Question

How is a mantle plume (hot spot) different from volcanoes in the Ring of Fire? How are they similar? Give one specific example of a hot spot volcano.

Answer 1

The difference is the matle plum (hot spot)  is nowhere near tectonic plate edges,  
Even though they located far away from the tectonic edge, mantle plume still able to spewed out  enough lava to covered the whole continent

hope this helps

Answer 2

The difference between a hot spot volcano and the volcanoes from Ring of Fire can mainly be seen in the way of formation and functioning. The hot spot volcanoes are far away from any tectonic plate boundary and they manage to penetrate the crust over them and come out on the surface to usually create volcanic islands. The activity of the volcanoes from the Ring of Fire depends directly from the activity between the bordering tectonic plates, and as the borders move over time, the volcanoes stop existing, and new ones rise in the direction where the boundary moves.

The similarity can be seen in the type of eruptions, and that usually both types of volcanoes form volcanic islands.

Example for a hot spot volcano is Mauna Loa on Hawaii.