of the plate gradually moves forward.
Potential energy keeps building up in the locked or stuck portion of the plates. When the unstuck part of the plate has moved far enough, the force exerted by it pulls the stuck regions apart. This ripping of the stuck part of opposing plates results in release of oodles of potential energy, that was stored for the sliding movement.
As the ripples of these waves move, they shake our earth and quaking of the earth takes place. There are two kinds of waves that radiate through the earth during an earthquake, one called the Rayleigh waves which move with a rolling, up and down motion, while the other is called love waves, which cause the ground to twist from side to side.
They are responsible for quaking, cracking of the earth's crust, crumbling of buildings, etc. Depending on the amount of energy released in the form of these waves, the earthquake's magnitude varies. They're also triggered by volcanic eruptions wherein, molten magma under the earth's crust exert enormous pressure, releasing it through openings in the plates.
There is a lot of research being conducted by scientists in the field of earthquake forecasting, so as to minimize the amount of devastation caused by it. Intimating people before an earthquake and evacuating the area would help save millions of lives.
However, despite all the decades of efforts scientists have not been able to predict earthquakes, so, the best thing to do as of today is to update yourself about earthquake management.