Earthquake isolines are strains that join factors of equal seismic depth. They’re used to map the distribution of floor shaking after an earthquake. Isolines can be utilized to determine areas which can be susceptible to injury from future earthquakes.
Earthquake isolines are usually created utilizing knowledge from seismometers. Seismometers are devices that measure the bottom movement brought on by earthquakes. The info from seismometers can be utilized to create a map of the earthquake’s epicenter and to find out the magnitude of the earthquake.