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The majority of the volcanoes are found in these geologically active borders. Divergent and convergent plate borders are the two types of plate boundaries that are most likely to result in volcanic activity.
Where the tectonic plates are moving in the same direction is known as destructive or convergent plate borders. Here, volcanoes can occur when an oceanic plate sinks beneath another oceanic plate or when an oceanic plate sinks beneath a continental plate. Subduction zones and mid-ocean ridges are examples of divergent borders where volcanism occurs, although transform boundaries are less frequently affected.There is a lot of volcanic activity along divergent borders and regions of continental rifting, in addition to the majority of volcanoes being connected to convergent plate boundaries (at subduction zones). The tectonic plate borders are home to 60% of all active volcanoes. The majority of volcanoes are situated around the Pacific Ocean's "Ring of Fire," which is a band of volcanic activity.
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