1. Earthquakes are caused by movements in the Earth's crust along fault lines and plate boundaries. The most severe earthquakes typically occur at destructive and conservative plate boundaries.
2. Scientists can measure earthquakes using seismographs, which detect seismic waves. The Richter scale is used to quantify the magnitude or strength of an earthquake based on the seismograph recording.
3. In addition to the Richter scale, the Mercalli scale is used to describe the intensity or amount of damage caused by an earthquake based on observations of its effects.