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Did you know that the earth receives over 1,000 earthquakes in a year? Most of them are in the arctic region and at the fault lines of the tectonic plates. A majority of them are less than the magnitude of 3 on the Richter Scale so they don't pose a great threat to us! But there is something that affects students studying Earthquake Engineering on a greater level. Ever-growing Piles of Assignments are causing stress to students in universities across the globe. Thankfully, our competent Earthquake Engineering Homework Help can help students with their stress! Our Experts can leverage their decades of knowledge to write plagiarism-free, polished, and well-referenced assignment solutions for you in a jiffy! Get help from our experts and get an impressive, high-scoring solution written for yourself while you relax!
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Fundamentally, the earthquake would occur when the fault line encounters a sudden breaking point in the rocks under the surface of the earth. The process of breaking rocks and rubbing against each other makes them strong enough to cause seismic vibrations that traverse the earth like an earthquake. If the vibrations are strong enough, they can cause a lot of damage to man-made structures when they reach the surface of the earth.
The closer the breaking point, the greater would be the energy experienced in the region. Earthquakes that span over large fault lines can be immensely destructive. For example, the Tsunami that hit Japan in 2011 was a result of an Earthquake that moved one of the primary tectonic plates underneath the region.
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Plate tectonics is an acclaimed theory that describes the large-scale motion of large plates and the simultaneous vibrations of smaller plates in the Earth's lithosphere. Since the beginning of the tectonic processes that began around 3.5 billion years ago, earthquakes have been the native force to the forces of nature.
A tectonic plate is alternatively known as a lithospheric plate. It is nothing but a slab of irregularly shaped solid rock that is composed of oceanic lithosphere. The sizes of these plates can vary significantly from being a few sq km in area to hundreds of sq km in area. These layers together compose the oceanic and continental lithosphere.
Faults are the areas of the crust that move with respect to each other. These are the meeting points of two tectonic plates. But, as the rocks do not move very easily, strain builds up between the fault lines. At weak points, this strain breaks the rocks and forms a ridge or a rift.
Locking interface is the event when one of the plates slides down beneath the other rock. They are not free to pass each other smoothly, or in some places, they grate very slowly and steadily past each other. It is very often that the plates would lock together to an extent. The area of the lock that touches and locks is known as the locking surface.
These plates are the types that are found underneath the pacific ocean but not found on any major landmass. Events like Volcanic eruptions and earthquakes are accosted with the regions that lie on the edges of this plate, for example, Japan, which lies on the west coast of North America and New Zealand.
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