Earthquakes can be measured using several methods, including:
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Seismographs: Instruments that record the motion of the ground during an earthquake, providing data on its intensity and duration.
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Richter scale: A logarithmic scale that quantifies the amount of energy released during an earthquake.
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Moment Magnitude Scale (Mw): A more modern scale that measures the total energy released and is more accurate for large earthquakes.
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Modified Mercalli Intensity Scale: A qualitative scale that assesses the impact of an earthquake based on human observations and structural damage.
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GPS and InSAR: Technologies that monitor ground displacement over time to assess tectonic movements and potential earthquake risks.
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