Volcanoes can form in a two different ways. The first is formed at destructive plate boundaries where one plate is subducted underneath the other. This subduction causes the plate to melt due to pressure and heat from the mantle. This newly melted crust is less dense than the surrounding magma which means it rises to the surface in the form of the volcano. The second type of volcano is formed by a concentration of radioactive elements in the mantle creating a magma column which creates an area of the crust which is thinner and creating a volcano at this point (a 'hot spot'). As the crust moves over the top of this hot spot it creates a chain of islands with only one active volcano (for example the Emperor Seamount Chain which Hawaii is part of).
a shield volcano
It forms a 'caldera'.
IT IS A Sheild volcano
A shield volcano forms where plates pull apart. This type of volcano has gentle sloping sides and is characterized by its low viscosity lava flows. Examples of shield volcanoes include those in Hawaii.
A divergent
nothing
A caldera may form in the centre of a very large volcano.
Composite
Cinder Cone Volcano
When magma slowly rises up the inside the crater of a larger volcano, it forms a Lava Dome.
No, it forms a volcano.
a volcano landform