The edges of the plate
Not that Often, According to scientist its about 30 years.
Countries not on a tectonic plate boundary can still experience earthquakes due to intraplate seismic activity. This can happen when stress builds up within a tectonic plate and is released suddenly, causing an earthquake. Additionally, faults within a plate can also generate seismic activity.
a tectonic plate
Earthquakes are least likely to occur in the interiors of tectonic plates, away from plate boundaries. These regions are known as intraplate regions and typically experience fewer seismic activities compared to areas along plate boundaries.
An earthquake zone is likely to be along fault lines or where two or more tectonic plates meet or a chain of volcanoes parallel to a continental coast.
The tectonic plates involved in Japan's 2011 earthquake were the Pacific Plate and the North American Plate. The earthquake resulted from the Pacific Plate subducting beneath the North American Plate along the Japan Trench.
The tectonic plates involved in the Haiti earthquake are the Caribbean Plate and the North American Plate. The earthquake was caused by the movement along a strike-slip fault between these two plates.
The city most likely to experience a major earthquake would be located near the boundaries where tectonic plates meet, such as in regions along the Pacific Ring of Fire, where there is high seismic activity due to plate interactions. Cities like Tokyo, Los Angeles, or Istanbul are more prone to major earthquakes due to their proximity to plate boundaries.
Where a tectonic plate slides past another.
earthquake
I think it was the Caribbean plate and the cocos plate.
The Haiti earthquake occurred at the boundary of the Caribbean tectonic plate and the North American tectonic plate. The specific fault line responsible for the earthquake was the Enriquillo-Plantain Garden fault zone.