Volcano-Intro

Convergent boundary

Divergent boundary

Hot spot

all of the choices

volcanic island arc

continental volcanic arc

mountain

none of the choices

seamounts are the early stage of composite volcanoes while volcanic islands are grown seamounts

seamounts are the early stage of shield volcanoes while volcanic islands are grown seamounts

seamounts are the late stage of composite volcanoes while volcanic islands are early seamounts of cinder cones

seamounts are the late stage of cinder cones while volcanic islands are early seamounts

Height

Shape

Location

none of these

Hawaiian Islands are formed due to hot spots.

It is also known as Intraplate Volcanism.

It is located far from plate boundaries.

It moves with the motions of plates.

Continental lithosphere resist subduction

It’s impossible to have two continental plates in a convergent boundary

Oceanic lithosphere resist subduction

There’s subduction between two continental plates but magma cools eventually