called the “”Ring of Fire”” due to the prevalence of volcanic action. Most quakes happen at zones where tectonic plates impact or slide against one another. These effects are normally slow and unnoticeable at first glance; on the other hand called the “”Ring of Fire”” due to the prevalence of volcanic action. Most quakes happen at zones where tectonic plates impact or slide against one another. These effects are normally slow and unnoticeable at first glance; on the other hand tremendous anxiety can develop between plates. At the point when this anxiety is discharged rapidly