All three rock types (igneous, sedimentary, and metamorphic) could be formed due to the presence of a hot spot or plume, although igneous rock would seem most obvious. Currently there is a debate occurring on the origin of so-called "hot spots". See related link below.
islands like Hawaii
A hot spot is not associated with a plate boundary.
A hot spot trail is the result of a plate moving over a stationary hot spot. Only the volcanoes near the hot spot. Those away from it in the direction of the plate's movement are extinct. A volcanic island arc is a chain of volcanoes that forms at a subduction zone, where one oceanic plate slides beneath another. The volcanoes in such an arc will be largely active.
A volcanic hot spot forms from upwelling magma usually due to the subduction of a tectonic plate. As plates move over this area new volcanoes are formed. +++ A hot spot alone is the top of a convection plume in the Mantle, not above subduction. This type of hot spot can lead to continental rifting.
A Hot spot is stationary in time and burns though the solid lithosphere creating an island through volcanic eruptions. The lithosphere is separated into plates that move around so if a hot spot occurs under an oceanic plate it forms a island and as the plate moves (and the hot spot does not) it forms a chain of islands (as the plate moves over the hot spot). This is how the Hawaiian chain is formed.
islands like Hawaii
A hot spot is not associated with a plate boundary.
Hot lava, when cooled and solidified, forms igneous rocks. Examples include basalt, granite, and obsidian.
A hot spot trail is the result of a plate moving over a stationary hot spot. Only the volcanoes near the hot spot. Those away from it in the direction of the plate's movement are extinct. A volcanic island arc is a chain of volcanoes that forms at a subduction zone, where one oceanic plate slides beneath another. The volcanoes in such an arc will be largely active.
A volcanic hot spot forms from upwelling magma usually due to the subduction of a tectonic plate. As plates move over this area new volcanoes are formed. +++ A hot spot alone is the top of a convection plume in the Mantle, not above subduction. This type of hot spot can lead to continental rifting.
A hot spot. An example of a hot spot are the islands in Hawaii which were made from hot spots.
It's a fixed spot from below the mantle - the same type as the one that forms the Hawaiian Islands. And when it blows it will ruin America (for about a thousand years).
A Hot spot is stationary in time and burns though the solid lithosphere creating an island through volcanic eruptions. The lithosphere is separated into plates that move around so if a hot spot occurs under an oceanic plate it forms a island and as the plate moves (and the hot spot does not) it forms a chain of islands (as the plate moves over the hot spot). This is how the Hawaiian chain is formed.
No type of volcano forms at transform boundaries, unless an unconnected event (hot spot) creates it. Basically, no.
Igneous rocks are formed when rock melts in a volcano or other hot spot.
most volcanoes are formed from a hot spot in the earths crust.
lava ozzing out of a vent which is a hot spot