How do scientists know the size of earthquakes which occurred before recording instruments were used e.g. 1843, 1690 earthquakes?
The level of shaking from an earthquake diminishes with distance. Mathematical relationships between the area experiencing a specified level of shaking and events with instrumental magnitudes have been derived. These mathematical equations can then be used to estimate the magnitude of pre-instrumental earthquakes, for which the area with the specified level of shaking is known.