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Alright, so how do we know how strong an **earthquake** is? This is where the **Richter scale** and **moment magnitude scale** come in handy. These scales measure the size or magnitude of an **earthquake**. The **Richter scale**, developed in the 1930s, was one of the first methods for measuring **earthquake** strength. It's based on the amplitude of seismic waves recorded by seismographs. However, it's less accurate for very large **earthquakes**. The **moment magnitude scale** (Mw) is now the most widely used scale by seismologists. It measures the total energy released by an **earthquake**. This scale is calculated from the seismic moment, which considers the area of the fault that slipped, the distance the fault moved, and the rigidity of the rocks involved. The **moment magnitude scale** is more accurate for all sizes of **earthquakes**, especially the larger ones. So, when you see a magnitude listed for an **earthquake**, it's usually the **moment magnitude**. The magnitude is expressed as a number, for example, a 5.0 **earthquake** is ten times stronger than a 4.0 **earthquake**. The intensity of the **earthquake** is measured using the **Modified Mercalli Intensity Scale** (MMI). This scale measures the effects of an **earthquake** on the Earth's surface, humans, objects, and buildings. It's expressed in Roman numerals, ranging from I (not felt) to XII (catastrophic). The MMI gives you an idea of how much damage and shaking was experienced in a specific location. The intensity depends on the magnitude of the **earthquake**, the distance from the epicenter, and the local geological conditions. Both the magnitude and intensity scales are used to assess the impact of **earthquakes**. So, understanding how these **earthquakes** are measured helps us understand the impact and the severity of the **earthquake**. Now, let’s dig into what to do in case an **earthquake** occurs.
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