Volcanology
Volcanic arcs are chains of volcanoes that are formed above a subducting plate at convergent plate boundaries. These arcs typically result from the melting of the subducted oceanic crust, leading to magma formation that rises to the surface and creates volcanic activity. The volcanic arcs are crucial for understanding the relationship between tectonic processes and volcanism, as they illustrate how plate interactions can lead to significant geological features.
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