If the locations of earthquakes over the past 10 years were plotted on a world map, the observation that would be made is:
Earthquakes generally occur along the edges of tectonic plates.
This is because most earthquakes are associated with the movement of tectonic plates, which often leads to seismic activity along plate boundaries. Regions situated near these boundaries, such as the Pacific Ring of Fire, experience a higher frequency of earthquakes compared to areas situated in the interior of tectonic plates or away from plate boundaries.