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Before we jump into the titans of seismic events, let's get acquainted with the fundamental concepts. An **earthquake** is essentially the result of a sudden release of energy in the Earth's lithosphere, creating seismic waves. These waves radiate outwards from the **focus**, or the point where the rupture begins, and travel through the Earth. The point on the surface directly above the focus is called the **epicenter**. Now, the main culprit behind these events? Tectonic plates, my friends! These massive slabs of rock are constantly moving, interacting at **fault lines**. When stress builds up along these fault lines, the rocks eventually give way, leading to an earthquake. There are three main power query m nested if statement types of fault lines: strike-slip, normal, and reverse faults. Each type of fault moves differently, resulting in different types of ground motions during an earthquake. This is where those nasty **seismic waves** come into play. These can be categorized into P-waves (primary waves), which are the fastest and travel through solids and liquids, and S-waves (secondary waves), which are slower and can only travel through solids. Then there are surface waves, like Love waves and Rayleigh waves, which cause the most destruction. So, how do we measure this ground shaking? Scientists use instruments called **seismographs** to record the ground motion, and from this data, they can calculate the magnitude of an earthquake.
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