As usual Minnesota is right.

To embellish his answer a little, here are some excerpts from
Annals of the Former World by John McPhee, a Pulitzer-Prize winning book about geology. Highly recommended.
(Page 390, discussing Yellowstone): "[Geologists] believe that as North America slides over this fixed locus of thermal energy the rising heat is so intense that it penetrates the plate...The geologic term for such a place is 'hot spot.' The earth seems to have about sixty of them -- most older, and many less productive, than Yellowstone...Hawaii is the world's most preserved and trackable hot spot."
(Page 392): "Hot spots provide one more way of calculating plate velocities, for hot spots are to the drift of plates as stars to navigation."
(Page 397): "Heat rising from hot spots apparently lubricates the asthenosphere -- the layer on which the plates slide. According to theory, the plates would stop moving if the hot spots were not there...From very deep in the mantle (and perhaps all the way from the core) the heat is thought to rise in a concentrated column, and for this reason is alternatively called a plume."
(Pages 398-9): "Hot spots seem to be active for roughly a hundred million years...The perforations made by hot spots may be analogous to the perforations in sheets of postage stamps. Plume tracks might weaken the plates through which they pass, so that tens of millions of years later the plates would break apart along those lines."
Hope that helps.