how are earthquakes at continental plate boundaries different from earthquakes at mid ocean ridges
Earthquakes at continental plate boundaries are typically larger and more powerful than earthquakes at mid-ocean ridges. This is because at plate boundaries, tectonic plates are continuously scraping past or colliding with each other, causing intense pressure and friction to build up until it is released in the form of an earthquake. These earthquakes can cause significant damage to infrastructure and result in widespread destruction.
On the other hand, earthquakes at mid-ocean ridges are generally smaller and less destructive. This is because at mid-ocean ridges, tectonic plates are moving away from each other, allowing magma to rise up from the mantle and create new oceanic crust. The earthquakes that occur at mid-ocean ridges are usually a result of the movement of magma and the formation of new crust, rather than the intense pressure and friction seen at continental plate boundaries.