Describe two types of plate boundarieswhere volcanic eruptions can occur?

There are three main types of plate boundaries: divergent boundaries, convergent boundaries, and transform boundaries. Volcanic eruptions can occur at divergent boundaries and convergent boundaries.

1. Divergent boundaries: At a divergent boundary, two tectonic plates are moving apart from each other. This pulling apart causes magma to rise from the mantle, creating a gap or rift between the plates. As the magma reaches the surface, it erupts, forming volcanic activity. Examples of divergent boundaries include the Mid-Atlantic Ridge and the East African Rift Zone.

2. Convergent boundaries: At a convergent boundary, two tectonic plates are moving towards each other. There are three types of convergent boundaries: oceanic-oceanic, oceanic-continental, and continental-continental.

- Oceanic-Oceanic Convergence: When two oceanic plates collide, the denser one sinks beneath the other in a process called subduction. As the oceanic plate goes deeper into the mantle, it is subjected to high temperature and pressure, causing it to melt partially. This molten material rises to the surface, resulting in volcanic eruptions. The Pacific Ring of Fire, which includes the subduction zones around the Pacific Ocean, is a prime example of oceanic-oceanic convergence.

- Oceanic-Continental Convergence: When an oceanic plate collides with a continental plate, the denser oceanic plate is subducted beneath the lighter continental plate. The subduction process triggers the melting of the oceanic plate, leading to the formation of volcanoes on the continental plate. Well-known examples of oceanic-continental convergence volcanic activity include the Cascade Range in the western United States and the Andes Mountains in South America.

It's worth noting that while volcanic eruptions predominantly occur at divergent and convergent boundaries, they can also happen within the boundaries themselves, such as in the case of volcanic arcs or volcanic islands formed at convergent boundaries.